Updated Rupice Mineral Resource Estimate
Adriatic Metals PLC
('Adriatic Metals' or the 'Company')
UPDATED RUPICE MINERAL RESOURCE ESTIMATE AND DRILLING RESULTS
To see the images referred to in the release, please click here
http://www.rns-pdf.londonstockexchange.com/rns/5481X_1-2020-8-31.pdf
HIGHLIGHTS:
• Indicated and Inferred Mineral Resource estimate ("MRE") for Adriatic Metals' 100%-owned Rupice silver-gold-zinc-lead deposit in Bosnia & Herzegovina, now stands at:
• 12.0Mt @ 149g/t Ag, 1.4g/t Au, 4.1% Zn, 2.6% Pb, 0.5% Cu, 25% BaSO4 (reported above a cut-off grade of 50g/t AgEq) containing 58Moz Ag, 527koz Au, 489kt Zn & 312kt Pb
• This represents a 32% increase in tonnes compared to the maiden 2019 Rupice MRE (using a 50g/t AgEq cut-off).
• 79% of the updated Mineral Resource is classified as Indicated.
• The updated MRE will provide the foundation to the PFS, which will incorporate ongoing metallurgical test work results and mining studies designed to optimise and improve the planned development configuration of the project compared with that outlined in the November 2019 Scoping Study.
• Recent drilling has also intersected high-grade massive sulphide mineralisation at Rupice - with the system remaining open towards the north and down-dip to the south.
Adriatic Metals Plc (ASX:ADT, LSE:ADT1) ("Adriatic" or the "Company") is pleased to announce the updated Mineral Resource estimate for the Rupice Silver Deposit in the Vares Silver Project, in Bosnia & Herzegovina, which has been completed by CSA Global Pty Ltd ("CSA Global").
Paul Cronin, Adriatic's Managing Director and CEO commented, "I am thrilled that we have substantially increased our resource base as we go into the next stage of project development. This updated MRE shows the world class nature of the deposit and positions the Company as one of the leading silver developers in the industry." He also added "During the COVID-19 pandemic, I have been impressed by the resolve of our Vares based team to deliver results in a timely and safe manner. Rupice is an exceptionally high-grade silver dominant deposit, and the increase in tonnes will expand on the results of our 2019 Scoping Study, as we seek to finalise a Pre-Feasibility Study in the coming weeks."
MRE UPDATE
The updated Indicated and Inferred Mineral Resource estimate was prepared by CSA Global in Perth and comprises 12.0 Mt at 149 g/t Ag, 1.4g/t Au, 4.1% Zn and 2.6% Pb, as set out in Table 1.
Table 1 - Rupice updated MRE by Classification
|
Rupice Mineral Resources, August 2020 |
|||||||||||||||
|
JORC Classification |
Tonnes (mt) |
Grades |
Contained metal |
||||||||||||
|
Ag |
Zn |
Pb |
Au |
Cu |
Sb |
BaSO4 |
Ag |
Zn |
Pb |
Au |
Cu |
Sb |
BaSO4 |
||
|
g/t |
% |
% |
g/t |
% |
% |
% |
Moz |
Kt |
Kt |
Koz |
Kt |
kt |
Kt |
||
|
Indicated |
9.5 |
176 |
4.9 |
3.1 |
1.6 |
0.5 |
0.2 |
29 |
54 |
466 |
294 |
500 |
52 |
22 |
2,732 |
|
Inferred |
2.5 |
49 |
0.9 |
0.7 |
0.3 |
0.2 |
0.1 |
9 |
4 |
23 |
18 |
27 |
4 |
3 |
218 |
|
Total |
12.0 |
149 |
4.1 |
2.6 |
1.4 |
0.5 |
0.2 |
25 |
58 |
488 |
312 |
526 |
56 |
24 |
2,949 |
Notes:
· Mineral Resources are based on JORC Code definitions.
· A cut-off grade of 50g/t silver equivalent has been applied.
· AgEq - Silver equivalent was calculated using conversion factors of 31.1 for Zn, 24.88 for Pb, 80.0 for Au, 1.87 for BaSO4, 80.87 for Cu and 80.87 for Sb, and recoveries of 90% for all elements. Metal prices used were US$2,500/t for Zn, US$2,000/t for Pb, $150/t for BaSO4, $2,000/oz for Au, $25/oz for Ag, $6500/t for Sb and $6,500 for Cu.
· The applied formula was: AgEq = Ag(g/t) * 90% + 31.1 * Zn(%) * 90% + 24.88 * Pb(%) * 90% + 1.87 * BaSO4% * 90% + 80 * Au(g/t) * 90% + 80.87 * Sb(%) * 90% + 80.87 * Cu(%)* 90%
· It is the opinion of Adriatic Metals and the Competent Persons that all elements and products included in the metal equivalent formula have a reasonable potential to be recovered and sold.
· Metallurgical recoveries of 90% have been applied in the metal equivalent formula based on recent and ongoing test work results.
· A bulk density was calculated for each model cell using regression formula BD = 2.745 + BaSO4 * 0.01793 + Pb * 0.06728 - Zn * 0.01317 + Cu * 0.1105 for the halo domain, BD = 2.7341 + BaSO4 * 0.01823 + Pb * 0.04801 + Zn * 0.03941 - Cu * 0.01051 for the fault zones and BD = 2.7949 + BaSO4 * 0.01599 + Pb * 0.05419 + Zn * 0.01169 + Cu * 0.06303 for the low grade domain. Bulk density values were interpolated to the combined high-grade domain from 631 BD measurements.
· Rows and columns may not add up exactly due to rounding.
RUPICE DRILLING AND SAMPLING
For the Mineral Resource estimate, a total of 167 diamond drill holes ( 46 historical drill holes and 121 drill holes from the Company's drilling programmes in 2017 (8 holes), 2018 (39 holes), 2019 (52 holes) and 2020 (22 holes) ) for 38,135m define the current limits of the known mineralisation. The deposit was drilled and sampled using diamond drill holes at a nominal 20m by 20m spacing.
Drill holes drilled by the Company were generally angled -50° to -80° mostly towards the southwest with dip angles set to optimally intersect the mineralised bodies. Additional drill holes were drilled from the opposite direction, and perpendicular to the mineralised trend. All the historical holes were vertical and focussed on the up-dip portion of the Rupice mineralisation.
The drill core was sampled for assay; whole core for the historical drilling and half core (HQ and PQ) for the recent drilling. Recent assays were sent to ALS in Bor, Serbia for multi-element analyses.
RUPICE GEOLOGY AND MINERALISATION
The host rocks at Rupice comprises Middle Triassic limestone, dolostone, calcareous and dolomitic marl, and a range of mostly fine-grained siliciclastic rocks including cherty mudstone, mudstone, siltstone and fine-grained sandstone. The main mineralised horizon is a brecciated dolomitic unit that dips at around 50o to the northeast and has been preferentially mineralised with base, precious and transitional metals. The Triassic sequence has been intensely deformed both by early stage ductile shearing and late stage brittle faulting.
The Rupice polymetallic mineralisation consists of sphalerite, galena, barite and chalcopyrite with silver, gold, tetrahedrite, boulangerite and bournonite, with pyrite. The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody.
To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south.
RUPICE MODELLING AND GRADE INTERPOLATION
The main geological features that control the polymetallic mineralisation at Rupice were interpreted using geological and structural data collected. Three main domains were interpreted and wireframed individually; the main mineralised brecciated dolomitic units, that hosts the high-grade mineralisation; the fault zones that off-set and displace these main mineralised bodies; and a lower-grade halos peripheral and in the footwall of the main mineralised bodies.
Statistical analysis of modelled domains showed that the main mineralised brecciated dolomite has a bimodal population for the majority of the elements being modelled. The higher-grade populations clustered spatially and were subsequently individually interpreted and wireframed.
Ten elements were modelled; Ag, Zn, Pb, BaSO4, Cu, Au, Sb, Hg, As and S, and the higher-grade populations were interpreted and wireframed for all elements except Hg, As and Sb.
All the domains were interpreted on a section by section basis and were used to generate 3D 'solid' wireframes. The same methodology was applied for the individual high-grade populations.
Once mineralisation for each element was interpreted and wireframed, classical statistical analysis was repeated for the samples within the interpreted domains. Drill data was composited to 2m down hole intervals. Boundary statistical analyses and top cuts were determined and applied.
The geostatistical analysis generated a series of semi-variograms that were used during grade estimation using Ordinary Kriging ("OK"). The semi-variogram ranges determined from the analysis contribute heavily to the determination of the search neighbourhood dimensions. All variograms were calculated and modelled for the composited sample file, constrained by the corresponding mineralised envelopes for each element. Where low-grade and high-grade domains were modelled, samples were combined for both domains to make sure that the number of samples was sufficient for robust geostatistical analysis. It was found that absolute semi-variograms were difficult to model for most of elements, and therefore, relative semi-variograms were modelled for Pb, BaSO4, Ag, Au, Sb, Hg, As and Cu. Absolute variograms were modelled for Zn and S.
The density values were calculated for each model cell using a regression formula for all the domains except the combined high-grade domain. The formula was calculated using scattergrams for density versus BaSO4, Pb, Cu and Zn grades. Density values were interpolated within the limits of the combined high-grade domain.
A block model was constructed, constrained by the interpreted mineralised envelopes. A parent cell size of 5 m(E) x 5 m(N) x 5 m(RL) was adopted with standard sub-celling to 1 m(E) x 1 m(N) x 1 m(RL) to maintain the volumetric resolution of the mineralised lenses.
Grades for all ten elements were interpolated into the empty block model using the Ordinary Kriging method and a "parent block estimation" technique, i.e. all sub-cells within a parent cell were populated with the same grade. The OK process was performed at different search radii until all cells were interpolated. The search radii were determined by means of the evaluation of the semi-variogram parameters, which determined the kriging weights to be applied to samples at specified distances.
Block grades were validated both visually and statistically and all modelling was completed using Micromine software.
RUPICE CLASSIFICATION AND REPORTING
Clause 20 of the JORC (2012) Code requires that all reports of Mineral Resources must have reasonable prospects for eventual economic extraction, regardless of the classification of the resource. The Rupice deposit has reasonable prospects for eventual economic extraction on the following basis:
· Metallurgical test work by WAI has confirmed that the Rupice mineralisation is amenable to flotation processes;
· Preliminary metallurgical test work has confirmed that a barite concentrate should meet API specifications;
· A marketing study by a leading consultant in the field of barite confirmed that there is an opportunity to enter the market as a niche player levering any logistical advantages for a supplier in Bosnia & Herzegovina;
· The cut-off grade adopted for reporting (50g/t Ag equivalent) is considered reasonable given the Mineral Resource will most likely be exploited by underground mining methods and processed using flotation techniques.
The Scoping Study demonstrated that the deposit potentially has a positive net present value (NPV), and that the mineralised zone is potentially mineable using underground methods under the given economic scenario and parameters. CSA Global did not estimate Ore Reserves for the deposit. The deposit appears to have reasonable prospects of eventual economic extraction under a realistic set of criteria.
The Rupice Mineral Resource has been classified based on the guidelines specified in the JORC Code. The classification level is based upon an assessment of geological understanding of the deposit, geological and mineralisation continuity, drill hole spacing, QC results, search and interpolation parameters and an analysis of available density information. The MRE is reported by classification in Table 1, above a cut-off grade of 50g/t silver equivalent.
RECENT DRILL RESULTS
The Company is pleased to announce that it has received assay results from BR-10-20, BR-11-20, BR-12-20, BR-13-20, BR-17-20, BR-18-20, BR-20-20, BR-22-20 and BR-23-20, which have been incorporated into the recent Mineral Resource estimate.
Drillhole BR-20-20 (Figure 7) is the most southern drill hole drilled at Rupice to date. It was designed to test the extension of the Rupice orebody along strike to the southeast. The results from this hole have shown that the massive sulphide mineralisation continues southwards. Follow up drilling will test the continuity of mineralisation to the south, up-dip and down-dip from this intercept.
Drillholes BR-11-20, BR-12-20 (Figure 5) and BR-13-20 (Figure 5) successfully intersected mineralisation. They were designed to test the shallower part of the deposit to the south-west, and to confirm historic drilling results.
BR-17-20 and BR-18-20 (Figure 6) were designed to test the up-dip continuation of the known massive sulphide mineralisation in the central part of the deposit. They were also designed to test potential massive sulphide mineralisation in the footwall of the main mineralised body. Higher grade mineralisation was intercepted in two shorter intervals up-dip from the main mineralised body in BR-17-20, followed by a wider low-grade halo in the footwall of the deposit.
For BR-18-20, massive sulphide mineralisation was encountered up-dip from the main mineralised body, confirming continuity of the known mineralised zone.
Drill hole BR-14-20 in the northern part Rupice, and BR-15-20 in the south-western part of Rupice were also drilled. These were designed as investigate continuity of mineralised zone. Mineralisation was encountered, however of a weaker tenor.
Mineralisation still remains open down-dip and to the south and north, into previously untested ground outside of the current ore block model.
The mineralised intervals of the drill holes are shown in Table 2 with further information in Appendix 1.
Table 2 - Drill Hole Results for the Reported Holes; Lead or Zinc greater than 1%,
|
Hole |
From (m) |
To (m) |
Interval (m) |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 % |
|
BR-10-20 |
204.0 |
206.0 |
2.0 |
2.45 |
1.24 |
0.45 |
16 |
0.07 |
0 |
|
BR-11-20 |
62.2 |
67.0 |
4.8 |
1.68 |
1.73 |
0.66 |
150 |
0.51 |
56 |
|
BR-12-20 |
113.5 |
116.4 |
2.9 |
4.52 |
3.44 |
1.29 |
224 |
0.29 |
32 |
|
BR-13-20 |
123.5 |
134.9 |
11.4 |
2.39 |
1.58 |
0.69 |
54 |
0.55 |
14 |
|
BR-17-20 |
204.0 |
206.0 |
2.0 |
1.85 |
0.82 |
0.89 |
141 |
0.27 |
26 |
|
BR-18-20 |
174.7 |
183.7 |
9.0 |
1.85 |
1.39 |
0.99 |
152 |
0.82 |
51 |
|
BR-20-20 |
228.2 |
238 |
9.8 |
1.62 |
1.50 |
0.55 |
106 |
0.45 |
24 |
|
BR-22-20 |
307.0 |
311.0 |
4.0 |
1.28 |
0.32 |
0.04 |
28 |
0.01 |
4 |
|
BR-23-20 |
329.0 |
338.6 |
9.6 |
5.01 |
5.03 |
1.28 |
431 |
0.60 |
57 |
Drilling at Jurasevac-Brestic was also conducted, designed to test the gravity anomaly defined after data reprocessing in March this year. Five diamond drill holes targeted the main gravity high, and massive and patchy pyrite, and weak lead, zinc and barite mineralisation was encountered. Drilling proved the validity of the gravity anomaly, however, economic mineralisation has not been encountered so far.
Exploration and hydrological drilling works continue on the Vares Silver Project with two rigs testing the mineralisation further southward at Rupice, and one at Veovaca drilling geotechnical and hydrological holes. More drillholes are planned for testing the extensions of Rupice deposit to the south and down-dip.
Authorised by, and for further information please contact:
Paul Cronin
Managing Director & CEO
info@adriaticmetals.com
** ENDS **
Market Abuse Regulation Disclosure
The information contained within this announcement is deemed by Adriatic (LEI: 549300OHAH2GL1DP0L61) to constitute inside information as stipulated under the Market Abuse Regulations (EU) No. 596/2014. The person responsible for arranging and authorising the release of this announcement on behalf of Adriatic is Paul Cronin, Managing Director and CEO.
For further information please visit
www.adriaticmetals.com
;
@AdriaticMetals
on Twitter; or contact:
|
Adriatic Metals PLC |
|
|
Paul Cronin / Emma Chetwynd Stapylton |
Tel: +44 (0) 203 950 9138 |
|
|
|
|
Tavistock Communications Limited |
|
|
Charles Vivian |
Tel: +44 (0) 7977 297903 |
|
Edward Lee |
Tel: +44 (0) 7736 220565 |
|
Gareth Tredway |
Tel: +44 (0) 7785 974264 |
|
|
|
|
The Capital Network |
|
|
Julia Maguire/Lelde Smits |
Tel: +61 2 8999 3699 |
About Adriatic Metals
Adriatic Metals Plc (ASX:ADT, LON:ADT1) is a precious and base metals explorer and developer that owns the world-class advanced polymetallic Vares project in Bosnia & Herzegovina.
The Vares project consists of two high-grade polymetallic deposits, located at Rupice and Veovaca. Bosnia & Herzegovina is well-positioned in central Europe and boasts a strong mining history, pro-mining environment, highly-skilled workforce as well as extensive existing infrastructure and logistics.
The Vares project's captivating economics and impressive resource inventory have attracted Adriatic's highly experienced team, which is expediting exploration efforts to expand the current JORC resource. Results of a recent scoping study indicate an NPV8 of US$917 million and IRR of 107%. Leveraging its first-mover advantage, Adriatic is rapidly advancing the project into the development phase and through to production.
There have been no material adverse changes in the assumptions underpinning the forecast financial information or material assumptions and technical parameters underpinning the Maiden Resource Estimate since the original relevant market announcements which continue to apply.
COMPETENT PERSONS REPORT
The information in this report that relates to the Mineral Resources is based on and fairly represents information and supporting information compiled by Dmitry Pertel. Dmitry Pertel is a full-time employee of CSA Global and is a Member of the Australian Institute of Geoscientists. Dmitry Pertel has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity which he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the Australasian Code for the Reporting of Exploration Results, Mineral Resources, and Ore Reserves (JORC Code). Dmitry Pertel consents to the disclosure of information in this report in the form and context in which it appears.
The information in this report which relates to Exploration Results is based on and fairly represents information and supporting information compiled by Mr Phillip Fox, who is a member of the Australian Institute of Geoscientists (AIG). Mr Fox is a consultant to Adriatic Metals Plc, and has sufficient experience relevant to the style of mineralisation and type of deposit under consideration and to the activity he is undertaking to qualify as a Competent Person as defined in the 2012 Edition of the "Australian Code of Reporting of Exploration Results, Mineral Resources and Ore Reserves". Mr Fox consents to the inclusion in this report of the matters based on that information in the form and context in which it appears.
DISCLAIMER
Forward-looking statements are statements that are not historical facts. Words such as "expect(s)", "feel(s)", "believe(s)", "will", "may", "anticipate(s)", "potential(s)"and similar expressions are intended to identify forward-looking statements. These statements include, but are not limited to statements regarding future production, resources or reserves and exploration results. All of such statements are subject to certain risks and uncertainties, many of which are difficult to predict and generally beyond the control of the Company, that could cause actual results to differ materially from those expressed in, or implied or projected by, the forward-looking information and statements. These risks and uncertainties include, but are not limited to: (i) those relating to the interpretation of drill results, the geology, grade and continuity of mineral deposits and conclusions of economic evaluations, (ii) risks relating to possible variations in reserves, grade, planned mining dilution and ore loss, or recovery rates and changes in project parameters as plans continue to be refined, (iii) the potential for delays in exploration or development activities or the completion of feasibility studies, (iv) risks related to commodity price and foreign exchange rate fluctuations, (v) risks related to failure to obtain adequate financing on a timely basis and on acceptable terms or delays in obtaining governmental approvals or in the completion of development or construction activities, and (vi) other risks and uncertainties related to the Company's prospects, properties and business strategy. Our audience is cautioned not to place undue reliance on these forward-looking statements that speak only as of the date hereof, and we do not undertake any obligation to revise and disseminate forward-looking statements to reflect events or circumstances after the date hereof, or to reflect the occurrence of or non-occurrence of any events.
Table 3 - Collar Information for reported drill holes (MGI Balkans Z6)
|
Drill Hole |
Easting |
Northing |
Elevation |
Average Azimuth (TN) |
Average Dip |
Depth (m) |
|
BR-10-20 |
6519271 |
4894736 |
1206 |
58 |
-85 |
373.6 |
|
BR-11-20 |
6519241 |
4894518 |
1212 |
226 |
-61 |
184.0 |
|
BR-12-20 |
6519275 |
4894592 |
1217 |
227 |
-55 |
130.1 |
|
BR-13-20 |
6519275 |
4894592 |
1217 |
228 |
-71 |
155.2 |
|
BR-17-20 |
6519079 |
4894785 |
1162 |
54 |
-73 |
498.5 |
|
BR-18-20 |
6519151 |
4894717 |
1187 |
64 |
-85 |
607.0 |
|
BR-20-20 |
6519446 |
4894547 |
1265 |
231 |
-73 |
252.2 |
|
BR-22-20 |
6519216 |
4894898 |
1124 |
149 |
-86 |
312.7 |
|
BR-23-20 |
6519411 |
4894627 |
1264 |
223 |
-90 |
368.0 |
Table 4 - Assay Results for reported drill holes
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-10-20 |
0 |
1 |
1 |
0.0054 |
0.0011 |
0.0025 |
<0.5 |
0.0044 |
0.015 |
|
BR-10-20 |
1 |
2.5 |
1.5 |
0.0071 |
0.001 |
<0.005 |
<0.5 |
0.0044 |
0.015 |
|
BR-10-20 |
2.5 |
4.5 |
2 |
0.0166 |
0.0053 |
<0.005 |
<0.5 |
0.0034 |
0.015 |
|
BR-10-20 |
4.5 |
6.5 |
2 |
0.008 |
0.0026 |
<0.005 |
<0.5 |
0.0027 |
0.015 |
|
BR-10-20 |
6.5 |
7.5 |
1 |
0.0055 |
0.0012 |
0.008 |
<0.5 |
0.0038 |
0.015 |
|
BR-10-20 |
7.5 |
9.5 |
2 |
0.01 |
0.001 |
<0.005 |
<0.5 |
0.0045 |
0.015 |
|
BR-10-20 |
9.5 |
11.5 |
2 |
0.0164 |
0.0015 |
<0.005 |
<0.5 |
0.0042 |
0.015 |
|
BR-10-20 |
11.5 |
13.5 |
2 |
0.019 |
0.0059 |
<0.005 |
<0.5 |
0.0038 |
0.015 |
|
BR-10-20 |
13.5 |
14.4 |
0.9 |
0.0257 |
0.0092 |
<0.005 |
<0.5 |
0.0037 |
0.015 |
|
BR-10-20 |
14.4 |
16.4 |
2 |
0.0075 |
0.0062 |
<0.005 |
<0.5 |
0.0015 |
0.015 |
|
BR-10-20 |
16.4 |
17.6 |
1.2 |
0.0079 |
0.0068 |
<0.005 |
<0.5 |
0.0022 |
0.015 |
|
BR-10-20 |
17.6 |
19 |
1.4 |
0.0139 |
0.0167 |
0.005 |
<0.5 |
0.006 |
0.03 |
|
BR-10-20 |
19 |
21 |
2 |
0.0174 |
0.0327 |
0.011 |
<0.5 |
0.0048 |
0.015 |
|
BR-10-20 |
21 |
23 |
2 |
0.0112 |
0.0217 |
<0.005 |
<0.5 |
0.003 |
0.015 |
|
BR-10-20 |
23 |
25 |
2 |
0.006 |
0.0045 |
0.006 |
<0.5 |
0.0035 |
0.03 |
|
BR-10-20 |
25 |
27 |
2 |
0.0103 |
0.0195 |
<0.005 |
<0.5 |
0.0037 |
0.03 |
|
BR-10-20 |
27 |
28.2 |
1.2 |
0.0101 |
0.0224 |
0.007 |
<0.5 |
0.0041 |
0.03 |
|
BR-10-20 |
28.2 |
30 |
1.8 |
0.0088 |
0.0122 |
0.005 |
<0.5 |
0.0036 |
0.015 |
|
BR-10-20 |
30 |
32 |
2 |
0.0083 |
0.0101 |
0.007 |
<0.5 |
0.004 |
0.03 |
|
BR-10-20 |
32 |
34 |
2 |
0.0081 |
0.0107 |
0.01 |
<0.5 |
0.0037 |
0.015 |
|
BR-10-20 |
34 |
36 |
2 |
0.0075 |
0.0176 |
0.005 |
<0.5 |
0.0038 |
0.015 |
|
BR-10-20 |
36 |
38 |
2 |
0.0086 |
0.0212 |
<0.005 |
<0.5 |
0.0042 |
0.015 |
|
BR-10-20 |
38 |
40 |
2 |
0.01 |
0.0091 |
0.006 |
<0.5 |
0.0057 |
0.015 |
|
BR-10-20 |
40 |
42 |
2 |
0.027 |
0.0222 |
0.005 |
<0.5 |
0.0041 |
0.015 |
|
BR-10-20 |
42 |
43.3 |
1.3 |
0.0292 |
0.0276 |
<0.005 |
<0.5 |
0.0032 |
0.015 |
|
BR-10-20 |
43.3 |
44.9 |
1.6 |
0.0132 |
0.0426 |
<0.005 |
<0.5 |
0.0067 |
0.03 |
|
BR-10-20 |
44.9 |
46 |
1.1 |
0.0138 |
0.0169 |
<0.005 |
<0.5 |
0.0021 |
0.015 |
|
BR-10-20 |
46 |
48 |
2 |
0.0234 |
0.0155 |
0.006 |
<0.5 |
0.0039 |
0.015 |
|
BR-10-20 |
48 |
50 |
2 |
0.0227 |
0.0231 |
<0.005 |
<0.5 |
0.003 |
0.03 |
|
BR-10-20 |
50 |
51.9 |
1.9 |
0.0124 |
0.0121 |
<0.005 |
<0.5 |
0.0013 |
0.046 |
|
BR-10-20 |
51.9 |
53 |
1.1 |
0.0094 |
0.0098 |
<0.005 |
<0.5 |
0.0011 |
0.015 |
|
BR-10-20 |
53 |
55 |
2 |
0.0109 |
0.0371 |
<0.005 |
<0.5 |
0.0033 |
0.03 |
|
BR-10-20 |
55 |
57 |
2 |
0.0066 |
0.0042 |
<0.005 |
<0.5 |
0.0017 |
0.03 |
|
BR-10-20 |
57 |
59 |
2 |
0.0231 |
0.0244 |
<0.005 |
<0.5 |
0.0128 |
0.046 |
|
BR-10-20 |
59 |
60.3 |
1.3 |
0.0528 |
0.0179 |
0.005 |
<0.5 |
0.0033 |
0.046 |
|
BR-10-20 |
60.3 |
63.2 |
2.9 |
No sample |
|||||
|
BR-10-20 |
63.2 |
65 |
1.8 |
0.0067 |
0.0132 |
<0.005 |
<0.5 |
0.012 |
0.106 |
|
BR-10-20 |
65 |
67 |
2 |
0.0095 |
0.0232 |
0.011 |
<0.5 |
0.0063 |
0.213 |
|
BR-10-20 |
67 |
69 |
2 |
0.0067 |
0.0175 |
0.008 |
<0.5 |
0.0031 |
0.061 |
|
BR-10-20 |
69 |
71 |
2 |
0.0063 |
0.0061 |
0.009 |
<0.5 |
0.0041 |
0.046 |
|
BR-10-20 |
71 |
73 |
2 |
0.0055 |
0.0036 |
<0.005 |
<0.5 |
0.0026 |
0.046 |
|
BR-10-20 |
73 |
74.4 |
1.4 |
0.0101 |
0.0115 |
<0.005 |
<0.5 |
0.0037 |
0.046 |
|
BR-10-20 |
74.4 |
74.9 |
0.5 |
No sample |
|||||
|
BR-10-20 |
74.9 |
76.6 |
1.7 |
0.0074 |
0.0059 |
0.005 |
<0.5 |
0.0042 |
0.03 |
|
BR-10-20 |
76.6 |
78 |
1.4 |
0.0175 |
0.0069 |
0.007 |
<0.5 |
0.0117 |
0.046 |
|
BR-10-20 |
78 |
80 |
2 |
0.0119 |
0.0055 |
<0.005 |
<0.5 |
0.0059 |
0.03 |
|
BR-10-20 |
80 |
82 |
2 |
0.0153 |
0.0076 |
<0.005 |
<0.5 |
0.0057 |
0.03 |
|
BR-10-20 |
82 |
84 |
2 |
0.0266 |
0.0434 |
0.006 |
<0.5 |
0.0096 |
0.03 |
|
BR-10-20 |
84 |
85 |
1 |
0.0182 |
0.0282 |
<0.005 |
<0.5 |
0.0083 |
0.046 |
|
BR-10-20 |
85 |
86.5 |
1.5 |
0.0179 |
0.0136 |
0.006 |
0.5 |
0.0091 |
0.03 |
|
BR-10-20 |
86.5 |
88 |
1.5 |
0.0195 |
0.0029 |
0.006 |
<0.5 |
0.0073 |
0.03 |
|
BR-10-20 |
88 |
90 |
2 |
0.0114 |
0.0063 |
0.011 |
<0.5 |
0.0078 |
0.03 |
|
BR-10-20 |
90 |
91.4 |
1.4 |
0.0119 |
0.0079 |
0.008 |
<0.5 |
0.0082 |
0.015 |
|
BR-10-20 |
91.4 |
93 |
1.6 |
0.0139 |
0.0048 |
0.008 |
<0.5 |
0.0068 |
0.03 |
|
BR-10-20 |
93 |
95 |
2 |
0.0117 |
0.0035 |
<0.005 |
<0.5 |
0.0046 |
0.03 |
|
BR-10-20 |
95 |
95.9 |
0.9 |
0.0109 |
0.0026 |
<0.005 |
<0.5 |
0.0041 |
0.015 |
|
BR-10-20 |
95.9 |
97 |
1.1 |
0.0082 |
0.0021 |
<0.005 |
<0.5 |
0.0027 |
0.015 |
|
BR-10-20 |
97 |
99 |
2 |
0.0087 |
0.002 |
<0.005 |
<0.5 |
0.0024 |
0.015 |
|
BR-10-20 |
99 |
100.7 |
1.7 |
0.0094 |
0.003 |
0.007 |
<0.5 |
<0.005 |
0.015 |
|
BR-10-20 |
100.7 |
102 |
1.3 |
0.0072 |
0.0065 |
<0.005 |
<0.5 |
0.0021 |
0.015 |
|
BR-10-20 |
102 |
104 |
2 |
0.0097 |
0.0071 |
<0.005 |
<0.5 |
0.0013 |
0.015 |
|
BR-10-20 |
104 |
106 |
2 |
0.0097 |
0.007 |
<0.005 |
<0.5 |
0.0014 |
0.015 |
|
BR-10-20 |
106 |
108 |
2 |
0.0113 |
0.0087 |
<0.005 |
<0.5 |
0.002 |
0.015 |
|
BR-10-20 |
108 |
110 |
2 |
0.0141 |
0.0095 |
<0.005 |
<0.5 |
0.0023 |
0.015 |
|
BR-10-20 |
110 |
111 |
1 |
0.0247 |
0.0121 |
<0.005 |
<0.5 |
0.0039 |
0.03 |
|
BR-10-20 |
111 |
112.2 |
1.2 |
0.0234 |
0.0271 |
<0.005 |
<0.5 |
0.0048 |
0.046 |
|
BR-10-20 |
112.2 |
117.8 |
5.6 |
No sample |
|||||
|
BR-10-20 |
117.8 |
119 |
1.2 |
0.0778 |
0.0479 |
0.007 |
1 |
0.0286 |
0.046 |
|
BR-10-20 |
119 |
121 |
2 |
0.0368 |
0.0942 |
<0.005 |
0.6 |
0.009 |
0.228 |
|
BR-10-20 |
121 |
123 |
2 |
0.0144 |
0.0353 |
<0.005 |
<0.5 |
0.0014 |
0.015 |
|
BR-10-20 |
123 |
125 |
2 |
0.0119 |
0.038 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-10-20 |
125 |
127 |
2 |
0.006 |
0.0524 |
<0.005 |
<0.5 |
0.001 |
0.076 |
|
BR-10-20 |
127 |
129 |
2 |
0.0226 |
0.172 |
0.005 |
1.1 |
0.0155 |
0.015 |
|
BR-10-20 |
129 |
131 |
2 |
0.0303 |
0.2 |
<0.005 |
1.3 |
0.0091 |
0.03 |
|
BR-10-20 |
131 |
132.8 |
1.8 |
0.0318 |
0.15 |
<0.005 |
1.2 |
0.0037 |
0.03 |
|
BR-10-20 |
132.8 |
134 |
1.2 |
0.0164 |
0.0563 |
<0.005 |
<0.5 |
0.004 |
0.046 |
|
BR-10-20 |
134 |
136 |
2 |
0.0229 |
0.0501 |
<0.005 |
<0.5 |
<0.005 |
0.061 |
|
BR-10-20 |
136 |
138 |
2 |
0.012 |
0.0428 |
<0.005 |
0.6 |
0.0024 |
0.061 |
|
BR-10-20 |
138 |
138.5 |
0.5 |
0.0123 |
0.0942 |
<0.005 |
<0.5 |
0.0024 |
0.03 |
|
BR-10-20 |
138.5 |
139 |
0.5 |
No sample |
|||||
|
BR-10-20 |
139 |
141 |
2 |
0.0148 |
0.028 |
<0.005 |
<0.5 |
0.0008 |
0.015 |
|
BR-10-20 |
141 |
143 |
2 |
0.0178 |
0.0226 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-10-20 |
143 |
145 |
2 |
0.0134 |
0.0331 |
<0.005 |
<0.5 |
0.0015 |
0.046 |
|
BR-10-20 |
145 |
147 |
2 |
0.0103 |
0.0088 |
<0.005 |
<0.5 |
0.0007 |
0.137 |
|
BR-10-20 |
147 |
149 |
2 |
0.0195 |
0.005 |
<0.005 |
<0.5 |
0.0021 |
0.137 |
|
BR-10-20 |
149 |
151 |
2 |
0.0191 |
0.0047 |
<0.005 |
<0.5 |
0.0021 |
0.091 |
|
BR-10-20 |
151 |
153 |
2 |
0.0122 |
0.0032 |
<0.005 |
<0.5 |
0.0016 |
0.548 |
|
BR-10-20 |
153 |
153.8 |
0.8 |
0.018 |
0.0066 |
<0.005 |
<0.5 |
<0.005 |
0.046 |
|
BR-10-20 |
153.8 |
155 |
1.2 |
0.0105 |
0.0035 |
<0.005 |
<0.5 |
0.0018 |
0.03 |
|
BR-10-20 |
155 |
157 |
2 |
0.0287 |
0.008 |
<0.005 |
<0.5 |
0.0021 |
0.03 |
|
BR-10-20 |
157 |
159 |
2 |
0.0127 |
0.0043 |
<0.005 |
<0.5 |
0.0019 |
0.061 |
|
BR-10-20 |
159 |
161 |
2 |
0.0157 |
0.004 |
<0.005 |
<0.5 |
0.0024 |
0.137 |
|
BR-10-20 |
161 |
162.2 |
1.2 |
0.0079 |
0.001 |
0.009 |
<0.5 |
0.0013 |
0.213 |
|
BR-10-20 |
162.2 |
164 |
1.8 |
0.0085 |
0.0003 |
<0.005 |
<0.5 |
0.0003 |
0.106 |
|
BR-10-20 |
164 |
165.6 |
1.6 |
0.0094 |
0.0011 |
0.04 |
<0.5 |
0.0033 |
0.106 |
|
BR-10-20 |
165.6 |
167 |
1.4 |
0.0093 |
0.0044 |
0.014 |
1.8 |
0.0109 |
0.669 |
|
BR-10-20 |
167 |
169 |
2 |
0.017 |
0.005 |
<0.005 |
<0.5 |
0.0015 |
0.715 |
|
BR-10-20 |
169 |
171 |
2 |
0.0267 |
0.0026 |
<0.005 |
<0.5 |
0.0013 |
0.73 |
|
BR-10-20 |
171 |
173 |
2 |
0.043 |
0.0651 |
<0.005 |
1.7 |
0.0055 |
0.167 |
|
BR-10-20 |
173 |
175 |
2 |
0.0526 |
0.123 |
0.005 |
1.9 |
0.0067 |
0.548 |
|
BR-10-20 |
175 |
175.9 |
0.9 |
0.0059 |
<0.005 |
0.013 |
<0.5 |
0.001 |
0.335 |
|
BR-10-20 |
175.9 |
177 |
1.1 |
0.0114 |
0.0012 |
<0.005 |
<0.5 |
0.0007 |
0.167 |
|
BR-10-20 |
177 |
178.4 |
1.4 |
0.0131 |
0.0022 |
0.01 |
<0.5 |
0.002 |
0.472 |
|
BR-10-20 |
178.4 |
180 |
1.6 |
0.0429 |
0.0078 |
0.014 |
0.6 |
0.0027 |
0.183 |
|
BR-10-20 |
180 |
182 |
2 |
0.0167 |
0.0082 |
0.026 |
1.1 |
0.0019 |
0.228 |
|
BR-10-20 |
182 |
184 |
2 |
0.0311 |
0.0102 |
0.029 |
2.3 |
0.0017 |
0.38 |
|
BR-10-20 |
184 |
186 |
2 |
0.0796 |
0.0727 |
0.047 |
5.2 |
0.0064 |
0.304 |
|
BR-10-20 |
186 |
188 |
2 |
0.0557 |
0.0348 |
0.033 |
23.3 |
0.0083 |
0.487 |
|
BR-10-20 |
188 |
189.9 |
1.9 |
0.241 |
0.0682 |
0.034 |
15.7 |
0.0068 |
0.593 |
|
BR-10-20 |
189.9 |
191 |
1.1 |
0.0832 |
0.0343 |
0.012 |
3.6 |
0.0119 |
0.487 |
|
BR-10-20 |
191 |
192 |
1 |
0.0088 |
0.004 |
0.032 |
0.7 |
0.0016 |
0.152 |
|
BR-10-20 |
192 |
193 |
1 |
0.0116 |
0.0045 |
0.027 |
0.5 |
0.0015 |
1.034 |
|
BR-10-20 |
193 |
194 |
1 |
0.01 |
0.0054 |
0.013 |
0.6 |
0.0032 |
0.441 |
|
BR-10-20 |
194 |
195 |
1 |
0.0106 |
0.016 |
0.013 |
0.7 |
0.004 |
0.487 |
|
BR-10-20 |
195 |
196 |
1 |
0.0086 |
0.0413 |
<0.005 |
0.5 |
0.0034 |
1.156 |
|
BR-10-20 |
196 |
197 |
1 |
0.0147 |
0.0103 |
<0.005 |
2.3 |
0.0036 |
0.228 |
|
BR-10-20 |
197 |
198 |
1 |
0.0082 |
0.0018 |
0.007 |
1 |
0.001 |
0.046 |
|
BR-10-20 |
198 |
199 |
1 |
0.217 |
0.127 |
0.028 |
6.5 |
0.0088 |
8.276 |
|
BR-10-20 |
199 |
200 |
1 |
0.0192 |
0.017 |
0.02 |
6.6 |
0.0263 |
1.491 |
|
BR-10-20 |
200 |
201 |
1 |
0.0091 |
0.0064 |
<0.005 |
1.4 |
0.0009 |
1.004 |
|
BR-10-20 |
201 |
202 |
1 |
0.0427 |
0.0281 |
0.021 |
3 |
0.0045 |
0.517 |
|
BR-10-20 |
202 |
203 |
1 |
0.0331 |
0.493 |
0.165 |
13.2 |
0.13 |
0.578 |
|
BR-10-20 |
203 |
204 |
1 |
0.022 |
0.0195 |
0.172 |
1.1 |
0.002 |
0.213 |
|
BR-10-20 |
204 |
205 |
1 |
1.295 |
0.615 |
0.354 |
7.3 |
0.0351 |
0.456 |
|
BR-10-20 |
205 |
206 |
1 |
3.6 |
1.86 |
0.545 |
24.8 |
0.101 |
0.198 |
|
BR-10-20 |
206 |
206.9 |
0.9 |
0.0594 |
0.034 |
0.027 |
1.5 |
0.0022 |
0.806 |
|
BR-10-20 |
206.9 |
208 |
1.1 |
0.0139 |
0.0235 |
0.095 |
0.5 |
0.0028 |
1.78 |
|
BR-10-20 |
208 |
209 |
1 |
0.0261 |
0.0139 |
0.06 |
<0.5 |
0.0021 |
0.061 |
|
BR-10-20 |
209 |
210 |
1 |
0.0265 |
0.0088 |
0.032 |
<0.5 |
0.0104 |
0.152 |
|
BR-10-20 |
210 |
211 |
1 |
0.0109 |
0.0105 |
0.037 |
<0.5 |
0.002 |
0.046 |
|
BR-10-20 |
211 |
212 |
1 |
0.024 |
0.0069 |
0.027 |
<0.5 |
0.0012 |
0.046 |
|
BR-10-20 |
212 |
213 |
1 |
0.0113 |
0.0275 |
0.023 |
<0.5 |
0.0028 |
0.046 |
|
BR-10-20 |
213 |
214 |
1 |
0.038 |
0.222 |
0.031 |
1.5 |
0.0099 |
0.03 |
|
BR-10-20 |
214 |
215 |
1 |
0.0403 |
0.288 |
0.049 |
2 |
0.0071 |
0.061 |
|
BR-10-20 |
215 |
216 |
1 |
0.0451 |
0.0182 |
0.055 |
<0.5 |
0.002 |
0.183 |
|
BR-10-20 |
216 |
217 |
1 |
0.0619 |
0.0137 |
0.026 |
<0.5 |
0.0013 |
0.091 |
|
BR-10-20 |
217 |
218 |
1 |
0.0847 |
0.014 |
0.034 |
<0.5 |
0.0016 |
0.076 |
|
BR-10-20 |
218 |
219 |
1 |
0.0963 |
0.015 |
0.187 |
0.8 |
0.0033 |
0.046 |
|
BR-10-20 |
219 |
220 |
1 |
0.173 |
0.007 |
0.189 |
1.2 |
0.0068 |
0.015 |
|
BR-10-20 |
220 |
221 |
1 |
0.0986 |
0.007 |
0.183 |
1.4 |
0.005 |
0.03 |
|
BR-10-20 |
221 |
222 |
1 |
0.13 |
0.0075 |
0.194 |
1.3 |
0.0048 |
0.015 |
|
BR-10-20 |
222 |
223 |
1 |
0.124 |
0.0062 |
0.152 |
0.7 |
0.0029 |
0.015 |
|
BR-10-20 |
223 |
224 |
1 |
0.682 |
0.0389 |
0.688 |
10.9 |
0.119 |
0.015 |
|
BR-10-20 |
224 |
225 |
1 |
0.0527 |
0.0086 |
0.167 |
1.8 |
0.0169 |
0.015 |
|
BR-10-20 |
225 |
226 |
1 |
0.161 |
0.0126 |
0.272 |
2.8 |
0.0113 |
0.03 |
|
BR-10-20 |
226 |
227 |
1 |
0.813 |
0.057 |
0.764 |
12.4 |
0.348 |
0.122 |
|
BR-10-20 |
227 |
228 |
1 |
0.435 |
0.0548 |
0.216 |
3.2 |
0.0336 |
0.35 |
|
BR-10-20 |
228 |
229 |
1 |
0.514 |
0.081 |
0.235 |
3.7 |
0.0413 |
0.03 |
|
BR-10-20 |
229 |
230 |
1 |
0.0689 |
0.0583 |
0.11 |
1.5 |
0.0118 |
0.472 |
|
BR-10-20 |
230 |
231 |
1 |
0.0708 |
0.0048 |
0.042 |
<0.5 |
0.0015 |
0.578 |
|
BR-10-20 |
231 |
232 |
1 |
0.0466 |
0.0047 |
0.056 |
0.5 |
0.0036 |
0.106 |
|
BR-10-20 |
232 |
233 |
1 |
0.0435 |
<0.005 |
0.063 |
<0.5 |
0.0015 |
0.03 |
|
BR-10-20 |
233 |
234 |
1 |
0.0359 |
0.0345 |
0.069 |
0.5 |
0.0043 |
0.015 |
|
BR-10-20 |
234 |
235 |
1 |
0.0402 |
0.0097 |
0.056 |
0.7 |
0.0017 |
1.171 |
|
BR-10-20 |
235 |
236 |
1 |
0.0195 |
0.028 |
0.116 |
0.6 |
0.0027 |
0.061 |
|
BR-10-20 |
236 |
237 |
1 |
0.0113 |
0.0069 |
0.086 |
<0.5 |
0.0016 |
0.015 |
|
BR-10-20 |
237 |
238 |
1 |
0.0181 |
0.0049 |
0.095 |
<0.5 |
0.0015 |
0.015 |
|
BR-10-20 |
238 |
239 |
1 |
0.0534 |
0.0051 |
0.039 |
<0.5 |
0.001 |
0.03 |
|
BR-10-20 |
239 |
240 |
1 |
0.0118 |
0.0093 |
0.051 |
<0.5 |
0.0103 |
0.03 |
|
BR-10-20 |
240 |
241 |
1 |
0.0279 |
0.0108 |
0.055 |
0.5 |
0.0022 |
0.243 |
|
BR-10-20 |
241 |
242 |
1 |
0.0198 |
0.0259 |
0.009 |
<0.5 |
0.0004 |
0.03 |
|
BR-10-20 |
242 |
243 |
1 |
0.0037 |
0.0106 |
0.026 |
<0.5 |
0.0002 |
0.061 |
|
BR-10-20 |
243 |
244 |
1 |
0.154 |
0.0414 |
0.026 |
<0.5 |
0.0411 |
2.601 |
|
BR-10-20 |
244 |
244.8 |
0.8 |
0.0384 |
0.0066 |
0.012 |
<0.5 |
0.0007 |
0.289 |
|
BR-10-20 |
244.8 |
246 |
1.2 |
0.0234 |
0.006 |
0.016 |
<0.5 |
0.0017 |
0.03 |
|
BR-10-20 |
246 |
247.3 |
1.3 |
0.022 |
0.0005 |
<0.005 |
<0.5 |
0.0004 |
0.015 |
|
BR-10-20 |
247.3 |
249 |
1.7 |
0.013 |
0.0006 |
<0.005 |
<0.5 |
0.0008 |
0.008 |
|
BR-10-20 |
249 |
251 |
2 |
0.0161 |
0.0008 |
<0.005 |
<0.5 |
0.0002 |
0.015 |
|
BR-10-20 |
251 |
253 |
2 |
0.0113 |
0.0005 |
0.012 |
<0.5 |
0.0001 |
0.008 |
|
BR-10-20 |
253 |
255 |
2 |
0.0165 |
0.0008 |
0.007 |
<0.5 |
0.0002 |
0.061 |
|
BR-10-20 |
255 |
257 |
2 |
0.017 |
0.0005 |
0.007 |
<0.5 |
0.0001 |
0.008 |
|
BR-10-20 |
257 |
258.3 |
1.3 |
0.0226 |
0.0004 |
<0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-10-20 |
258.3 |
260 |
1.7 |
0.0179 |
0.0011 |
<0.005 |
<0.5 |
0.001 |
0.008 |
|
BR-10-20 |
260 |
262 |
2 |
0.0272 |
0.002 |
<0.005 |
<0.5 |
0.0511 |
0.046 |
|
BR-10-20 |
262 |
262.5 |
0.5 |
0.0189 |
0.0007 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-10-20 |
262.5 |
264 |
1.5 |
0.0165 |
0.0006 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-10-20 |
264 |
266 |
2 |
0.0491 |
0.001 |
<0.005 |
<0.5 |
0.0006 |
0.061 |
|
BR-10-20 |
266 |
266.9 |
0.9 |
0.0096 |
0.001 |
<0.005 |
<0.5 |
0.0008 |
0.046 |
|
BR-10-20 |
266.9 |
268 |
1.1 |
0.0156 |
0.0008 |
<0.005 |
<0.5 |
0.0011 |
0.03 |
|
BR-10-20 |
268 |
270 |
2 |
0.0138 |
0.0007 |
0.005 |
<0.5 |
0.0023 |
0.046 |
|
BR-10-20 |
270 |
272 |
2 |
0.0223 |
0.001 |
<0.005 |
<0.5 |
0.0007 |
0.015 |
|
BR-10-20 |
272 |
273.4 |
1.4 |
0.0146 |
0.0008 |
<0.005 |
<0.5 |
0.0003 |
0.015 |
|
BR-10-20 |
273.4 |
275 |
1.6 |
0.0113 |
0.0007 |
<0.005 |
<0.5 |
0.0005 |
0.046 |
|
BR-10-20 |
275 |
277 |
2 |
0.0106 |
0.0012 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-10-20 |
277 |
279 |
2 |
0.0093 |
0.0008 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-10-20 |
279 |
281 |
2 |
0.0109 |
0.0004 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-10-20 |
281 |
283 |
2 |
0.0111 |
0.0004 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-10-20 |
283 |
283.8 |
0.8 |
0.0106 |
0.0008 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-10-20 |
283.8 |
285 |
1.2 |
0.0123 |
0.0005 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-10-20 |
285 |
287 |
2 |
0.0082 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.122 |
|
BR-10-20 |
287 |
289 |
2 |
0.0073 |
0.001 |
<0.005 |
<0.5 |
0.0017 |
0.38 |
|
BR-10-20 |
289 |
291 |
2 |
0.0241 |
0.0017 |
0.007 |
<0.5 |
0.0003 |
0.122 |
|
BR-10-20 |
291 |
293 |
2 |
0.0192 |
0.0098 |
0.048 |
1.6 |
0.0045 |
0.274 |
|
BR-10-20 |
293 |
294 |
1 |
0.014 |
0.0107 |
0.037 |
1.3 |
0.0023 |
0.289 |
|
BR-10-20 |
294 |
295 |
1 |
0.0133 |
0.0056 |
0.013 |
0.7 |
0.0046 |
0.152 |
|
BR-10-20 |
295 |
296 |
1 |
0.104 |
0.0503 |
0.068 |
3.1 |
0.0036 |
0.259 |
|
BR-10-20 |
296 |
297 |
1 |
0.0526 |
0.0683 |
0.033 |
4.5 |
0.0078 |
0.243 |
|
BR-10-20 |
297 |
298 |
1 |
0.262 |
0.18 |
0.112 |
7.9 |
0.0121 |
0.046 |
|
BR-10-20 |
298 |
299 |
1 |
0.331 |
0.124 |
0.174 |
8.6 |
0.0139 |
0.183 |
|
BR-10-20 |
299 |
300 |
1 |
0.191 |
0.0993 |
0.066 |
3.7 |
0.0054 |
0.137 |
|
BR-10-20 |
300 |
301 |
1 |
0.0702 |
0.0156 |
0.071 |
2.8 |
0.0032 |
0.076 |
|
BR-10-20 |
301 |
302 |
1 |
0.373 |
0.079 |
0.122 |
3.2 |
0.0051 |
0.152 |
|
BR-10-20 |
302 |
303 |
1 |
0.0253 |
0.0047 |
0.024 |
1.3 |
0.0008 |
0.061 |
|
BR-10-20 |
303 |
304 |
1 |
0.159 |
0.251 |
0.085 |
4.5 |
0.0063 |
0.578 |
|
BR-10-20 |
304 |
305 |
1 |
0.235 |
0.135 |
0.049 |
3.5 |
0.0072 |
0.365 |
|
BR-10-20 |
305 |
306 |
1 |
0.254 |
0.345 |
0.106 |
6.4 |
0.0228 |
0.517 |
|
BR-10-20 |
306 |
307.2 |
1.2 |
0.0908 |
0.0632 |
0.078 |
2.9 |
0.0091 |
0.517 |
|
BR-10-20 |
307.2 |
308.4 |
1.2 |
0.135 |
0.0273 |
0.021 |
1.4 |
0.0009 |
0.198 |
|
BR-10-20 |
308.4 |
309.4 |
1 |
0.0472 |
0.0573 |
0.044 |
2.4 |
0.0015 |
0.882 |
|
BR-10-20 |
309.4 |
310.6 |
1.2 |
0.308 |
0.114 |
0.051 |
4 |
0.003 |
0.38 |
|
BR-10-20 |
310.6 |
311.7 |
1.1 |
0.132 |
0.0393 |
0.042 |
4.3 |
0.0049 |
0.289 |
|
BR-10-20 |
311.7 |
312.8 |
1.1 |
0.264 |
0.133 |
0.08 |
14 |
0.0191 |
0.943 |
|
BR-10-20 |
312.8 |
314 |
1.2 |
0.363 |
0.324 |
0.133 |
23 |
0.0344 |
1.978 |
|
BR-10-20 |
314 |
315 |
1 |
0.183 |
0.0626 |
0.08 |
5 |
0.0065 |
0.608 |
|
BR-10-20 |
315 |
316.2 |
1.2 |
0.127 |
0.0218 |
0.031 |
1.4 |
0.0019 |
0.106 |
|
BR-10-20 |
316.2 |
317.4 |
1.2 |
0.416 |
0.181 |
0.119 |
7.8 |
0.0217 |
0.35 |
|
BR-10-20 |
317.4 |
318.6 |
1.2 |
0.29 |
0.178 |
0.142 |
28.4 |
0.0907 |
0.152 |
|
BR-10-20 |
318.6 |
319.8 |
1.2 |
0.145 |
0.0964 |
0.138 |
12.7 |
0.0604 |
0.091 |
|
BR-10-20 |
319.8 |
321 |
1.2 |
0.599 |
0.608 |
0.195 |
14.4 |
0.0714 |
0.548 |
|
BR-10-20 |
321 |
322 |
1 |
0.742 |
0.432 |
0.319 |
18.1 |
0.0746 |
0.335 |
|
BR-10-20 |
322 |
323.2 |
1.2 |
0.478 |
0.224 |
0.161 |
6.3 |
0.015 |
0.593 |
|
BR-10-20 |
323.2 |
324 |
0.8 |
0.0914 |
0.0216 |
0.036 |
1.2 |
0.005 |
0.228 |
|
BR-10-20 |
324 |
325 |
1 |
0.0524 |
0.0238 |
0.063 |
1.1 |
0.0095 |
0.396 |
|
BR-10-20 |
325 |
326 |
1 |
0.101 |
0.0769 |
0.04 |
1.3 |
0.0045 |
0.685 |
|
BR-10-20 |
326 |
327 |
1 |
0.149 |
0.0196 |
0.058 |
0.7 |
0.0019 |
0.137 |
|
BR-10-20 |
327 |
328 |
1 |
0.127 |
0.0802 |
0.165 |
3.9 |
0.0501 |
0.608 |
|
BR-10-20 |
328 |
329 |
1 |
0.0658 |
0.0779 |
0.104 |
1.9 |
0.0155 |
0.274 |
|
BR-10-20 |
329 |
330 |
1 |
0.0294 |
0.0806 |
0.158 |
1.3 |
0.0086 |
0.076 |
|
BR-10-20 |
330 |
331 |
1 |
0.0714 |
0.0215 |
0.088 |
1 |
0.0051 |
0.091 |
|
BR-10-20 |
331 |
332 |
1 |
0.0487 |
0.071 |
0.075 |
1.6 |
0.0143 |
0.198 |
|
BR-10-20 |
332 |
333 |
1 |
0.0316 |
0.0447 |
0.058 |
1 |
0.0047 |
0.122 |
|
BR-10-20 |
333 |
334 |
1 |
0.211 |
0.317 |
0.322 |
6.9 |
0.108 |
1.4 |
|
BR-10-20 |
334 |
335 |
1 |
0.142 |
0.452 |
0.178 |
6.5 |
0.0792 |
0.487 |
|
BR-10-20 |
335 |
336 |
1 |
0.281 |
0.653 |
0.121 |
9 |
0.13 |
0.974 |
|
BR-10-20 |
336 |
337 |
1 |
0.0504 |
0.0131 |
0.051 |
<0.5 |
0.0014 |
0.152 |
|
BR-10-20 |
337 |
338 |
1 |
0.148 |
0.0659 |
0.081 |
1.4 |
0.0121 |
0.076 |
|
BR-10-20 |
338 |
339 |
1 |
0.249 |
0.453 |
1.655 |
7.9 |
0.112 |
0.091 |
|
BR-10-20 |
339 |
340 |
1 |
0.223 |
0.311 |
0.164 |
13.1 |
0.296 |
1.993 |
|
BR-10-20 |
340 |
341 |
1 |
0.264 |
0.213 |
0.29 |
3.8 |
0.0657 |
0.532 |
|
BR-10-20 |
341 |
342 |
1 |
0.028 |
0.0188 |
0.093 |
0.5 |
0.0073 |
0.091 |
|
BR-10-20 |
342 |
343.8 |
1.8 |
0.0086 |
0.0075 |
0.037 |
<0.5 |
0.0004 |
0.061 |
|
BR-10-20 |
343.8 |
345 |
1.2 |
0.0171 |
0.0623 |
0.025 |
0.6 |
0.0023 |
0.061 |
|
BR-10-20 |
345 |
347 |
2 |
0.0795 |
0.035 |
0.023 |
1.4 |
0.0067 |
0.259 |
|
BR-10-20 |
347 |
349 |
2 |
0.168 |
0.0828 |
0.007 |
2.7 |
0.0033 |
0.654 |
|
BR-10-20 |
349 |
351 |
2 |
0.0095 |
0.0013 |
<0.005 |
0.6 |
0.0028 |
0.532 |
|
BR-10-20 |
351 |
353 |
2 |
0.0085 |
0.0008 |
<0.005 |
<0.5 |
0.0003 |
0.152 |
|
BR-10-20 |
353 |
355 |
2 |
0.0104 |
0.0007 |
<0.005 |
<0.5 |
0.0005 |
0.198 |
|
BR-10-20 |
355 |
357 |
2 |
0.0096 |
0.0014 |
<0.005 |
0.8 |
0.0034 |
0.091 |
|
BR-10-20 |
357 |
359 |
2 |
0.0111 |
0.0015 |
<0.005 |
0.6 |
0.0014 |
0.198 |
|
BR-10-20 |
359 |
361 |
2 |
0.0099 |
0.0014 |
<0.005 |
1.4 |
0.0044 |
0.213 |
|
BR-10-20 |
361 |
363 |
2 |
0.0106 |
0.0012 |
<0.005 |
<0.5 |
0.0003 |
0.167 |
|
BR-10-20 |
363 |
365 |
2 |
0.011 |
0.0011 |
<0.005 |
<0.5 |
0.0005 |
0.122 |
|
BR-10-20 |
365 |
367 |
2 |
0.0114 |
0.002 |
<0.005 |
3.7 |
0.0093 |
0.228 |
|
BR-10-20 |
367 |
369 |
2 |
0.0118 |
0.0015 |
<0.005 |
1.4 |
0.004 |
0.274 |
|
BR-10-20 |
369 |
371 |
2 |
0.0124 |
0.0032 |
<0.005 |
0.9 |
0.0006 |
0.152 |
|
BR-10-20 |
371 |
373 |
2 |
0.0117 |
0.0013 |
<0.005 |
0.8 |
0.0005 |
0.152 |
|
BR-10-20 |
373 |
373.6 |
0.6 |
0.012 |
0.0051 |
<0.005 |
1.2 |
0.0005 |
0.243 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-11-20 |
0 |
1.8 |
1.8 |
0.0263 |
0.019 |
0.01 |
<0.5 |
0.0082 |
0.076 |
|
BR-11-20 |
1.8 |
3 |
1.2 |
0.0037 |
0.0015 |
<0.005 |
<0.5 |
0.0021 |
0.015 |
|
BR-11-20 |
3 |
5 |
2 |
0.0038 |
0.0015 |
<0.005 |
<0.5 |
0.0018 |
0.008 |
|
BR-11-20 |
5 |
6.5 |
1.5 |
No sample |
|||||
|
BR-11-20 |
6.5 |
8.1 |
1.6 |
0.006 |
0.0085 |
<0.005 |
<0.5 |
0.005 |
0.015 |
|
BR-11-20 |
8.1 |
10 |
1.9 |
0.0297 |
0.263 |
0.005 |
5.5 |
0.024 |
0.046 |
|
BR-11-20 |
10 |
11.3 |
1.3 |
0.0243 |
0.197 |
0.006 |
1.5 |
0.0102 |
0.076 |
|
BR-11-20 |
11.3 |
12.6 |
1.3 |
0.0138 |
0.0059 |
<0.005 |
<0.5 |
0.0006 |
0.03 |
|
BR-11-20 |
12.6 |
13.5 |
0.9 |
No sample |
|||||
|
BR-11-20 |
13.5 |
15 |
1.5 |
0.0103 |
0.0023 |
<0.005 |
<0.5 |
0.002 |
0.03 |
|
BR-11-20 |
15 |
15.7 |
0.7 |
0.011 |
0.0033 |
<0.005 |
<0.5 |
0.0017 |
0.015 |
|
BR-11-20 |
15.7 |
17 |
1.3 |
0.0121 |
0.0035 |
<0.005 |
<0.5 |
0.0019 |
0.015 |
|
BR-11-20 |
17 |
18.4 |
1.4 |
0.0122 |
0.0029 |
<0.005 |
<0.5 |
0.0005 |
0.015 |
|
BR-11-20 |
18.4 |
20 |
1.6 |
0.0075 |
0.0013 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-11-20 |
20 |
22 |
2 |
0.0122 |
0.0012 |
<0.005 |
<0.5 |
<0.0001 |
0.046 |
|
BR-11-20 |
22 |
24 |
2 |
0.0069 |
0.001 |
<0.005 |
<0.5 |
<0.0001 |
0.03 |
|
BR-11-20 |
24 |
26 |
2 |
0.0101 |
0.0045 |
0.007 |
<0.5 |
0.0057 |
0.015 |
|
BR-11-20 |
26 |
28 |
2 |
0.0085 |
0.0125 |
<0.005 |
<0.5 |
<0.005 |
0.03 |
|
BR-11-20 |
28 |
30 |
2 |
0.0101 |
0.0017 |
<0.005 |
<0.5 |
0.0003 |
0.03 |
|
BR-11-20 |
30 |
31 |
1 |
0.0099 |
0.0013 |
<0.005 |
<0.5 |
0.0003 |
0.015 |
|
BR-11-20 |
31 |
32.3 |
1.3 |
0.0093 |
0.0034 |
<0.005 |
<0.5 |
0.0035 |
0.015 |
|
BR-11-20 |
32.3 |
34 |
1.7 |
0.0107 |
0.0023 |
<0.005 |
<0.5 |
0.0002 |
0.076 |
|
BR-11-20 |
34 |
35.5 |
1.5 |
0.0113 |
0.0024 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-11-20 |
35.5 |
37 |
1.5 |
0.0121 |
0.0022 |
<0.005 |
<0.5 |
0.0063 |
0.03 |
|
BR-11-20 |
37 |
39 |
2 |
0.0172 |
0.0036 |
<0.005 |
<0.5 |
0.0003 |
0.106 |
|
BR-11-20 |
39 |
41 |
2 |
0.0147 |
0.0018 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-11-20 |
41 |
43 |
2 |
0.0129 |
0.002 |
<0.005 |
<0.5 |
<0.0001 |
0.061 |
|
BR-11-20 |
43 |
45 |
2 |
0.0123 |
0.0018 |
<0.005 |
<0.5 |
0.0009 |
0.046 |
|
BR-11-20 |
45 |
47 |
2 |
0.013 |
0.0015 |
<0.005 |
<0.5 |
0.0042 |
0.061 |
|
BR-11-20 |
47 |
49 |
2 |
0.0102 |
0.0015 |
<0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-11-20 |
49 |
50.2 |
1.2 |
0.0097 |
0.0011 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-11-20 |
50.2 |
52 |
1.8 |
0.0103 |
0.0011 |
<0.005 |
0.5 |
0.0002 |
0.061 |
|
BR-11-20 |
52 |
53 |
1 |
0.018 |
0.0015 |
<0.005 |
2 |
0.0017 |
0.137 |
|
BR-11-20 |
53 |
55 |
2 |
0.0094 |
0.0013 |
<0.005 |
<0.5 |
0.0004 |
0.122 |
|
BR-11-20 |
55 |
56.5 |
1.5 |
0.0095 |
0.0009 |
<0.005 |
<0.5 |
0.0002 |
0.076 |
|
BR-11-20 |
56.5 |
57.5 |
1 |
0.171 |
0.0336 |
<0.005 |
0.7 |
0.0035 |
0.091 |
|
BR-11-20 |
57.5 |
58.6 |
1.1 |
0.0917 |
0.0184 |
0.008 |
5 |
0.0022 |
0.837 |
|
BR-11-20 |
58.6 |
59.6 |
1 |
0.137 |
0.0436 |
0.043 |
18 |
0.0087 |
2.115 |
|
BR-11-20 |
59.6 |
60.6 |
1 |
0.371 |
0.13 |
0.078 |
134 |
0.002 |
12.368 |
|
BR-11-20 |
60.6 |
61.6 |
1 |
0.15 |
0.0949 |
0.057 |
27.2 |
0.0012 |
5.811 |
|
BR-11-20 |
61.6 |
62.2 |
0.6 |
0.115 |
0.0715 |
0.226 |
10.1 |
0.0385 |
15.669 |
|
BR-11-20 |
62.2 |
63.2 |
1 |
2.22 |
2.86 |
0.596 |
204 |
0.567 |
75.149 |
|
BR-11-20 |
63.2 |
64.2 |
1 |
1.145 |
1.18 |
0.534 |
120 |
1.07 |
86.559 |
|
BR-11-20 |
64.2 |
64.8 |
0.6 |
3.09 |
3.42 |
1.925 |
283 |
0.778 |
83.212 |
|
BR-11-20 |
64.8 |
65.6 |
0.8 |
0.0621 |
0.0913 |
0.093 |
9.6 |
0.0362 |
7.454 |
|
BR-11-20 |
65.6 |
65.9 |
0.3 |
4.42 |
3.76 |
1.165 |
303 |
0.582 |
81.082 |
|
BR-11-20 |
65.9 |
67 |
1.1 |
1.315 |
0.926 |
0.43 |
118 |
0.133 |
23.883 |
|
BR-11-20 |
67 |
68 |
1 |
0.0795 |
0.0599 |
0.028 |
1.4 |
0.0193 |
0.593 |
|
BR-11-20 |
68 |
68.5 |
0.5 |
0.0276 |
0.0558 |
0.028 |
0.8 |
0.0075 |
0.228 |
|
BR-11-20 |
68.5 |
69.2 |
0.7 |
0.0255 |
0.0544 |
0.042 |
0.5 |
0.0276 |
0.73 |
|
BR-11-20 |
69.2 |
71 |
1.8 |
0.0041 |
0.0015 |
<0.005 |
<0.5 |
0.001 |
0.03 |
|
BR-11-20 |
71 |
73 |
2 |
0.0062 |
0.0017 |
<0.005 |
<0.5 |
0.002 |
0.015 |
|
BR-11-20 |
73 |
75 |
2 |
0.0044 |
0.0012 |
<0.005 |
<0.5 |
0.0008 |
0.03 |
|
BR-11-20 |
75 |
76 |
1 |
0.0114 |
0.0036 |
<0.005 |
<0.5 |
0.008 |
0.015 |
|
BR-11-20 |
76 |
77.3 |
1.3 |
0.0116 |
0.0938 |
<0.005 |
<0.5 |
0.0397 |
0.046 |
|
BR-11-20 |
77.3 |
79 |
1.7 |
0.0041 |
0.0041 |
<0.005 |
<0.5 |
0.0029 |
0.046 |
|
BR-11-20 |
79 |
81 |
2 |
0.0041 |
0.0007 |
<0.005 |
<0.5 |
0.0021 |
0.015 |
|
BR-11-20 |
81 |
83 |
2 |
0.0061 |
0.0007 |
<0.005 |
<0.5 |
0.0018 |
0.015 |
|
BR-11-20 |
83 |
85 |
2 |
0.0037 |
0.0005 |
<0.005 |
<0.5 |
0.0018 |
0.015 |
|
BR-11-20 |
85 |
87 |
2 |
0.0053 |
<0.005 |
<0.005 |
<0.5 |
0.0019 |
0.015 |
|
BR-11-20 |
87 |
89 |
2 |
0.0074 |
0.0023 |
<0.005 |
<0.5 |
0.001 |
0.046 |
|
BR-11-20 |
89 |
91 |
2 |
0.0052 |
0.0017 |
0.006 |
<0.5 |
0.001 |
0.03 |
|
BR-11-20 |
91 |
93 |
2 |
0.0053 |
0.001 |
<0.005 |
<0.5 |
0.0017 |
0.046 |
|
BR-11-20 |
93 |
95 |
2 |
0.0065 |
0.002 |
<0.005 |
<0.5 |
0.002 |
0.046 |
|
BR-11-20 |
95 |
97 |
2 |
0.0077 |
0.0048 |
<0.005 |
<0.5 |
0.0029 |
0.015 |
|
BR-11-20 |
97 |
99 |
2 |
0.0062 |
0.0038 |
<0.005 |
<0.5 |
0.0019 |
0.259 |
|
BR-11-20 |
99 |
100 |
1 |
0.006 |
0.0037 |
<0.005 |
<0.5 |
0.0021 |
0.03 |
|
BR-11-20 |
100 |
102 |
2 |
0.0059 |
0.0017 |
<0.005 |
<0.5 |
0.0011 |
0.015 |
|
BR-11-20 |
102 |
104 |
2 |
0.0088 |
0.0018 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-11-20 |
104 |
106 |
2 |
0.009 |
0.0012 |
<0.005 |
<0.5 |
0.0014 |
0.03 |
|
BR-11-20 |
106 |
108 |
2 |
0.0052 |
0.0019 |
<0.005 |
<0.5 |
0.0016 |
0.03 |
|
BR-11-20 |
108 |
110 |
2 |
0.008 |
0.0021 |
<0.005 |
<0.5 |
0.0012 |
0.015 |
|
BR-11-20 |
110 |
112 |
2 |
0.0104 |
0.0016 |
<0.005 |
<0.5 |
0.0022 |
0.03 |
|
BR-11-20 |
112 |
114 |
2 |
0.0078 |
0.002 |
<0.005 |
<0.5 |
0.0013 |
0.03 |
|
BR-11-20 |
114 |
116 |
2 |
0.0074 |
0.002 |
<0.005 |
<0.5 |
0.0009 |
0.243 |
|
BR-11-20 |
116 |
118 |
2 |
0.0072 |
0.0027 |
<0.005 |
<0.5 |
0.0017 |
0.015 |
|
BR-11-20 |
118 |
120 |
2 |
0.0189 |
0.0014 |
<0.005 |
<0.5 |
0.0011 |
0.183 |
|
BR-11-20 |
120 |
122 |
2 |
0.0107 |
0.0021 |
<0.005 |
<0.5 |
0.0013 |
0.03 |
|
BR-11-20 |
122 |
123.8 |
1.8 |
0.0068 |
0.0063 |
<0.005 |
<0.5 |
0.0021 |
0.046 |
|
BR-11-20 |
123.8 |
125 |
1.2 |
0.006 |
0.0017 |
<0.005 |
<0.5 |
0.0046 |
0.03 |
|
BR-11-20 |
125 |
127 |
2 |
0.009 |
0.0022 |
0.008 |
<0.5 |
0.0031 |
0.015 |
|
BR-11-20 |
127 |
128.9 |
1.9 |
0.0336 |
0.0082 |
<0.005 |
<0.5 |
0.0042 |
0.091 |
|
BR-11-20 |
128.9 |
130.2 |
1.3 |
0.0109 |
0.0695 |
0.006 |
<0.5 |
0.0055 |
0.578 |
|
BR-11-20 |
130.2 |
132.2 |
2 |
0.0195 |
0.012 |
0.006 |
<0.5 |
0.0005 |
0.015 |
|
BR-11-20 |
132.2 |
134.2 |
2 |
0.0113 |
0.0103 |
<0.005 |
<0.5 |
0.0046 |
0.03 |
|
BR-11-20 |
134.2 |
135 |
0.8 |
0.0109 |
0.006 |
0.009 |
0.5 |
0.0039 |
0.198 |
|
BR-11-20 |
135 |
136 |
1 |
0.013 |
0.0106 |
<0.005 |
0.5 |
0.0032 |
0.046 |
|
BR-11-20 |
136 |
137 |
1 |
0.0096 |
0.03 |
0.005 |
0.5 |
0.0054 |
0.076 |
|
BR-11-20 |
137 |
138 |
1 |
0.0087 |
0.029 |
<0.005 |
<0.5 |
0.0044 |
0.076 |
|
BR-11-20 |
138 |
139 |
1 |
0.0063 |
0.0178 |
0.01 |
<0.5 |
0.0047 |
0.122 |
|
BR-11-20 |
139 |
140 |
1 |
0.01 |
0.0137 |
0.014 |
<0.5 |
0.0064 |
0.517 |
|
BR-11-20 |
140 |
141 |
1 |
0.0141 |
0.0511 |
0.008 |
<0.5 |
0.0167 |
0.152 |
|
BR-11-20 |
141 |
142.2 |
1.2 |
0.0216 |
0.0553 |
0.007 |
<0.5 |
0.0129 |
0.106 |
|
BR-11-20 |
142.2 |
143 |
0.8 |
0.0246 |
0.0212 |
<0.005 |
0.5 |
0.0027 |
0.411 |
|
BR-11-20 |
143 |
144 |
1 |
0.006 |
0.0032 |
<0.005 |
<0.5 |
0.0005 |
0.137 |
|
BR-11-20 |
144 |
145 |
1 |
0.0051 |
0.0033 |
<0.005 |
<0.5 |
0.0015 |
0.106 |
|
BR-11-20 |
145 |
146 |
1 |
0.0268 |
0.0051 |
<0.005 |
<0.5 |
0.0007 |
0.183 |
|
BR-11-20 |
146 |
146.8 |
0.8 |
0.0122 |
0.0047 |
<0.005 |
<0.5 |
0.0013 |
0.046 |
|
BR-11-20 |
146.8 |
147.3 |
0.5 |
0.0153 |
0.0026 |
<0.005 |
<0.5 |
0.0012 |
0.152 |
|
BR-11-20 |
147.3 |
148.5 |
1.2 |
0.0148 |
0.0021 |
0.007 |
<0.5 |
0.0014 |
0.046 |
|
BR-11-20 |
148.5 |
150.5 |
2 |
0.0104 |
0.0017 |
<0.005 |
<0.5 |
0.0005 |
0.061 |
|
BR-11-20 |
150.5 |
152.5 |
2 |
0.0093 |
0.0029 |
<0.005 |
<0.5 |
0.0026 |
0.046 |
|
BR-11-20 |
152.5 |
154 |
1.5 |
0.0235 |
0.0103 |
<0.005 |
<0.5 |
0.002 |
0.03 |
|
BR-11-20 |
154 |
156 |
2 |
0.0149 |
0.0043 |
<0.005 |
<0.5 |
0.0019 |
0.046 |
|
BR-11-20 |
156 |
158 |
2 |
0.01 |
0.0032 |
<0.005 |
<0.5 |
0.0012 |
0.046 |
|
BR-11-20 |
158 |
159 |
1 |
0.0077 |
0.003 |
<0.005 |
<0.5 |
0.0015 |
0.03 |
|
BR-11-20 |
159 |
161 |
2 |
0.0119 |
0.0019 |
<0.005 |
<0.5 |
0.0012 |
0.061 |
|
BR-11-20 |
161 |
163 |
2 |
0.0128 |
0.0035 |
<0.005 |
<0.5 |
0.0008 |
0.137 |
|
BR-11-20 |
163 |
163.7 |
0.7 |
0.0146 |
0.0018 |
<0.005 |
<0.5 |
0.0002 |
0.061 |
|
BR-11-20 |
163.7 |
165.4 |
1.7 |
0.0139 |
0.0027 |
<0.005 |
<0.5 |
0.0031 |
0.106 |
|
BR-11-20 |
165.4 |
167.4 |
2 |
0.008 |
0.0017 |
<0.005 |
<0.5 |
0.0019 |
0.243 |
|
BR-11-20 |
167.4 |
169.4 |
2 |
0.0079 |
0.0016 |
<0.005 |
<0.5 |
<0.005 |
0.137 |
|
BR-11-20 |
169.4 |
171 |
1.6 |
0.0077 |
0.0011 |
<0.005 |
<0.5 |
0.0034 |
0.061 |
|
BR-11-20 |
171 |
173 |
2 |
0.0068 |
0.001 |
<0.005 |
<0.5 |
0.0004 |
0.076 |
|
BR-11-20 |
173 |
175 |
2 |
0.0059 |
0.0007 |
<0.005 |
<0.5 |
0.0013 |
0.076 |
|
BR-11-20 |
175 |
177 |
2 |
0.0067 |
0.0009 |
<0.005 |
<0.5 |
0.0018 |
0.076 |
|
BR-11-20 |
177 |
179 |
2 |
0.0062 |
0.0012 |
<0.005 |
<0.5 |
0.0012 |
0.091 |
|
BR-11-20 |
179 |
181 |
2 |
0.0052 |
0.0012 |
0.005 |
<0.5 |
0.0014 |
0.061 |
|
BR-11-20 |
181 |
182 |
1 |
0.0121 |
0.0058 |
0.017 |
<0.5 |
0.0028 |
0.061 |
|
BR-11-20 |
182 |
183 |
1 |
0.0059 |
0.0036 |
0.013 |
<0.5 |
0.0007 |
0.061 |
|
BR-11-20 |
183 |
184 |
1 |
0.0075 |
0.0009 |
0.005 |
<0.5 |
0.0018 |
0.213 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-12-20 |
0 |
1 |
1 |
0.0099 |
0.0053 |
<0.005 |
<0.5 |
0.0109 |
0.046 |
|
BR-12-20 |
1 |
2.6 |
1.6 |
0.0095 |
0.0018 |
<0.005 |
<0.5 |
0.0074 |
0.03 |
|
BR-12-20 |
2.6 |
3.1 |
0.5 |
No sample |
|||||
|
BR-12-20 |
3.1 |
5 |
1.9 |
0.0085 |
0.0021 |
0.005 |
<0.5 |
0.0073 |
0.046 |
|
BR-12-20 |
5 |
7 |
2 |
0.0101 |
0.0018 |
0.006 |
<0.5 |
0.0107 |
0.046 |
|
BR-12-20 |
7 |
9.6 |
2.6 |
No sample |
|||||
|
BR-12-20 |
9.6 |
10.4 |
0.8 |
0.0088 |
0.0016 |
0.007 |
<0.5 |
0.0058 |
0.03 |
|
BR-12-20 |
10.4 |
12 |
1.6 |
0.0076 |
0.0042 |
0.005 |
<0.5 |
0.0038 |
0.046 |
|
BR-12-20 |
12 |
12.1 |
0.1 |
No sample |
|||||
|
BR-12-20 |
12.1 |
14 |
1.9 |
0.0079 |
0.0044 |
0.005 |
<0.5 |
0.0045 |
0.03 |
|
BR-12-20 |
14 |
17.8 |
3.8 |
No sample |
|||||
|
BR-12-20 |
17.8 |
19.8 |
2 |
0.0069 |
0.002 |
0.006 |
<0.5 |
0.0075 |
0.03 |
|
BR-12-20 |
19.8 |
21.5 |
1.7 |
0.0068 |
0.0018 |
0.008 |
<0.5 |
0.0077 |
0.015 |
|
BR-12-20 |
21.5 |
24.3 |
2.8 |
No sample |
|||||
|
BR-12-20 |
24.3 |
25.3 |
1 |
0.0056 |
0.0012 |
0.022 |
<0.5 |
0.006 |
0.015 |
|
BR-12-20 |
25.3 |
25.8 |
0.5 |
0.0081 |
0.0018 |
0.013 |
<0.5 |
0.01 |
0.03 |
|
BR-12-20 |
25.8 |
31 |
5.2 |
No sample |
|||||
|
BR-12-20 |
31 |
33 |
2 |
0.0103 |
0.0034 |
0.008 |
<0.5 |
0.0063 |
0.015 |
|
BR-12-20 |
33 |
35 |
2 |
0.0096 |
0.0048 |
0.009 |
<0.5 |
0.0087 |
0.015 |
|
BR-12-20 |
35 |
37 |
2 |
0.0099 |
0.0016 |
0.01 |
<0.5 |
0.0072 |
0.03 |
|
BR-12-20 |
37 |
38.6 |
1.6 |
0.008 |
0.0029 |
0.005 |
<0.5 |
0.0055 |
0.015 |
|
BR-12-20 |
38.6 |
40 |
1.4 |
0.0038 |
0.0009 |
<0.005 |
<0.5 |
<0.005 |
0.015 |
|
BR-12-20 |
40 |
41.8 |
1.8 |
0.0086 |
0.0017 |
<0.005 |
<0.5 |
0.0015 |
0.046 |
|
BR-12-20 |
41.8 |
42.6 |
0.8 |
0.0106 |
0.0024 |
<0.005 |
<0.5 |
0.0013 |
0.046 |
|
BR-12-20 |
42.6 |
45.7 |
3.1 |
No sample |
|||||
|
BR-12-20 |
45.7 |
47.2 |
1.5 |
0.0156 |
0.0058 |
<0.005 |
<0.5 |
0.0015 |
0.076 |
|
BR-12-20 |
47.2 |
47.7 |
0.5 |
No sample |
|||||
|
BR-12-20 |
47.7 |
49 |
1.3 |
0.0109 |
0.0022 |
<0.005 |
<0.5 |
0.001 |
0.015 |
|
BR-12-20 |
49 |
50.2 |
1.2 |
0.0067 |
0.0089 |
<0.005 |
<0.5 |
0.002 |
0.015 |
|
BR-12-20 |
50.2 |
51.4 |
1.2 |
0.002 |
0.0085 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-12-20 |
51.4 |
59.5 |
8.1 |
No sample |
|||||
|
BR-12-20 |
59.5 |
60.7 |
1.2 |
0.0109 |
0.0035 |
<0.005 |
<0.5 |
0.0004 |
0.03 |
|
BR-12-20 |
60.7 |
62.5 |
1.8 |
0.0113 |
0.0062 |
<0.005 |
<0.5 |
0.0016 |
0.061 |
|
BR-12-20 |
62.5 |
64 |
1.5 |
0.0098 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-12-20 |
64 |
66 |
2 |
0.01 |
0.001 |
<0.005 |
<0.5 |
0.0048 |
0.061 |
|
BR-12-20 |
66 |
68 |
2 |
0.0097 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-12-20 |
68 |
70 |
2 |
0.0095 |
0.0015 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-12-20 |
70 |
72 |
2 |
0.0098 |
0.0012 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-12-20 |
72 |
74 |
2 |
0.0112 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-12-20 |
74 |
76 |
2 |
0.0156 |
0.0012 |
<0.005 |
0.6 |
0.0041 |
0.061 |
|
BR-12-20 |
76 |
78 |
2 |
0.017 |
0.0006 |
<0.005 |
<0.5 |
0.0023 |
0.046 |
|
BR-12-20 |
78 |
80 |
2 |
0.0161 |
0.0011 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-12-20 |
80 |
82 |
2 |
0.0164 |
0.0009 |
<0.005 |
1.9 |
0.0076 |
0.061 |
|
BR-12-20 |
82 |
84 |
2 |
0.0162 |
0.0012 |
<0.005 |
0.6 |
0.0028 |
0.061 |
|
BR-12-20 |
84 |
86 |
2 |
0.0127 |
0.0016 |
<0.005 |
1.4 |
0.0062 |
0.091 |
|
BR-12-20 |
86 |
88 |
2 |
0.0092 |
0.0012 |
<0.005 |
<0.5 |
0.0003 |
0.061 |
|
BR-12-20 |
88 |
90 |
2 |
0.0086 |
0.0012 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-12-20 |
90 |
92 |
2 |
0.0079 |
0.0013 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-12-20 |
92 |
94 |
2 |
0.009 |
0.001 |
<0.005 |
<0.5 |
0.0008 |
0.061 |
|
BR-12-20 |
94 |
96 |
2 |
0.0127 |
0.001 |
<0.005 |
<0.5 |
0.0006 |
0.122 |
|
BR-12-20 |
96 |
98 |
2 |
0.01 |
0.0013 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-12-20 |
98 |
100 |
2 |
0.0115 |
0.0014 |
<0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-12-20 |
100 |
102 |
2 |
0.0123 |
0.001 |
<0.005 |
2.8 |
0.0027 |
0.167 |
|
BR-12-20 |
102 |
102.7 |
0.7 |
0.0142 |
0.0012 |
<0.005 |
13.6 |
0.0134 |
0.091 |
|
BR-12-20 |
102.7 |
103.5 |
0.8 |
0.208 |
0.0242 |
0.005 |
6.4 |
0.0041 |
1.978 |
|
BR-12-20 |
103.5 |
104.5 |
1 |
0.1805 |
0.0276 |
0.033 |
14.6 |
0.0016 |
3.24 |
|
BR-12-20 |
104.5 |
105.5 |
1 |
0.511 |
0.257 |
0.037 |
13.9 |
0.0059 |
1.217 |
|
BR-12-20 |
105.5 |
106.5 |
1 |
0.0863 |
0.0153 |
0.013 |
1.1 |
0.0028 |
0.38 |
|
BR-12-20 |
106.5 |
107.5 |
1 |
0.0578 |
0.0113 |
0.009 |
2.1 |
0.0029 |
2.54 |
|
BR-12-20 |
107.5 |
108.5 |
1 |
0.047 |
0.0089 |
<0.005 |
3.9 |
0.0006 |
0.867 |
|
BR-12-20 |
108.5 |
109 |
0.5 |
0.1425 |
0.103 |
0.006 |
65.7 |
0.0061 |
0.35 |
|
BR-12-20 |
109 |
109.7 |
0.7 |
0.1685 |
0.0647 |
0.009 |
34.6 |
0.0034 |
0.335 |
|
BR-12-20 |
109.7 |
110.5 |
0.8 |
0.0117 |
0.011 |
0.028 |
1.9 |
0.0018 |
1.46 |
|
BR-12-20 |
110.5 |
111.5 |
1 |
0.1185 |
0.446 |
0.059 |
8.4 |
0.0491 |
3.499 |
|
BR-12-20 |
111.5 |
112.5 |
1 |
0.376 |
0.165 |
0.2 |
6.8 |
0.0213 |
3.636 |
|
BR-12-20 |
112.5 |
113.5 |
1 |
0.683 |
0.339 |
0.3 |
31 |
0.131 |
6.587 |
|
BR-12-20 |
113.5 |
114 |
0.5 |
4.75 |
3.78 |
1.455 |
220 |
0.549 |
70.89 |
|
BR-12-20 |
114 |
114.7 |
0.7 |
11.6 |
6.39 |
2.56 |
520 |
0.59 |
69.216 |
|
BR-12-20 |
114.7 |
116.4 |
1.7 |
1.53 |
2.12 |
0.717 |
104 |
0.0878 |
4.822 |
|
BR-12-20 |
116.4 |
118.4 |
2 |
0.016 |
0.0174 |
0.005 |
<0.5 |
0.0038 |
0.563 |
|
BR-12-20 |
118.4 |
118.9 |
0.5 |
No sample |
|||||
|
BR-12-20 |
118.9 |
120.8 |
1.9 |
0.0755 |
0.0649 |
0.005 |
<0.5 |
0.0077 |
0.152 |
|
BR-12-20 |
120.8 |
122.8 |
2 |
0.0239 |
0.0157 |
0.01 |
<0.5 |
0.0177 |
0.046 |
|
BR-12-20 |
122.8 |
124.5 |
1.7 |
0.0063 |
0.0035 |
<0.005 |
<0.5 |
0.0014 |
0.046 |
|
BR-12-20 |
124.5 |
126.5 |
2 |
0.0075 |
0.003 |
<0.005 |
<0.5 |
0.0015 |
0.03 |
|
BR-12-20 |
126.5 |
128.5 |
2 |
0.0091 |
0.0038 |
0.005 |
<0.5 |
0.0018 |
0.03 |
|
BR-12-20 |
128.5 |
130.1 |
1.6 |
0.0096 |
0.0036 |
<0.005 |
<0.5 |
0.0013 |
0.03 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-13-20 |
0 |
1.5 |
1.5 |
0.0095 |
0.0024 |
0.006 |
<0.5 |
0.0074 |
0.061 |
|
BR-13-20 |
1.5 |
4.8 |
3.3 |
No sample |
|||||
|
BR-13-20 |
4.8 |
6.7 |
1.9 |
0.0094 |
0.0021 |
0.005 |
<0.5 |
0.0053 |
0.046 |
|
BR-13-20 |
6.7 |
8.2 |
1.5 |
0.0105 |
0.0027 |
<0.005 |
<0.5 |
0.0066 |
0.046 |
|
BR-13-20 |
8.2 |
10.2 |
2 |
0.0097 |
0.0014 |
<0.005 |
<0.5 |
0.0066 |
0.046 |
|
BR-13-20 |
10.2 |
12.2 |
2 |
0.0099 |
0.0017 |
0.005 |
<0.5 |
0.0064 |
0.046 |
|
BR-13-20 |
12.2 |
14.2 |
2 |
0.0113 |
0.0026 |
0.006 |
<0.5 |
0.0077 |
0.091 |
|
BR-13-20 |
14.2 |
16.2 |
2 |
0.0073 |
0.002 |
<0.005 |
<0.5 |
0.007 |
0.03 |
|
BR-13-20 |
16.2 |
18.2 |
2 |
0.0085 |
0.0019 |
0.007 |
<0.5 |
0.0047 |
0.046 |
|
BR-13-20 |
18.2 |
19.8 |
1.6 |
0.0031 |
0.0013 |
<0.005 |
<0.5 |
0.0016 |
0.015 |
|
BR-13-20 |
19.8 |
21.8 |
2 |
0.0035 |
0.001 |
<0.005 |
<0.5 |
0.0018 |
0.015 |
|
BR-13-20 |
21.8 |
23.7 |
1.9 |
0.0066 |
0.0013 |
0.005 |
<0.5 |
0.0062 |
0.015 |
|
BR-13-20 |
23.7 |
25.7 |
2 |
0.0067 |
0.0023 |
0.006 |
<0.5 |
0.005 |
0.015 |
|
BR-13-20 |
25.7 |
27.2 |
1.5 |
0.0169 |
0.0204 |
0.01 |
<0.5 |
0.0089 |
0.03 |
|
BR-13-20 |
27.2 |
28.2 |
1 |
0.0284 |
0.0559 |
0.015 |
<0.5 |
0.0119 |
0.03 |
|
BR-13-20 |
28.2 |
30 |
1.8 |
0.0113 |
0.0078 |
0.012 |
<0.5 |
0.0103 |
0.091 |
|
BR-13-20 |
30 |
32 |
2 |
0.007 |
0.0024 |
0.009 |
<0.5 |
0.007 |
0.015 |
|
BR-13-20 |
32 |
34 |
2 |
0.0084 |
0.0022 |
0.009 |
<0.5 |
0.0076 |
0.03 |
|
BR-13-20 |
34 |
36 |
2 |
0.0104 |
0.0023 |
0.017 |
<0.5 |
0.0079 |
0.03 |
|
BR-13-20 |
36 |
38 |
2 |
0.0075 |
0.0026 |
0.011 |
<0.5 |
0.0066 |
0.015 |
|
BR-13-20 |
38 |
40 |
2 |
0.0084 |
0.0022 |
<0.005 |
<0.5 |
0.0049 |
0.03 |
|
BR-13-20 |
40 |
42 |
2 |
0.0056 |
0.002 |
<0.005 |
<0.5 |
0.0036 |
0.061 |
|
BR-13-20 |
42 |
44 |
2 |
0.0089 |
0.0038 |
<0.005 |
<0.5 |
0.0058 |
0.03 |
|
BR-13-20 |
44 |
44.9 |
0.9 |
0.0095 |
0.0075 |
<0.005 |
<0.5 |
0.0027 |
0.015 |
|
BR-13-20 |
44.9 |
46.9 |
2 |
0.0064 |
0.0039 |
<0.005 |
<0.5 |
0.0015 |
0.03 |
|
BR-13-20 |
46.9 |
48.3 |
1.4 |
0.0067 |
0.0054 |
<0.005 |
<0.5 |
0.001 |
0.03 |
|
BR-13-20 |
48.3 |
49.5 |
1.2 |
0.0099 |
0.0022 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-13-20 |
49.5 |
50.6 |
1.1 |
0.015 |
0.0027 |
<0.005 |
<0.5 |
0.0015 |
0.015 |
|
BR-13-20 |
50.6 |
52.6 |
2 |
0.007 |
0.0009 |
<0.005 |
<0.5 |
0.0013 |
0.03 |
|
BR-13-20 |
52.6 |
54.6 |
2 |
0.0114 |
0.0018 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-13-20 |
54.6 |
56.6 |
2 |
0.0138 |
0.005 |
0.006 |
<0.5 |
0.0029 |
0.03 |
|
BR-13-20 |
56.6 |
57.3 |
0.7 |
0.0119 |
0.0017 |
<0.005 |
<0.5 |
0.0012 |
0.046 |
|
BR-13-20 |
57.3 |
59 |
1.7 |
0.0105 |
0.0011 |
<0.005 |
<0.5 |
0.0012 |
0.061 |
|
BR-13-20 |
59 |
60.5 |
1.5 |
0.0129 |
0.002 |
<0.005 |
<0.5 |
0.0036 |
0.046 |
|
BR-13-20 |
60.5 |
62.5 |
2 |
0.0118 |
0.003 |
<0.005 |
<0.5 |
0.0015 |
0.046 |
|
BR-13-20 |
62.5 |
64.5 |
2 |
0.0138 |
0.0019 |
<0.005 |
<0.5 |
0.0044 |
0.061 |
|
BR-13-20 |
64.5 |
66.5 |
2 |
0.0121 |
0.0009 |
<0.005 |
<0.5 |
0.0011 |
0.152 |
|
BR-13-20 |
66.5 |
68.5 |
2 |
0.0182 |
0.0088 |
<0.005 |
4.4 |
0.0033 |
0.243 |
|
BR-13-20 |
68.5 |
70 |
1.5 |
0.0108 |
0.0013 |
<0.005 |
0.8 |
0.0006 |
0.502 |
|
BR-13-20 |
70 |
70.9 |
0.9 |
0.0101 |
0.0014 |
<0.005 |
0.9 |
0.0013 |
0.046 |
|
BR-13-20 |
70.9 |
72 |
1.1 |
0.0067 |
0.0058 |
<0.005 |
3 |
0.0021 |
0.122 |
|
BR-13-20 |
72 |
74 |
2 |
0.0114 |
0.0014 |
<0.005 |
1.7 |
0.0019 |
0.122 |
|
BR-13-20 |
74 |
76 |
2 |
0.0086 |
0.0163 |
<0.005 |
5.4 |
0.0018 |
0.624 |
|
BR-13-20 |
76 |
77 |
1 |
0.0054 |
0.0036 |
<0.005 |
1.1 |
0.0008 |
0.289 |
|
BR-13-20 |
77 |
78.1 |
1.1 |
0.0064 |
0.0024 |
<0.005 |
5.1 |
0.002 |
0.228 |
|
BR-13-20 |
78.1 |
80 |
1.9 |
0.0084 |
0.0008 |
0.007 |
16.6 |
0.0036 |
0.304 |
|
BR-13-20 |
80 |
82 |
2 |
0.0153 |
0.0041 |
0.006 |
5.4 |
0.0015 |
0.502 |
|
BR-13-20 |
82 |
84 |
2 |
0.0173 |
0.0067 |
<0.005 |
23 |
0.0048 |
0.213 |
|
BR-13-20 |
84 |
86 |
2 |
0.0105 |
0.0015 |
<0.005 |
2.2 |
0.0008 |
0.639 |
|
BR-13-20 |
86 |
87 |
1 |
0.0099 |
0.0009 |
<0.005 |
<0.5 |
0.0005 |
0.456 |
|
BR-13-20 |
87 |
88.4 |
1.4 |
0.0091 |
0.0012 |
<0.005 |
1 |
0.001 |
1.293 |
|
BR-13-20 |
88.4 |
90 |
1.6 |
0.0092 |
0.0035 |
<0.005 |
2.4 |
0.0014 |
0.167 |
|
BR-13-20 |
90 |
92 |
2 |
0.0072 |
0.0033 |
<0.005 |
3.1 |
0.0022 |
0.122 |
|
BR-13-20 |
92 |
94 |
2 |
0.0098 |
0.0009 |
<0.005 |
0.5 |
0.0004 |
0.243 |
|
BR-13-20 |
94 |
96 |
2 |
0.0091 |
0.0013 |
<0.005 |
2 |
0.0014 |
1.947 |
|
BR-13-20 |
96 |
96.8 |
0.8 |
0.0455 |
0.0185 |
<0.005 |
8.3 |
0.0029 |
2.54 |
|
BR-13-20 |
96.8 |
98 |
1.2 |
0.0123 |
0.0066 |
<0.005 |
3.3 |
0.0015 |
0.441 |
|
BR-13-20 |
98 |
99.1 |
1.1 |
0.0205 |
0.0096 |
<0.005 |
9.3 |
0.0023 |
0.183 |
|
BR-13-20 |
99.1 |
100.6 |
1.5 |
0.0291 |
0.0167 |
<0.005 |
26.6 |
0.0058 |
1.323 |
|
BR-13-20 |
100.6 |
102.1 |
1.5 |
0.0117 |
0.0064 |
<0.005 |
3.4 |
0.003 |
0.183 |
|
BR-13-20 |
102.1 |
104 |
1.9 |
0.0139 |
0.0013 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-13-20 |
104 |
106 |
2 |
0.0142 |
0.0013 |
<0.005 |
2.3 |
0.004 |
0.076 |
|
BR-13-20 |
106 |
108 |
2 |
0.0154 |
0.0012 |
<0.005 |
<0.5 |
0.0004 |
0.456 |
|
BR-13-20 |
108 |
110 |
2 |
0.0111 |
0.0011 |
<0.005 |
<0.5 |
0.0001 |
0.122 |
|
BR-13-20 |
110 |
112 |
2 |
0.01 |
0.0009 |
<0.005 |
<0.5 |
0.0002 |
0.183 |
|
BR-13-20 |
112 |
114 |
2 |
0.0096 |
0.0021 |
<0.005 |
2.2 |
0.0014 |
0.106 |
|
BR-13-20 |
114 |
116 |
2 |
0.0278 |
0.0159 |
<0.005 |
11.3 |
0.0107 |
0.624 |
|
BR-13-20 |
116 |
118 |
2 |
0.0198 |
0.0038 |
<0.005 |
2.3 |
0.003 |
0.167 |
|
BR-13-20 |
118 |
120 |
2 |
0.0091 |
0.0014 |
<0.005 |
2.2 |
0.0007 |
0.304 |
|
BR-13-20 |
120 |
121.65 |
1.65 |
0.0104 |
0.0035 |
0.009 |
3.5 |
0.0002 |
0.243 |
|
BR-13-20 |
121.65 |
122.5 |
0.85 |
0.125 |
0.0482 |
0.044 |
22.1 |
0.0033 |
2.343 |
|
BR-13-20 |
122.5 |
123.5 |
1 |
0.371 |
0.143 |
0.085 |
35.7 |
0.0067 |
3.134 |
|
BR-13-20 |
123.5 |
124.5 |
1 |
1.275 |
1.495 |
0.172 |
33.3 |
<0.53 |
1.384 |
|
BR-13-20 |
124.5 |
125.5 |
1 |
1.08 |
0.325 |
0.263 |
18.8 |
0.797 |
4.168 |
|
BR-13-20 |
125.5 |
126.5 |
1 |
1.28 |
0.377 |
0.532 |
23.5 |
1.105 |
0.882 |
|
BR-13-20 |
126.5 |
127 |
0.5 |
0.209 |
0.0229 |
0.296 |
2 |
0.0154 |
0.106 |
|
BR-13-20 |
127 |
127.5 |
0.5 |
0.1685 |
0.0049 |
0.076 |
0.5 |
0.002 |
0.532 |
|
BR-13-20 |
127.5 |
128.5 |
1 |
0.824 |
0.66 |
0.188 |
15.4 |
0.267 |
2.83 |
|
BR-13-20 |
128.5 |
129.5 |
1 |
12 |
8.32 |
1.29 |
160 |
2.02 |
1.171 |
|
BR-13-20 |
129.5 |
130.5 |
1 |
5.49 |
2.84 |
0.751 |
69.4 |
0.491 |
7.013 |
|
BR-13-20 |
130.5 |
131.5 |
1 |
0.65 |
0.502 |
0.36 |
25.3 |
0.116 |
6.648 |
|
BR-13-20 |
131.5 |
132.6 |
1.1 |
0.935 |
0.398 |
0.325 |
55 |
0.157 |
13.113 |
|
BR-13-20 |
132.6 |
133.7 |
1.1 |
1.075 |
0.392 |
0.21 |
22.5 |
0.29 |
15.441 |
|
BR-13-20 |
133.7 |
134 |
0.3 |
1.665 |
2.13 |
2.27 |
106 |
0.51 |
84.429 |
|
BR-13-20 |
134 |
134.9 |
0.9 |
1.905 |
2.23 |
3.18 |
174 |
0.584 |
84.277 |
|
BR-13-20 |
134.9 |
136 |
1.1 |
0.174 |
0.226 |
0.196 |
9.2 |
0.016 |
7.606 |
|
BR-13-20 |
136 |
137 |
1 |
0.287 |
0.176 |
0.028 |
11.3 |
0.0124 |
0.654 |
|
BR-13-20 |
137 |
138 |
1 |
0.286 |
0.101 |
0.014 |
10.3 |
0.0106 |
0.03 |
|
BR-13-20 |
138 |
139.1 |
1.1 |
0.37 |
0.26 |
0.012 |
9.4 |
0.0078 |
1.582 |
|
BR-13-20 |
139.1 |
141 |
1.9 |
0.0732 |
0.132 |
0.007 |
1 |
0.0039 |
1.171 |
|
BR-13-20 |
141 |
143 |
2 |
0.144 |
0.022 |
0.009 |
<0.5 |
0.0068 |
0.076 |
|
BR-13-20 |
143 |
145 |
2 |
0.0529 |
0.0265 |
0.018 |
<0.5 |
0.0093 |
0.03 |
|
BR-13-20 |
145 |
147 |
2 |
0.0128 |
0.0322 |
0.023 |
<0.5 |
0.012 |
0.061 |
|
BR-13-20 |
147 |
149 |
2 |
0.0265 |
0.0362 |
0.024 |
<0.5 |
0.008 |
0.03 |
|
BR-13-20 |
149 |
149.5 |
0.5 |
No sample |
|||||
|
BR-13-20 |
149.5 |
151.5 |
2 |
0.0229 |
0.0115 |
<0.005 |
<0.5 |
0.0035 |
0.03 |
|
BR-13-20 |
151.5 |
153.5 |
2 |
0.005 |
0.006 |
<0.005 |
<0.5 |
0.0017 |
0.03 |
|
BR-13-20 |
153.5 |
155.2 |
1.7 |
0.0083 |
0.0081 |
<0.005 |
<0.5 |
0.0007 |
0.03 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-17-20 |
0 |
118.8 |
No sample |
||||||
|
BR-17-20 |
118.8 |
119.8 |
1 |
0.261 |
0.342 |
0.017 |
2.6 |
0.026 |
0.213 |
|
BR-17-20 |
119.8 |
120.8 |
1 |
0.161 |
0.0628 |
<0.005 |
3 |
0.0046 |
0.015 |
|
BR-17-20 |
120.8 |
121.8 |
1 |
0.0132 |
0.0056 |
<0.005 |
<0.5 |
0.0004 |
0.015 |
|
BR-17-20 |
121.8 |
122.8 |
1 |
0.0247 |
0.0081 |
<0.005 |
<0.5 |
0.0009 |
0.015 |
|
BR-17-20 |
122.8 |
123.8 |
1 |
0.0276 |
0.0037 |
0.006 |
<0.5 |
0.0004 |
0.03 |
|
BR-17-20 |
123.8 |
124.8 |
1 |
0.0074 |
0.0017 |
<0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-17-20 |
124.8 |
125.8 |
1 |
0.0052 |
0.0016 |
<0.005 |
<0.5 |
0.0004 |
0.008 |
|
BR-17-20 |
125.8 |
126.5 |
0.7 |
0.343 |
0.0791 |
0.005 |
1.1 |
0.0035 |
0.015 |
|
BR-17-20 |
126.5 |
127 |
0.5 |
0.369 |
0.104 |
0.008 |
5.6 |
0.0074 |
0.015 |
|
BR-17-20 |
127 |
127.5 |
0.5 |
0.257 |
0.0508 |
0.006 |
6.8 |
0.0058 |
0.015 |
|
BR-17-20 |
127.5 |
128 |
0.5 |
0.123 |
0.0312 |
0.008 |
1.2 |
0.0021 |
0.015 |
|
BR-17-20 |
128 |
128.5 |
0.5 |
0.287 |
0.0628 |
0.007 |
<0.5 |
0.003 |
0.015 |
|
BR-17-20 |
128.5 |
129 |
0.5 |
0.102 |
0.159 |
0.009 |
4.9 |
0.0052 |
0.015 |
|
BR-17-20 |
129 |
129.5 |
0.5 |
0.138 |
0.0238 |
<0.005 |
2.6 |
0.0031 |
0.008 |
|
BR-17-20 |
129.5 |
130.5 |
1 |
0.029 |
0.0062 |
0.005 |
0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
130.5 |
131 |
0.5 |
0.0371 |
0.0329 |
<0.005 |
1 |
0.001 |
0.008 |
|
BR-17-20 |
131 |
132 |
1 |
0.0424 |
0.0646 |
0.006 |
0.9 |
0.0009 |
0.008 |
|
BR-17-20 |
132 |
133 |
1 |
0.0754 |
0.0806 |
0.013 |
0.9 |
0.0007 |
0.008 |
|
BR-17-20 |
133 |
133.5 |
0.5 |
0.019 |
0.0444 |
0.007 |
0.8 |
0.0006 |
0.008 |
|
BR-17-20 |
133.5 |
134 |
0.5 |
0.0151 |
0.0501 |
<0.005 |
<0.5 |
0.0005 |
0.008 |
|
BR-17-20 |
134 |
134.5 |
0.5 |
0.0074 |
0.0157 |
0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-17-20 |
134.5 |
135 |
0.5 |
0.0029 |
0.0096 |
<0.005 |
<0.5 |
0.0005 |
0.008 |
|
BR-17-20 |
135 |
136 |
1 |
0.0055 |
0.0086 |
<0.005 |
<0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
136 |
137 |
1 |
0.0029 |
0.0106 |
<0.005 |
<0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
137 |
138 |
1 |
0.0138 |
0.0073 |
<0.005 |
<0.5 |
0.0002 |
0.008 |
|
BR-17-20 |
138 |
139 |
1 |
0.02 |
0.0084 |
0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-17-20 |
139 |
140 |
1 |
0.0226 |
0.0105 |
<0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-17-20 |
140 |
141 |
1 |
0.0064 |
0.0079 |
0.038 |
<0.5 |
0.0001 |
0.015 |
|
BR-17-20 |
141 |
142 |
1 |
0.022 |
0.0449 |
0.02 |
1.4 |
0.0007 |
0.008 |
|
BR-17-20 |
142 |
143 |
1 |
0.0199 |
0.0464 |
<0.005 |
0.5 |
0.0004 |
0.008 |
|
BR-17-20 |
143 |
144 |
1 |
0.0205 |
0.0842 |
<0.005 |
<0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
144 |
145 |
1 |
0.0156 |
0.0529 |
<0.005 |
<0.5 |
0.0004 |
0.008 |
|
BR-17-20 |
145 |
146 |
1 |
0.0159 |
0.12 |
<0.005 |
0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
146 |
147 |
1 |
0.0181 |
0.0711 |
<0.005 |
<0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
147 |
148 |
1 |
0.011 |
0.0497 |
<0.005 |
<0.5 |
0.0002 |
0.015 |
|
BR-17-20 |
148 |
149 |
1 |
0.0132 |
0.12 |
<0.005 |
0.6 |
0.0004 |
0.076 |
|
BR-17-20 |
149 |
150 |
1 |
0.0039 |
0.1 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-17-20 |
150 |
151 |
1 |
0.0141 |
0.295 |
<0.005 |
1.1 |
0.0003 |
0.015 |
|
BR-17-20 |
151 |
152 |
1 |
0.0037 |
0.0534 |
0.006 |
<0.5 |
0.0002 |
0.015 |
|
BR-17-20 |
152 |
153 |
1 |
0.0273 |
0.026 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-17-20 |
153 |
154 |
1 |
0.0071 |
0.0058 |
0.005 |
<0.5 |
0.0001 |
0.008 |
|
BR-17-20 |
154 |
155 |
1 |
0.0033 |
0.0037 |
0.006 |
<0.5 |
0.0003 |
0.008 |
|
BR-17-20 |
155 |
156 |
1 |
0.0022 |
0.0011 |
<0.005 |
<0.5 |
0.0006 |
0.03 |
|
BR-17-20 |
156 |
157 |
1 |
<0.005 |
0.0004 |
<0.005 |
<0.5 |
0.0002 |
0.106 |
|
BR-17-20 |
157 |
158 |
1 |
0.0033 |
0.0004 |
0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-17-20 |
158 |
159 |
1 |
0.0041 |
0.0018 |
<0.005 |
<0.5 |
0.0016 |
0.03 |
|
BR-17-20 |
159 |
160 |
1 |
0.0084 |
0.0012 |
<0.005 |
<0.5 |
0.0003 |
0.015 |
|
BR-17-20 |
160 |
161 |
1 |
0.0086 |
0.0026 |
<0.005 |
<0.5 |
0.001 |
0.015 |
|
BR-17-20 |
161 |
162 |
1 |
0.0052 |
0.002 |
<0.005 |
<0.5 |
0.0021 |
0.03 |
|
BR-17-20 |
162 |
163 |
1 |
0.0038 |
0.0019 |
<0.005 |
<0.5 |
0.0007 |
0.015 |
|
BR-17-20 |
163 |
163.6 |
0.6 |
0.0028 |
0.0009 |
0.005 |
<0.5 |
0.0006 |
0.015 |
|
BR-17-20 |
163.6 |
164.5 |
0.9 |
0.012 |
0.0037 |
<0.005 |
<0.5 |
0.0038 |
0.03 |
|
BR-17-20 |
164.5 |
165.5 |
1 |
0.0106 |
0.0018 |
<0.005 |
<0.5 |
0.002 |
0.061 |
|
BR-17-20 |
165.5 |
166.5 |
1 |
0.01 |
0.002 |
<0.005 |
<0.5 |
0.0012 |
0.076 |
|
BR-17-20 |
166.5 |
167.5 |
1 |
0.0147 |
0.0036 |
<0.005 |
<0.5 |
0.0022 |
0.091 |
|
BR-17-20 |
167.5 |
168 |
0.5 |
0.0219 |
0.0124 |
<0.005 |
<0.5 |
0.013 |
0.061 |
|
BR-17-20 |
168 |
168.9 |
0.9 |
0.0134 |
0.0035 |
<0.005 |
<0.5 |
0.0013 |
0.061 |
|
BR-17-20 |
168.9 |
170.8 |
1.9 |
0.0123 |
<0.005 |
0.005 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
170.8 |
172.8 |
2 |
0.0128 |
0.0021 |
<0.005 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
172.8 |
174.8 |
2 |
0.0087 |
0.0065 |
<0.005 |
<0.5 |
0.0039 |
0.076 |
|
BR-17-20 |
174.8 |
176 |
1.2 |
0.0104 |
0.0016 |
<0.005 |
<0.5 |
0.0003 |
0.076 |
|
BR-17-20 |
176 |
178 |
2 |
0.0136 |
0.001 |
<0.005 |
<0.5 |
0.002 |
0.061 |
|
BR-17-20 |
178 |
179 |
1 |
0.013 |
0.0013 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-17-20 |
179 |
180.1 |
1.1 |
0.0134 |
0.001 |
<0.005 |
<0.5 |
0.0056 |
0.061 |
|
BR-17-20 |
180.1 |
182.1 |
2 |
0.0197 |
0.007 |
<0.005 |
<0.5 |
0.0015 |
0.73 |
|
BR-17-20 |
182.1 |
183 |
0.9 |
0.0398 |
0.0114 |
<0.005 |
<0.5 |
0.0022 |
0.061 |
|
BR-17-20 |
183 |
184 |
1 |
0.009 |
0.0033 |
<0.005 |
<0.5 |
0.002 |
0.411 |
|
BR-17-20 |
184 |
185 |
1 |
0.0099 |
0.0023 |
<0.005 |
0.9 |
0.0009 |
0.472 |
|
BR-17-20 |
185 |
186 |
1 |
0.0121 |
0.0073 |
0.011 |
1.7 |
0.0019 |
0.335 |
|
BR-17-20 |
186 |
187 |
1 |
0.0697 |
0.0267 |
0.015 |
19 |
0.0064 |
0.396 |
|
BR-17-20 |
187 |
188 |
1 |
0.013 |
0.0016 |
0.01 |
0.7 |
0.0004 |
0.198 |
|
BR-17-20 |
188 |
189 |
1 |
0.0149 |
0.0042 |
0.008 |
3.5 |
0.0017 |
0.548 |
|
BR-17-20 |
189 |
190 |
1 |
0.0092 |
0.0063 |
0.006 |
4.9 |
0.0011 |
0.806 |
|
BR-17-20 |
190 |
191 |
1 |
0.0219 |
0.017 |
0.021 |
6.7 |
0.0019 |
1.019 |
|
BR-17-20 |
191 |
192 |
1 |
0.38 |
0.261 |
0.027 |
49.6 |
0.0147 |
2.83 |
|
BR-17-20 |
192 |
192.9 |
0.9 |
0.0161 |
0.0252 |
0.018 |
4.2 |
0.0016 |
2.221 |
|
BR-17-20 |
192.9 |
193.5 |
0.6 |
1.67 |
0.288 |
0.966 |
279 |
0.585 |
36.206 |
|
BR-17-20 |
193.5 |
194 |
0.5 |
4.13 |
2.81 |
1.75 |
137 |
1.29 |
54.46 |
|
BR-17-20 |
194 |
194.5 |
0.5 |
2.23 |
0.754 |
2.01 |
124 |
0.324 |
38.944 |
|
BR-17-20 |
194.5 |
195 |
0.5 |
0.606 |
0.221 |
0.692 |
19.3 |
0.0881 |
11.546 |
|
BR-17-20 |
195 |
196 |
1 |
0.229 |
0.0482 |
0.157 |
4.5 |
0.0239 |
1.034 |
|
BR-17-20 |
196 |
196.5 |
0.5 |
0.226 |
0.0879 |
0.151 |
4 |
0.0407 |
3.59 |
|
BR-17-20 |
196.5 |
197 |
0.5 |
0.0818 |
0.0327 |
0.227 |
6.7 |
0.0211 |
0.578 |
|
BR-17-20 |
197 |
198 |
1 |
0.0633 |
0.0098 |
0.095 |
2.4 |
0.0058 |
0.532 |
|
BR-17-20 |
198 |
199 |
1 |
0.0993 |
0.0126 |
0.084 |
1.2 |
0.0035 |
0.106 |
|
BR-17-20 |
199 |
200 |
1 |
0.0483 |
0.0233 |
0.082 |
1.2 |
0.0047 |
0.061 |
|
BR-17-20 |
200 |
201 |
1 |
0.0182 |
0.0104 |
0.062 |
1.1 |
0.0021 |
0.046 |
|
BR-17-20 |
201 |
202 |
1 |
0.0127 |
0.0034 |
0.021 |
<0.5 |
0.001 |
0.03 |
|
BR-17-20 |
202 |
203 |
1 |
0.0333 |
0.0157 |
0.069 |
0.9 |
0.0065 |
0.806 |
|
BR-17-20 |
203 |
203.5 |
0.5 |
0.105 |
0.0455 |
0.077 |
0.9 |
0.0129 |
0.274 |
|
BR-17-20 |
203.5 |
204 |
0.5 |
0.043 |
0.0089 |
0.056 |
<0.5 |
0.0023 |
0.487 |
|
BR-17-20 |
204 |
204.5 |
0.5 |
1.315 |
0.414 |
0.883 |
112 |
0.235 |
19.852 |
|
BR-17-20 |
204.5 |
205 |
0.5 |
1.135 |
0.493 |
0.774 |
151 |
0.249 |
31.642 |
|
BR-17-20 |
205 |
205.5 |
0.5 |
0.734 |
0.322 |
0.682 |
79.2 |
0.0916 |
15.288 |
|
BR-17-20 |
205.5 |
206 |
0.5 |
4.21 |
2.05 |
1.21 |
223 |
0.506 |
36.966 |
|
BR-17-20 |
206 |
206.7 |
0.7 |
0.21 |
0.372 |
0.532 |
42.3 |
0.0483 |
4.503 |
|
BR-17-20 |
206.7 |
208 |
1.3 |
0.0053 |
0.0019 |
0.006 |
<0.5 |
0.001 |
0.076 |
|
BR-17-20 |
208 |
210 |
2 |
0.0039 |
0.0008 |
0.016 |
<0.5 |
0.0037 |
0.015 |
|
BR-17-20 |
210 |
212 |
2 |
0.0037 |
0.0008 |
<0.005 |
<0.5 |
0.0023 |
0.015 |
|
BR-17-20 |
212 |
214 |
2 |
0.0057 |
0.002 |
<0.005 |
<0.5 |
0.0024 |
0.03 |
|
BR-17-20 |
214 |
216 |
2 |
0.006 |
0.0017 |
0.01 |
<0.5 |
0.0018 |
0.015 |
|
BR-17-20 |
216 |
218 |
2 |
0.0036 |
0.0016 |
0.005 |
<0.5 |
0.0012 |
0.03 |
|
BR-17-20 |
218 |
220 |
2 |
0.0062 |
0.0017 |
<0.005 |
<0.5 |
0.0015 |
0.091 |
|
BR-17-20 |
220 |
222 |
2 |
0.008 |
0.0028 |
<0.005 |
<0.5 |
0.0512 |
0.106 |
|
BR-17-20 |
222 |
222.9 |
0.9 |
0.0123 |
0.0034 |
0.012 |
<0.5 |
0.0066 |
0.441 |
|
BR-17-20 |
222.9 |
223.5 |
0.6 |
0.243 |
0.302 |
0.028 |
1.1 |
0.031 |
1.308 |
|
BR-17-20 |
223.5 |
224 |
0.5 |
0.31 |
0.226 |
0.063 |
1.5 |
0.0259 |
1.354 |
|
BR-17-20 |
224 |
224.5 |
0.5 |
0.207 |
0.172 |
0.05 |
0.8 |
0.0246 |
0.73 |
|
BR-17-20 |
224.5 |
225 |
0.5 |
0.204 |
0.0557 |
0.038 |
1.1 |
0.0182 |
0.426 |
|
BR-17-20 |
225 |
225.5 |
0.5 |
0.0601 |
0.0244 |
0.033 |
1.8 |
0.0256 |
0.213 |
|
BR-17-20 |
225.5 |
226 |
0.5 |
0.0103 |
0.013 |
0.02 |
0.7 |
0.0091 |
0.517 |
|
BR-17-20 |
226 |
226.5 |
0.5 |
0.0164 |
0.012 |
0.01 |
0.6 |
0.0047 |
0.472 |
|
BR-17-20 |
226.5 |
227.2 |
0.7 |
0.0194 |
0.0654 |
0.015 |
0.6 |
0.0095 |
1.034 |
|
BR-17-20 |
227.2 |
228.9 |
1.7 |
0.0098 |
0.0063 |
0.007 |
<0.5 |
0.0164 |
0.761 |
|
BR-17-20 |
228.9 |
229.7 |
0.8 |
0.0701 |
0.15 |
0.03 |
0.6 |
0.025 |
11.637 |
|
BR-17-20 |
229.7 |
230.5 |
0.8 |
0.0823 |
0.231 |
0.231 |
9.1 |
0.0252 |
9.371 |
|
BR-17-20 |
230.5 |
231 |
0.5 |
8.63 |
6.12 |
3.12 |
341 |
0.334 |
38.335 |
|
BR-17-20 |
231 |
231.5 |
0.5 |
5.67 |
4.11 |
1.74 |
266 |
0.492 |
13.737 |
|
BR-17-20 |
231.5 |
232 |
0.5 |
1.515 |
2.26 |
1.36 |
67.4 |
0.383 |
7.226 |
|
BR-17-20 |
232 |
232.9 |
0.9 |
0.177 |
0.409 |
0.515 |
8.1 |
0.11 |
4.716 |
|
BR-17-20 |
232.9 |
234 |
1.1 |
0.0107 |
0.0149 |
0.052 |
13.3 |
0.0093 |
0.821 |
|
BR-17-20 |
234 |
235 |
1 |
0.0494 |
0.0177 |
0.054 |
18.1 |
0.003 |
1.156 |
|
BR-17-20 |
235 |
236 |
1 |
0.0829 |
0.0406 |
0.063 |
4.5 |
0.0015 |
<0.59 |
|
BR-17-20 |
236 |
237 |
1 |
0.0501 |
0.0315 |
0.036 |
3.2 |
0.0105 |
1.308 |
|
BR-17-20 |
237 |
237.8 |
0.8 |
0.278 |
0.0564 |
0.139 |
2.1 |
0.007 |
0.061 |
|
BR-17-20 |
237.8 |
238.8 |
1 |
0.266 |
0.453 |
0.396 |
22.2 |
0.0264 |
0.091 |
|
BR-17-20 |
238.8 |
239.8 |
1 |
0.502 |
0.213 |
0.14 |
9.5 |
0.013 |
0.061 |
|
BR-17-20 |
239.8 |
240.8 |
1 |
0.182 |
0.121 |
0.153 |
15.7 |
0.0299 |
0.03 |
|
BR-17-20 |
240.8 |
241.8 |
1 |
0.0401 |
0.013 |
0.104 |
5.1 |
0.0023 |
0.046 |
|
BR-17-20 |
241.8 |
242.5 |
0.7 |
0.127 |
0.0363 |
0.124 |
9.3 |
0.0046 |
0.046 |
|
BR-17-20 |
242.5 |
243 |
0.5 |
0.188 |
0.0829 |
0.137 |
10.2 |
0.0087 |
0.046 |
|
BR-17-20 |
243 |
243.5 |
0.5 |
0.417 |
0.43 |
0.207 |
140 |
0.0319 |
0.289 |
|
BR-17-20 |
243.5 |
244 |
0.5 |
0.225 |
0.141 |
0.189 |
130 |
0.0366 |
0.167 |
|
BR-17-20 |
244 |
244.5 |
0.5 |
0.719 |
0.349 |
0.233 |
124 |
0.0361 |
0.791 |
|
BR-17-20 |
244.5 |
245 |
0.5 |
1.05 |
0.498 |
0.313 |
262 |
0.0839 |
1.719 |
|
BR-17-20 |
245 |
245.5 |
0.5 |
0.203 |
0.0423 |
0.127 |
8.7 |
0.0026 |
0.152 |
|
BR-17-20 |
245.5 |
246 |
0.5 |
0.118 |
0.067 |
0.182 |
7.2 |
0.0037 |
0.106 |
|
BR-17-20 |
246 |
246.5 |
0.5 |
0.694 |
0.264 |
0.459 |
29 |
0.0174 |
2.297 |
|
BR-17-20 |
246.5 |
247 |
0.5 |
0.892 |
0.512 |
0.457 |
41.1 |
0.0229 |
1.004 |
|
BR-17-20 |
247 |
247.5 |
0.5 |
1.11 |
0.541 |
0.388 |
84.1 |
0.0446 |
1.491 |
|
BR-17-20 |
247.5 |
248 |
0.5 |
1.07 |
0.341 |
0.372 |
48.9 |
0.0291 |
0.791 |
|
BR-17-20 |
248 |
248.5 |
0.5 |
0.872 |
0.383 |
0.548 |
49.6 |
0.0354 |
0.259 |
|
BR-17-20 |
248.5 |
249 |
0.5 |
0.253 |
0.1005 |
0.423 |
12 |
0.0102 |
0.274 |
|
BR-17-20 |
249 |
249.5 |
0.5 |
0.595 |
0.1215 |
0.464 |
14.3 |
0.015 |
0.502 |
|
BR-17-20 |
249.5 |
250 |
0.5 |
1.415 |
0.699 |
0.42 |
49.7 |
0.0408 |
1.05 |
|
BR-17-20 |
250 |
250.5 |
0.5 |
2.11 |
0.855 |
0.427 |
79.1 |
0.0779 |
1.536 |
|
BR-17-20 |
250.5 |
251 |
0.5 |
0.852 |
0.404 |
0.462 |
25.8 |
0.0364 |
0.624 |
|
BR-17-20 |
251 |
252 |
1 |
0.97 |
0.53 |
0.498 |
32.6 |
0.0446 |
0.852 |
|
BR-17-20 |
252 |
253 |
1 |
0.568 |
0.319 |
0.295 |
13.2 |
0.022 |
0.898 |
|
BR-17-20 |
253 |
254 |
1 |
0.411 |
0.285 |
0.355 |
8.4 |
0.0245 |
0.7 |
|
BR-17-20 |
254 |
255 |
1 |
0.191 |
0.352 |
0.242 |
17.3 |
0.0233 |
0.837 |
|
BR-17-20 |
255 |
256 |
1 |
0.0438 |
0.672 |
0.338 |
29.7 |
0.0299 |
0.38 |
|
BR-17-20 |
256 |
257 |
1 |
0.735 |
0.426 |
0.275 |
19.9 |
0.0211 |
0.304 |
|
BR-17-20 |
257 |
258 |
1 |
0.325 |
0.146 |
0.267 |
4.2 |
0.0084 |
0.73 |
|
BR-17-20 |
258 |
259 |
1 |
0.125 |
0.0665 |
0.423 |
3.8 |
0.0056 |
0.076 |
|
BR-17-20 |
259 |
260 |
1 |
0.335 |
0.18 |
0.282 |
7 |
0.0241 |
0.076 |
|
BR-17-20 |
260 |
261 |
1 |
0.33 |
0.152 |
0.304 |
4.7 |
0.0108 |
0.046 |
|
BR-17-20 |
261 |
262 |
1 |
0.154 |
0.279 |
0.303 |
23.6 |
0.0642 |
0.365 |
|
BR-17-20 |
262 |
263 |
1 |
0.266 |
0.409 |
0.223 |
23.6 |
0.0378 |
0.198 |
|
BR-17-20 |
263 |
264 |
1 |
0.507 |
0.325 |
0.218 |
33.4 |
0.0493 |
0.213 |
|
BR-17-20 |
264 |
265 |
1 |
0.438 |
0.0966 |
0.145 |
4.1 |
0.0032 |
0.061 |
|
BR-17-20 |
265 |
266 |
1 |
0.219 |
0.218 |
0.138 |
17.1 |
0.023 |
0.137 |
|
BR-17-20 |
266 |
267 |
1 |
0.0992 |
0.165 |
0.163 |
12.7 |
0.0095 |
0.03 |
|
BR-17-20 |
267 |
268 |
1 |
0.185 |
0.0899 |
0.201 |
15 |
0.013 |
0.091 |
|
BR-17-20 |
268 |
269 |
1 |
0.429 |
0.206 |
0.233 |
21.6 |
0.0287 |
0.198 |
|
BR-17-20 |
269 |
270 |
1 |
2.93 |
1.61 |
0.537 |
137 |
0.202 |
0.791 |
|
BR-17-20 |
270 |
271 |
1 |
0.967 |
0.414 |
0.32 |
47.2 |
0.0566 |
0.167 |
|
BR-17-20 |
271 |
272 |
1 |
0.0682 |
0.0391 |
0.156 |
6.1 |
0.0071 |
0.106 |
|
BR-17-20 |
272 |
273 |
1 |
0.462 |
0.246 |
0.161 |
27.7 |
0.021 |
0.122 |
|
BR-17-20 |
273 |
274.2 |
1.2 |
<0.5 |
0.201 |
0.284 |
7.1 |
0.006 |
0.122 |
|
BR-17-20 |
274.2 |
274.4 |
0.2 |
No sample |
|||||
|
BR-17-20 |
274.4 |
275 |
0.6 |
0.381 |
0.1405 |
0.081 |
5.9 |
0.0093 |
0.046 |
|
BR-17-20 |
275 |
276 |
1 |
0.144 |
0.05 |
0.041 |
1.1 |
0.0033 |
0.03 |
|
BR-17-20 |
276 |
277 |
1 |
0.234 |
0.078 |
0.057 |
6.6 |
0.0209 |
0.03 |
|
BR-17-20 |
277 |
278 |
1 |
0.241 |
0.0252 |
0.069 |
1.8 |
0.0051 |
0.03 |
|
BR-17-20 |
278 |
279 |
1 |
0.129 |
0.0637 |
0.086 |
1.2 |
0.0041 |
0.046 |
|
BR-17-20 |
279 |
280 |
1 |
0.0951 |
0.0139 |
0.05 |
0.8 |
<0.005 |
0.046 |
|
BR-17-20 |
280 |
281 |
1 |
0.0182 |
0.0105 |
0.039 |
<0.5 |
0.0017 |
0.046 |
|
BR-17-20 |
281 |
282 |
1 |
0.007 |
0.0114 |
0.06 |
<0.5 |
0.0013 |
0.198 |
|
BR-17-20 |
282 |
283 |
1 |
0.0066 |
0.0077 |
0.092 |
<0.5 |
0.002 |
0.061 |
|
BR-17-20 |
283 |
284 |
1 |
0.044 |
0.0295 |
0.104 |
2.1 |
0.0048 |
0.122 |
|
BR-17-20 |
284 |
285 |
1 |
0.31 |
0.252 |
0.086 |
21.5 |
0.0463 |
0.913 |
|
BR-17-20 |
285 |
286 |
1 |
0.424 |
0.174 |
0.064 |
14.8 |
0.0328 |
0.152 |
|
BR-17-20 |
286 |
287 |
1 |
0.0459 |
0.0091 |
0.075 |
3.2 |
0.0106 |
0.046 |
|
BR-17-20 |
287 |
288 |
1 |
0.0619 |
0.0395 |
0.047 |
2.3 |
0.0084 |
0.046 |
|
BR-17-20 |
288 |
289 |
1 |
0.064 |
0.0183 |
0.028 |
8.7 |
0.0364 |
0.106 |
|
BR-17-20 |
289 |
290 |
1 |
0.264 |
0.141 |
0.044 |
1.4 |
0.0115 |
0.259 |
|
BR-17-20 |
290 |
291 |
1 |
0.256 |
0.137 |
0.067 |
2.3 |
0.0131 |
0.639 |
|
BR-17-20 |
291 |
292 |
1 |
3.03 |
1.3 |
0.088 |
17.2 |
0.306 |
1.673 |
|
BR-17-20 |
292 |
293 |
1 |
0.199 |
0.0562 |
0.075 |
1 |
0.0037 |
0.106 |
|
BR-17-20 |
293 |
293.5 |
0.5 |
0.157 |
0.0691 |
0.073 |
2.4 |
0.013 |
0.106 |
|
BR-17-20 |
293.5 |
294.4 |
0.9 |
0.112 |
0.0575 |
0.049 |
0.9 |
0.0035 |
0.046 |
|
BR-17-20 |
294.4 |
295.4 |
1 |
0.104 |
0.0368 |
0.052 |
0.5 |
0.0019 |
0.319 |
|
BR-17-20 |
295.4 |
296 |
0.6 |
0.0203 |
0.0077 |
0.055 |
<0.5 |
0.0016 |
0.046 |
|
BR-17-20 |
296 |
297 |
1 |
0.0467 |
0.0086 |
0.065 |
<0.5 |
0.0019 |
0.198 |
|
BR-17-20 |
297 |
298 |
1 |
0.246 |
0.0573 |
0.05 |
2.6 |
0.0343 |
1.415 |
|
BR-17-20 |
298 |
299 |
1 |
0.0581 |
0.0049 |
0.042 |
<0.5 |
0.0012 |
0.03 |
|
BR-17-20 |
299 |
300 |
1 |
0.591 |
0.307 |
0.078 |
17 |
0.103 |
0.502 |
|
BR-17-20 |
300 |
301 |
1 |
0.267 |
0.068 |
0.214 |
4.1 |
0.0101 |
0.35 |
|
BR-17-20 |
301 |
302 |
1 |
0.0201 |
0.0038 |
0.042 |
<0.5 |
0.0012 |
0.259 |
|
BR-17-20 |
302 |
303 |
1 |
0.0578 |
0.0036 |
0.043 |
<0.5 |
0.0013 |
0.046 |
|
BR-17-20 |
303 |
304 |
1 |
0.0327 |
0.0038 |
0.038 |
<0.5 |
0.004 |
0.076 |
|
BR-17-20 |
304 |
305 |
1 |
0.129 |
0.219 |
0.033 |
3.5 |
0.044 |
0.776 |
|
BR-17-20 |
305 |
306 |
1 |
0.0431 |
0.0033 |
0.026 |
<0.5 |
0.0008 |
0.426 |
|
BR-17-20 |
306 |
307 |
1 |
0.148 |
0.0587 |
0.04 |
0.6 |
0.0069 |
0.289 |
|
BR-17-20 |
307 |
308 |
1 |
0.0937 |
0.0183 |
0.04 |
<0.5 |
0.0017 |
0.167 |
|
BR-17-20 |
308 |
309 |
1 |
0.0359 |
0.0112 |
0.041 |
<0.5 |
0.0011 |
0.076 |
|
BR-17-20 |
309 |
310 |
1 |
0.0228 |
0.0038 |
0.019 |
<0.5 |
0.0008 |
0.122 |
|
BR-17-20 |
310 |
311 |
1 |
0.0355 |
0.0073 |
0.025 |
<0.5 |
0.0015 |
0.076 |
|
BR-17-20 |
311 |
312 |
1 |
0.132 |
0.0169 |
0.043 |
<0.5 |
0.0011 |
0.106 |
|
BR-17-20 |
312 |
313 |
1 |
0.113 |
0.0153 |
0.031 |
<0.5 |
0.0015 |
0.319 |
|
BR-17-20 |
313 |
314 |
1 |
0.22 |
0.0415 |
0.038 |
<0.5 |
0.0013 |
0.091 |
|
BR-17-20 |
314 |
314.7 |
0.7 |
0.0801 |
0.0146 |
0.039 |
<0.5 |
0.0009 |
0.091 |
|
BR-17-20 |
314.7 |
315.5 |
0.8 |
0.0291 |
0.005 |
0.018 |
<0.5 |
0.0006 |
0.046 |
|
BR-17-20 |
315.5 |
316 |
0.5 |
0.0263 |
0.0031 |
0.016 |
<0.5 |
0.0005 |
0.03 |
|
BR-17-20 |
316 |
317 |
1 |
0.0179 |
0.0071 |
0.025 |
<0.5 |
0.0006 |
0.03 |
|
BR-17-20 |
317 |
318 |
1 |
0.0186 |
0.0035 |
0.028 |
<0.5 |
0.0007 |
0.03 |
|
BR-17-20 |
318 |
319 |
1 |
0.0352 |
0.0051 |
0.022 |
<0.5 |
0.0007 |
0.03 |
|
BR-17-20 |
319 |
320 |
1 |
0.0622 |
0.0027 |
0.016 |
<0.5 |
0.0007 |
0.137 |
|
BR-17-20 |
320 |
321 |
1 |
0.074 |
0.144 |
0.024 |
1.3 |
0.001 |
0.106 |
|
BR-17-20 |
321 |
322 |
1 |
0.0415 |
0.0149 |
0.01 |
<0.5 |
0.0007 |
0.913 |
|
BR-17-20 |
322 |
323 |
1 |
0.0337 |
0.024 |
0.01 |
<0.5 |
0.0005 |
0.137 |
|
BR-17-20 |
323 |
324 |
1 |
0.0235 |
0.0019 |
0.011 |
<0.5 |
0.0005 |
0.091 |
|
BR-17-20 |
324 |
325 |
1 |
0.0139 |
0.0023 |
0.008 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
325 |
326 |
1 |
0.0112 |
0.0047 |
0.014 |
<0.5 |
0.0005 |
0.046 |
|
BR-17-20 |
326 |
327 |
1 |
0.0061 |
0.002 |
0.009 |
<0.5 |
0.0004 |
0.061 |
|
BR-17-20 |
327 |
328 |
1 |
0.0295 |
0.0023 |
0.006 |
<0.5 |
0.0003 |
0.122 |
|
BR-17-20 |
328 |
329 |
1 |
0.0201 |
0.0017 |
0.012 |
<0.5 |
0.0006 |
0.061 |
|
BR-17-20 |
329 |
330 |
1 |
0.0269 |
0.0043 |
0.025 |
<0.5 |
0.0013 |
0.046 |
|
BR-17-20 |
330 |
331 |
1 |
0.0317 |
0.0018 |
0.014 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
331 |
332 |
1 |
0.0213 |
0.0031 |
0.009 |
<0.5 |
0.0003 |
0.091 |
|
BR-17-20 |
332 |
333 |
1 |
0.024 |
0.0031 |
0.015 |
<0.5 |
0.0003 |
0.061 |
|
BR-17-20 |
333 |
334 |
1 |
0.0694 |
0.006 |
0.012 |
<0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
334 |
335 |
1 |
0.0144 |
0.0019 |
0.007 |
<0.5 |
0.0002 |
0.091 |
|
BR-17-20 |
335 |
336 |
1 |
0.032 |
0.0168 |
0.023 |
<0.5 |
0.0009 |
0.167 |
|
BR-17-20 |
336 |
337 |
1 |
0.023 |
0.0092 |
0.02 |
<0.5 |
0.0006 |
0.122 |
|
BR-17-20 |
337 |
338 |
1 |
0.2 |
0.085 |
0.038 |
1.1 |
0.0134 |
1.552 |
|
BR-17-20 |
338 |
339 |
1 |
0.244 |
0.0795 |
0.033 |
1.1 |
0.0172 |
0.274 |
|
BR-17-20 |
339 |
340 |
1 |
0.813 |
0.32 |
0.034 |
3.5 |
0.0535 |
0.502 |
|
BR-17-20 |
340 |
341 |
1 |
0.118 |
0.0133 |
0.021 |
<0.5 |
0.0024 |
0.061 |
|
BR-17-20 |
341 |
342 |
1 |
0.495 |
0.155 |
0.078 |
4.1 |
0.0187 |
1.187 |
|
BR-17-20 |
342 |
343 |
1 |
0.364 |
0.0429 |
0.033 |
0.8 |
0.0023 |
2.434 |
|
BR-17-20 |
343 |
344 |
1 |
0.0578 |
0.0095 |
0.019 |
<0.5 |
0.0009 |
0.487 |
|
BR-17-20 |
344 |
345 |
1 |
0.0552 |
0.0114 |
0.013 |
<0.5 |
0.0009 |
0.106 |
|
BR-17-20 |
345 |
346.2 |
1.2 |
0.0908 |
0.0255 |
0.033 |
0.9 |
0.003 |
0.365 |
|
BR-17-20 |
346.2 |
347.4 |
1.2 |
0.177 |
0.0524 |
0.029 |
1.5 |
0.0069 |
0.106 |
|
BR-17-20 |
347.4 |
348.5 |
1.1 |
0.0864 |
0.0168 |
0.019 |
0.8 |
0.0016 |
0.35 |
|
BR-17-20 |
348.5 |
349.5 |
1 |
0.0385 |
0.0081 |
0.017 |
0.6 |
0.0009 |
0.091 |
|
BR-17-20 |
349.5 |
350.5 |
1 |
0.0463 |
0.0047 |
0.015 |
0.8 |
0.0005 |
0.304 |
|
BR-17-20 |
350.5 |
351.5 |
1 |
0.0079 |
0.0046 |
0.016 |
0.8 |
0.0009 |
0.228 |
|
BR-17-20 |
351.5 |
352.5 |
1 |
0.0206 |
0.0082 |
0.02 |
2.2 |
0.0007 |
0.106 |
|
BR-17-20 |
352.5 |
353.5 |
1 |
0.0149 |
0.0081 |
0.017 |
1.8 |
0.001 |
0.046 |
|
BR-17-20 |
353.5 |
354.5 |
1 |
0.194 |
0.168 |
0.027 |
10.2 |
0.0011 |
0.046 |
|
BR-17-20 |
354.5 |
355.5 |
1 |
0.106 |
0.0639 |
0.025 |
11.5 |
0.0011 |
0.122 |
|
BR-17-20 |
355.5 |
356.5 |
1 |
0.0183 |
0.0133 |
0.023 |
4.1 |
0.0018 |
0.046 |
|
BR-17-20 |
356.5 |
357.5 |
1 |
0.0055 |
0.003 |
0.018 |
4 |
0.0005 |
0.03 |
|
BR-17-20 |
357.5 |
358.5 |
1 |
0.0923 |
0.0242 |
0.019 |
4.7 |
0.0007 |
0.03 |
|
BR-17-20 |
358.5 |
359.5 |
1 |
0.0309 |
0.0122 |
0.017 |
4.3 |
0.0005 |
0.03 |
|
BR-17-20 |
359.5 |
360.5 |
1 |
0.0431 |
0.0102 |
0.019 |
4.7 |
0.0006 |
0.046 |
|
BR-17-20 |
360.5 |
361.5 |
1 |
0.0157 |
0.0072 |
0.017 |
13 |
0.0011 |
0.243 |
|
BR-17-20 |
361.5 |
363 |
1.5 |
0.0617 |
0.0308 |
0.016 |
8.6 |
0.0015 |
0.228 |
|
BR-17-20 |
363 |
364 |
1 |
0.0433 |
0.0423 |
0.008 |
4.6 |
0.0004 |
0.821 |
|
BR-17-20 |
364 |
365 |
1 |
0.114 |
0.0591 |
0.007 |
9.4 |
0.0015 |
0.776 |
|
BR-17-20 |
365 |
366 |
1 |
0.0325 |
0.0148 |
<0.005 |
2.9 |
0.0003 |
0.289 |
|
BR-17-20 |
366 |
367 |
1 |
0.0172 |
0.0308 |
0.013 |
2.3 |
0.0004 |
0.076 |
|
BR-17-20 |
367 |
368 |
1 |
0.0379 |
0.0034 |
0.008 |
1.9 |
0.0002 |
0.198 |
|
BR-17-20 |
368 |
369 |
1 |
0.0613 |
0.0084 |
0.007 |
2.7 |
0.0004 |
0.517 |
|
BR-17-20 |
369 |
370 |
1 |
0.147 |
0.0272 |
0.005 |
3.6 |
0.0005 |
0.456 |
|
BR-17-20 |
370 |
371 |
1 |
0.107 |
0.0073 |
0.007 |
2.3 |
0.0004 |
0.152 |
|
BR-17-20 |
371 |
372 |
1 |
0.0884 |
0.0033 |
0.008 |
1.5 |
0.0002 |
0.35 |
|
BR-17-20 |
372 |
373 |
1 |
0.057 |
0.0124 |
0.009 |
1.6 |
0.0003 |
0.106 |
|
BR-17-20 |
373 |
374 |
1 |
0.0053 |
0.0041 |
0.007 |
2.7 |
0.0004 |
0.365 |
|
BR-17-20 |
374 |
375 |
1 |
0.0244 |
0.0091 |
0.005 |
1.4 |
0.0002 |
0.061 |
|
BR-17-20 |
375 |
376 |
1 |
0.0245 |
0.0044 |
<0.005 |
1.1 |
0.0003 |
0.061 |
|
BR-17-20 |
376 |
377 |
1 |
0.0108 |
0.002 |
0.006 |
1.1 |
0.0003 |
0.046 |
|
BR-17-20 |
377 |
378 |
1 |
0.0197 |
0.0047 |
<0.005 |
1 |
0.0003 |
0.091 |
|
BR-17-20 |
378 |
379 |
1 |
0.0392 |
0.0076 |
0.005 |
1.3 |
0.0004 |
0.228 |
|
BR-17-20 |
379 |
380 |
1 |
0.0191 |
0.0056 |
0.005 |
0.8 |
0.0004 |
0.076 |
|
BR-17-20 |
380 |
381 |
1 |
0.0762 |
0.031 |
0.005 |
1.4 |
0.0032 |
0.076 |
|
BR-17-20 |
381 |
382 |
1 |
0.0544 |
0.0113 |
0.006 |
0.6 |
0.0009 |
0.228 |
|
BR-17-20 |
382 |
383 |
1 |
0.187 |
0.0575 |
0.009 |
4.3 |
0.0065 |
0.213 |
|
BR-17-20 |
383 |
384 |
1 |
0.0415 |
0.0056 |
0.006 |
1.1 |
0.0005 |
0.046 |
|
BR-17-20 |
384 |
385 |
1 |
0.0188 |
0.0054 |
0.006 |
0.6 |
0.0002 |
0.137 |
|
BR-17-20 |
385 |
386 |
1 |
0.0471 |
0.0028 |
<0.005 |
<0.5 |
0.0002 |
0.441 |
|
BR-17-20 |
386 |
387 |
1 |
0.0123 |
0.0053 |
<0.005 |
0.5 |
0.0001 |
0.046 |
|
BR-17-20 |
387 |
388 |
1 |
0.0132 |
0.0095 |
0.006 |
0.7 |
0.0002 |
0.046 |
|
BR-17-20 |
388 |
389 |
1 |
0.034 |
0.0221 |
0.016 |
1.4 |
0.0005 |
0.076 |
|
BR-17-20 |
389 |
390 |
1 |
0.0136 |
0.0059 |
0.006 |
0.6 |
0.0003 |
0.061 |
|
BR-17-20 |
390 |
391 |
1 |
0.0098 |
0.0013 |
0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-17-20 |
391 |
392 |
1 |
0.499 |
0.535 |
0.02 |
33.6 |
0.184 |
0.669 |
|
BR-17-20 |
392 |
393 |
1 |
0.0233 |
0.0077 |
0.015 |
1.3 |
0.0005 |
0.076 |
|
BR-17-20 |
393 |
394 |
1 |
0.191 |
0.0444 |
0.054 |
9.5 |
0.0017 |
0.365 |
|
BR-17-20 |
394 |
395 |
1 |
0.0847 |
0.1035 |
0.018 |
7.5 |
0.0006 |
1.232 |
|
BR-17-20 |
395 |
396 |
1 |
0.223 |
0.0603 |
0.026 |
25.1 |
0.0014 |
0.608 |
|
BR-17-20 |
396 |
397.3 |
1.3 |
0.232 |
0.0769 |
0.024 |
11 |
0.0008 |
2.145 |
|
BR-17-20 |
397.3 |
398 |
0.7 |
0.123 |
0.0628 |
0.023 |
5.6 |
0.0008 |
0.563 |
|
BR-17-20 |
398 |
400 |
2 |
0.0989 |
0.0387 |
0.017 |
9 |
0.0033 |
0.593 |
|
BR-17-20 |
400 |
402 |
2 |
0.0086 |
0.0022 |
0.013 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
402 |
404 |
2 |
0.0063 |
0.0022 |
0.019 |
0.8 |
0.0004 |
0.061 |
|
BR-17-20 |
404 |
406 |
2 |
0.0065 |
0.0013 |
0.012 |
0.5 |
0.0006 |
0.046 |
|
BR-17-20 |
406 |
408 |
2 |
0.011 |
0.0021 |
0.006 |
0.5 |
0.0003 |
0.061 |
|
BR-17-20 |
408 |
410 |
2 |
0.0531 |
0.0078 |
0.01 |
0.8 |
0.0003 |
0.137 |
|
BR-17-20 |
410 |
412 |
2 |
0.0238 |
0.0075 |
0.006 |
0.8 |
0.0002 |
0.213 |
|
BR-17-20 |
412 |
414 |
2 |
0.0128 |
0.007 |
0.007 |
0.8 |
0.0004 |
0.198 |
|
BR-17-20 |
414 |
416 |
2 |
0.0149 |
<0.005 |
0.007 |
0.5 |
0.0002 |
0.076 |
|
BR-17-20 |
416 |
417 |
1 |
0.0162 |
0.0037 |
0.006 |
0.6 |
0.0003 |
0.213 |
|
BR-17-20 |
417 |
417.7 |
0.7 |
0.022 |
0.0067 |
0.009 |
1 |
0.0002 |
0.304 |
|
BR-17-20 |
417.7 |
418.5 |
0.8 |
0.013 |
0.0028 |
0.009 |
<0.5 |
0.0003 |
0.03 |
|
BR-17-20 |
418.5 |
420 |
1.5 |
0.008 |
0.0019 |
0.016 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
420 |
421 |
1 |
0.0106 |
0.0017 |
0.011 |
<0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
421 |
422 |
1 |
0.0072 |
0.0016 |
0.007 |
<0.5 |
0.0002 |
0.274 |
|
BR-17-20 |
422 |
423 |
1 |
0.0254 |
0.0021 |
0.011 |
<0.5 |
0.0002 |
0.411 |
|
BR-17-20 |
423 |
424 |
1 |
0.0191 |
0.0018 |
0.016 |
<0.5 |
0.0002 |
0.198 |
|
BR-17-20 |
424 |
425 |
1 |
0.0458 |
0.0141 |
0.015 |
3 |
0.002 |
4.838 |
|
BR-17-20 |
425 |
426 |
1 |
0.0224 |
0.0028 |
0.014 |
0.7 |
0.0004 |
0.487 |
|
BR-17-20 |
426 |
427 |
1 |
0.0315 |
0.0039 |
0.008 |
0.7 |
0.0002 |
0.213 |
|
BR-17-20 |
427 |
428 |
1 |
0.0531 |
0.0099 |
0.022 |
6.7 |
0.0007 |
0.319 |
|
BR-17-20 |
428 |
429 |
1 |
0.0443 |
0.0079 |
0.008 |
0.5 |
0.0003 |
0.061 |
|
BR-17-20 |
429 |
430 |
1 |
0.0111 |
0.0084 |
0.007 |
<0.5 |
0.0005 |
0.061 |
|
BR-17-20 |
430 |
431 |
1 |
0.017 |
0.0188 |
0.009 |
0.6 |
0.0003 |
0.198 |
|
BR-17-20 |
431 |
432 |
1 |
0.0456 |
0.0081 |
0.006 |
<0.5 |
0.0003 |
0.091 |
|
BR-17-20 |
432 |
433 |
1 |
0.0288 |
0.0059 |
0.007 |
<0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
433 |
434 |
1 |
0.0705 |
0.0199 |
0.011 |
8.5 |
0.0019 |
0.106 |
|
BR-17-20 |
434 |
435 |
1 |
0.0316 |
0.0053 |
0.019 |
0.9 |
0.0004 |
0.365 |
|
BR-17-20 |
435 |
436 |
1 |
0.0277 |
0.0051 |
0.008 |
<0.5 |
0.0002 |
0.061 |
|
BR-17-20 |
436 |
437 |
1 |
0.006 |
0.0049 |
0.009 |
<0.5 |
0.0002 |
0.03 |
|
BR-17-20 |
437 |
438 |
1 |
0.105 |
0.135 |
0.032 |
6.3 |
0.0012 |
0.137 |
|
BR-17-20 |
438 |
439.4 |
1.4 |
0.0077 |
<0.005 |
0.011 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
439.4 |
440 |
0.6 |
0.0123 |
0.0017 |
0.01 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
440 |
441 |
1 |
0.016 |
0.009 |
0.016 |
2.9 |
0.0005 |
0.091 |
|
BR-17-20 |
441 |
442 |
1 |
0.292 |
0.121 |
0.064 |
35.2 |
0.0106 |
2.495 |
|
BR-17-20 |
442 |
443 |
1 |
0.0306 |
0.0198 |
0.025 |
5.6 |
0.0014 |
0.715 |
|
BR-17-20 |
443 |
444 |
1 |
0.0044 |
0.0035 |
0.017 |
1.4 |
0.0007 |
0.046 |
|
BR-17-20 |
444 |
445 |
1 |
0.0067 |
0.0023 |
0.018 |
0.5 |
0.0005 |
0.076 |
|
BR-17-20 |
445 |
446 |
1 |
0.014 |
0.0087 |
0.026 |
2.1 |
0.0005 |
0.274 |
|
BR-17-20 |
446 |
447.2 |
1.2 |
0.0596 |
0.0264 |
0.034 |
7.8 |
0.0017 |
0.411 |
|
BR-17-20 |
447.2 |
448 |
0.8 |
0.0349 |
0.0136 |
0.02 |
2.8 |
0.0007 |
0.076 |
|
BR-17-20 |
448 |
449 |
1 |
0.0322 |
0.0582 |
0.017 |
3.6 |
0.0008 |
0.106 |
|
BR-17-20 |
449 |
450 |
1 |
0.0592 |
0.0725 |
0.022 |
7.9 |
0.0029 |
2.023 |
|
BR-17-20 |
450 |
451 |
1 |
0.0222 |
0.0112 |
0.016 |
1.4 |
0.0005 |
2.419 |
|
BR-17-20 |
451 |
452 |
1 |
0.0044 |
<0.005 |
0.028 |
0.7 |
0.0004 |
0.821 |
|
BR-17-20 |
452 |
453 |
1 |
0.0162 |
0.0103 |
0.015 |
1 |
0.0005 |
0.076 |
|
BR-17-20 |
453 |
454 |
1 |
0.0124 |
0.0074 |
0.012 |
0.5 |
0.0003 |
0.517 |
|
BR-17-20 |
454 |
455 |
1 |
0.109 |
0.0188 |
0.011 |
1.3 |
0.0004 |
0.243 |
|
BR-17-20 |
455 |
456 |
1 |
0.0326 |
0.011 |
0.012 |
0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
456 |
457 |
1 |
0.0151 |
0.003 |
0.011 |
<0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
457 |
458 |
1 |
0.0767 |
0.0132 |
0.02 |
1.6 |
0.0017 |
0.456 |
|
BR-17-20 |
458 |
459 |
1 |
0.0458 |
0.0066 |
0.017 |
1.8 |
0.0021 |
0.046 |
|
BR-17-20 |
459 |
460 |
1 |
0.0244 |
0.0045 |
0.013 |
<0.5 |
0.0005 |
0.061 |
|
BR-17-20 |
460 |
461 |
1 |
0.0182 |
0.0017 |
0.01 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
461 |
462 |
1 |
0.0135 |
0.0059 |
0.009 |
1.2 |
0.0035 |
0.046 |
|
BR-17-20 |
462 |
463 |
1 |
0.0088 |
0.0023 |
0.008 |
<0.5 |
0.0006 |
0.03 |
|
BR-17-20 |
463 |
464 |
1 |
0.011 |
0.0205 |
0.009 |
8.3 |
0.0234 |
0.03 |
|
BR-17-20 |
464 |
465 |
1 |
0.0122 |
0.0023 |
0.006 |
<0.5 |
0.0013 |
0.046 |
|
BR-17-20 |
465 |
466 |
1 |
0.0144 |
0.0014 |
<0.005 |
<0.5 |
0.0016 |
0.046 |
|
BR-17-20 |
466 |
467 |
1 |
0.0111 |
0.0023 |
<0.005 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
467 |
468 |
1 |
0.0099 |
0.0015 |
0.005 |
<0.5 |
0.0014 |
0.03 |
|
BR-17-20 |
468 |
469 |
1 |
0.0084 |
0.001 |
0.011 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
469 |
470 |
1 |
0.0115 |
0.0011 |
0.018 |
<0.5 |
0.007 |
0.061 |
|
BR-17-20 |
470 |
471 |
1 |
0.0549 |
0.0014 |
0.007 |
<0.5 |
0.0012 |
0.259 |
|
BR-17-20 |
471 |
472 |
1 |
0.0141 |
0.0024 |
0.012 |
<0.5 |
0.0035 |
0.03 |
|
BR-17-20 |
472 |
473 |
1 |
0.0055 |
0.0031 |
0.006 |
<0.5 |
0.0023 |
0.061 |
|
BR-17-20 |
473 |
474 |
1 |
0.0163 |
0.0013 |
0.01 |
<0.5 |
0.0104 |
0.046 |
|
BR-17-20 |
474 |
475 |
1 |
0.0061 |
0.0013 |
0.027 |
<0.5 |
0.0013 |
0.061 |
|
BR-17-20 |
475 |
476 |
1 |
0.0046 |
0.0011 |
0.009 |
<0.5 |
0.0024 |
0.03 |
|
BR-17-20 |
476 |
477 |
1 |
0.0093 |
0.001 |
0.008 |
<0.5 |
0.0036 |
0.03 |
|
BR-17-20 |
477 |
478 |
1 |
0.0053 |
0.0007 |
0.009 |
<0.5 |
0.0013 |
0.03 |
|
BR-17-20 |
478 |
479 |
1 |
0.0122 |
0.0012 |
0.007 |
<0.5 |
0.0082 |
0.046 |
|
BR-17-20 |
479 |
480 |
1 |
0.0085 |
0.0099 |
0.007 |
<0.5 |
0.0085 |
0.152 |
|
BR-17-20 |
480 |
481.2 |
1.2 |
0.0281 |
0.007 |
0.008 |
<0.5 |
0.0018 |
1.065 |
|
BR-17-20 |
481.2 |
482.4 |
1.2 |
0.0076 |
0.0009 |
<0.005 |
<0.5 |
0.0004 |
0.046 |
|
BR-17-20 |
482.4 |
483.6 |
1.2 |
0.0077 |
0.0011 |
<0.005 |
<0.5 |
0.0018 |
0.046 |
|
BR-17-20 |
483.6 |
484.8 |
1.2 |
0.0075 |
0.0014 |
0.006 |
<0.5 |
0.0018 |
0.091 |
|
BR-17-20 |
484.8 |
486 |
1.2 |
0.0074 |
0.0016 |
0.006 |
<0.5 |
0.0006 |
0.046 |
|
BR-17-20 |
486 |
487.2 |
1.2 |
0.0086 |
0.0019 |
0.006 |
<0.5 |
0.0027 |
0.046 |
|
BR-17-20 |
487.2 |
488.4 |
1.2 |
0.0119 |
0.0035 |
0.011 |
1.7 |
0.0089 |
0.198 |
|
BR-17-20 |
488.4 |
489.6 |
1.2 |
0.0192 |
0.0074 |
0.008 |
1.1 |
0.0185 |
0.046 |
|
BR-17-20 |
489.6 |
490.8 |
1.2 |
0.0209 |
0.0022 |
0.008 |
<0.5 |
0.0015 |
0.046 |
|
BR-17-20 |
490.8 |
492 |
1.2 |
0.008 |
0.0011 |
<0.005 |
<0.5 |
0.0004 |
0.061 |
|
BR-17-20 |
492 |
493 |
1 |
0.0102 |
0.0038 |
0.007 |
<0.5 |
0.0021 |
0.076 |
|
BR-17-20 |
493 |
494 |
1 |
0.0155 |
0.0026 |
0.005 |
<0.5 |
0.0012 |
0.122 |
|
BR-17-20 |
494 |
495 |
1 |
0.008 |
0.0015 |
0.012 |
0.6 |
0.0055 |
0.106 |
|
BR-17-20 |
495 |
496 |
1 |
0.007 |
0.0009 |
0.006 |
<0.5 |
0.0007 |
0.046 |
|
BR-17-20 |
496 |
497 |
1 |
0.0072 |
0.0007 |
<0.005 |
<0.5 |
0.0003 |
0.046 |
|
BR-17-20 |
497 |
498 |
1 |
0.0061 |
0.0008 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-17-20 |
498 |
498.5 |
0.5 |
0.0121 |
0.0011 |
<0.005 |
<0.5 |
0.0003 |
0.061 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-18-20 |
0 |
135 |
No sample |
||||||
|
BR-18-20 |
135 |
137 |
2 |
0.01 |
0.001 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-18-20 |
137 |
139 |
2 |
0.009 |
0.0012 |
<0.005 |
<0.5 |
0.0006 |
0.106 |
|
BR-18-20 |
139 |
141 |
2 |
0.0084 |
0.0013 |
<0.005 |
<0.5 |
0.0002 |
0.03 |
|
BR-18-20 |
141 |
143 |
2 |
0.0077 |
0.001 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-18-20 |
143 |
145 |
2 |
0.0087 |
0.001 |
<0.005 |
<0.5 |
0.0015 |
0.319 |
|
BR-18-20 |
145 |
147 |
2 |
0.0082 |
0.0013 |
<0.005 |
<0.5 |
0.0001 |
0.03 |
|
BR-18-20 |
147 |
149 |
2 |
0.0074 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
149 |
151 |
2 |
0.0073 |
0.0006 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
151 |
153 |
2 |
0.0102 |
0.0011 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
153 |
155 |
2 |
0.0093 |
0.0007 |
0.005 |
<0.5 |
0.0003 |
0.046 |
|
BR-18-20 |
155 |
157 |
2 |
0.0128 |
0.0034 |
0.008 |
0.6 |
0.0014 |
0.076 |
|
BR-18-20 |
157 |
159 |
2 |
0.0075 |
0.001 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-18-20 |
159 |
161 |
2 |
0.0073 |
0.001 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
161 |
162 |
1 |
0.0067 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
162 |
163 |
1 |
0.0068 |
0.0007 |
<0.005 |
<0.5 |
0.0002 |
0.152 |
|
BR-18-20 |
163 |
164 |
1 |
0.0066 |
0.0009 |
0.006 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
164 |
165 |
1 |
0.0069 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.35 |
|
BR-18-20 |
165 |
166 |
1 |
0.0065 |
0.001 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
166 |
167 |
1 |
0.0067 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
167 |
168 |
1 |
0.0063 |
0.0008 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-18-20 |
168 |
169 |
1 |
0.0062 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
169 |
170.15 |
1.15 |
0.006 |
0.0009 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
170.15 |
171 |
0.85 |
0.0055 |
0.0009 |
<0.005 |
<0.5 |
0.0005 |
0.137 |
|
BR-18-20 |
171 |
172 |
1 |
0.006 |
0.001 |
<0.005 |
<0.5 |
0.0004 |
0.183 |
|
BR-18-20 |
172 |
173.1 |
1.1 |
0.0064 |
0.0011 |
<0.005 |
<0.5 |
0.0073 |
0.639 |
|
BR-18-20 |
173.1 |
173.9 |
0.8 |
0.0039 |
0.0048 |
0.202 |
1 |
0.0066 |
5.994 |
|
BR-18-20 |
173.9 |
174.7 |
0.8 |
0.0292 |
0.0113 |
0.134 |
2.1 |
0.0191 |
2.297 |
|
BR-18-20 |
174.7 |
175.5 |
0.8 |
1.495 |
1.025 |
0.483 |
86.9 |
0.874 |
26.926 |
|
BR-18-20 |
175.5 |
176.5 |
1 |
1.105 |
0.849 |
0.515 |
69.3 |
1.17 |
38.944 |
|
BR-18-20 |
176.5 |
177.5 |
1 |
0.341 |
0.189 |
0.58 |
28.5 |
0.886 |
41.834 |
|
BR-18-20 |
177.5 |
178.5 |
1 |
1.365 |
0.749 |
0.845 |
90.8 |
0.847 |
24.644 |
|
BR-18-20 |
178.5 |
179.5 |
1 |
0.689 |
1.02 |
0.328 |
98 |
1.39 |
44.116 |
|
BR-18-20 |
179.5 |
180.8 |
1.3 |
2.09 |
1.545 |
0.915 |
136 |
0.568 |
54.308 |
|
BR-18-20 |
180.8 |
181.3 |
0.5 |
1.005 |
2.19 |
1.45 |
155 |
0.943 |
85.189 |
|
BR-18-20 |
181.3 |
182 |
0.7 |
1.845 |
2.03 |
1.325 |
167 |
0.548 |
88.688 |
|
BR-18-20 |
182 |
182.5 |
0.5 |
2.07 |
2.35 |
1.14 |
393 |
0.576 |
85.189 |
|
BR-18-20 |
182.5 |
183 |
0.5 |
7.7 |
3.93 |
3.61 |
455 |
0.517 |
74.997 |
|
BR-18-20 |
183 |
183.7 |
0.7 |
3.6 |
1.71 |
1.495 |
312 |
0.311 |
44.42 |
|
BR-18-20 |
183.7 |
184.5 |
0.8 |
0.13 |
0.367 |
0.035 |
6.4 |
0.036 |
0.837 |
|
BR-18-20 |
184.5 |
185.5 |
1 |
0.107 |
0.0309 |
0.02 |
6 |
0.0038 |
0.669 |
|
BR-18-20 |
185.5 |
186.5 |
1 |
0.0978 |
0.166 |
0.005 |
5.2 |
0.0083 |
0.487 |
|
BR-18-20 |
186.5 |
187.5 |
1 |
0.0594 |
0.0256 |
<0.005 |
4.7 |
0.001 |
0.091 |
|
BR-18-20 |
187.5 |
188.5 |
1 |
0.0238 |
0.124 |
<0.005 |
5.8 |
0.0131 |
0.456 |
|
BR-18-20 |
188.5 |
189.5 |
1 |
0.0105 |
0.0771 |
<0.005 |
3.4 |
0.0087 |
1.521 |
|
BR-18-20 |
189.5 |
190.4 |
0.9 |
0.0237 |
0.0423 |
<0.005 |
4.5 |
0.0148 |
1.582 |
|
BR-18-20 |
190.4 |
192.4 |
2 |
0.0137 |
0.0937 |
0.016 |
2.4 |
0.0133 |
1.384 |
|
BR-18-20 |
192.4 |
194 |
1.6 |
0.228 |
0.226 |
0.014 |
4.7 |
0.0169 |
0.137 |
|
BR-18-20 |
194 |
196 |
2 |
0.15 |
0.241 |
0.012 |
1.7 |
0.0132 |
1.536 |
|
BR-18-20 |
196 |
197.4 |
1.4 |
0.0639 |
0.395 |
0.012 |
3 |
0.0115 |
3.544 |
|
BR-18-20 |
197.4 |
198.4 |
1 |
0.0057 |
0.0065 |
<0.005 |
<0.5 |
0.0023 |
0.061 |
|
BR-18-20 |
198.4 |
199.4 |
1 |
0.0036 |
0.0016 |
<0.005 |
<0.5 |
0.001 |
0.03 |
|
BR-18-20 |
199.4 |
200.4 |
1 |
0.0049 |
0.0021 |
<0.005 |
<0.5 |
0.0028 |
0.046 |
|
BR-18-20 |
200.4 |
201 |
0.6 |
0.0066 |
0.0011 |
<0.005 |
0.9 |
0.0126 |
0.046 |
|
BR-18-20 |
201 |
201.3 |
0.3 |
No sample |
|||||
|
BR-18-20 |
201.3 |
202.3 |
1 |
0.0051 |
0.0028 |
<0.005 |
<0.5 |
0.0017 |
0.106 |
|
BR-18-20 |
202.3 |
202.8 |
0.5 |
No sample |
|||||
|
BR-18-20 |
202.8 |
204.8 |
2 |
0.0069 |
0.002 |
<0.005 |
<0.5 |
0.0011 |
0.015 |
|
BR-18-20 |
204.8 |
206.8 |
2 |
0.0066 |
0.002 |
<0.005 |
<0.5 |
0.0011 |
0.03 |
|
BR-18-20 |
206.8 |
208.8 |
2 |
0.0067 |
0.0103 |
<0.005 |
<0.5 |
0.0026 |
0.03 |
|
BR-18-20 |
208.8 |
210.8 |
2 |
0.0089 |
0.004 |
<0.005 |
<0.5 |
0.0022 |
0.061 |
|
BR-18-20 |
210.8 |
212.8 |
2 |
0.0112 |
0.0111 |
0.037 |
<0.5 |
0.0104 |
0.03 |
|
BR-18-20 |
212.8 |
214.8 |
2 |
0.015 |
0.137 |
0.048 |
1.3 |
0.0316 |
0.167 |
|
BR-18-20 |
214.8 |
216.8 |
2 |
0.0067 |
0.0034 |
<0.005 |
<0.5 |
0.0018 |
0.198 |
|
BR-18-20 |
216.8 |
218.8 |
2 |
0.0064 |
0.003 |
<0.005 |
<0.5 |
0.0015 |
0.03 |
|
BR-18-20 |
218.8 |
220.8 |
2 |
0.0102 |
0.0058 |
<0.005 |
<0.5 |
0.0042 |
0.03 |
|
BR-18-20 |
220.8 |
222.8 |
2 |
0.008 |
0.0152 |
0.007 |
<0.5 |
0.0034 |
1.445 |
|
BR-18-20 |
222.8 |
224.2 |
1.4 |
0.0088 |
0.0048 |
0.009 |
<0.5 |
0.0031 |
0.03 |
|
BR-18-20 |
224.2 |
225 |
0.8 |
0.07 |
0.0568 |
0.026 |
1.2 |
0.0153 |
0.015 |
|
BR-18-20 |
225 |
226 |
1 |
0.0558 |
0.105 |
0.032 |
1.6 |
0.0186 |
0.122 |
|
BR-18-20 |
226 |
227 |
1 |
0.134 |
0.108 |
0.012 |
5.6 |
0.0088 |
0.532 |
|
BR-18-20 |
227 |
228 |
1 |
0.0604 |
0.152 |
0.04 |
1.6 |
0.0252 |
3.544 |
|
BR-18-20 |
228 |
229 |
1 |
0.0781 |
0.13 |
0.037 |
1.2 |
0.0167 |
1.749 |
|
BR-18-20 |
229 |
231 |
2 |
0.197 |
0.426 |
0.253 |
2.4 |
0.0157 |
9.493 |
|
BR-18-20 |
231 |
233 |
2 |
0.675 |
1.015 |
0.261 |
10.3 |
0.0441 |
0.365 |
|
BR-18-20 |
233 |
235 |
2 |
0.54 |
0.249 |
0.07 |
113 |
0.05 |
0.426 |
|
BR-18-20 |
235 |
237 |
2 |
0.239 |
0.115 |
0.059 |
45.4 |
0.0097 |
0.183 |
|
BR-18-20 |
237 |
239 |
2 |
0.876 |
0.28 |
0.145 |
69.4 |
0.0376 |
0.837 |
|
BR-18-20 |
239 |
241 |
2 |
0.259 |
0.128 |
0.053 |
16 |
0.0172 |
0.183 |
|
BR-18-20 |
241 |
243 |
2 |
0.328 |
0.176 |
0.044 |
38.1 |
0.0334 |
0.867 |
|
BR-18-20 |
243 |
245 |
2 |
0.0697 |
0.187 |
0.079 |
48.8 |
0.0304 |
0.487 |
|
BR-18-20 |
245 |
247 |
2 |
0.267 |
0.346 |
0.132 |
86 |
0.0303 |
1.749 |
|
BR-18-20 |
247 |
249 |
2 |
0.155 |
0.364 |
0.106 |
162 |
0.0408 |
1.278 |
|
BR-18-20 |
249 |
251 |
2 |
0.212 |
0.194 |
0.057 |
81.3 |
0.0202 |
0.426 |
|
BR-18-20 |
251 |
253 |
2 |
0.327 |
0.112 |
0.039 |
51.4 |
0.0086 |
0.821 |
|
BR-18-20 |
253 |
255 |
2 |
0.335 |
0.0954 |
0.042 |
47.5 |
0.0108 |
0.426 |
|
BR-18-20 |
255 |
257 |
2 |
0.325 |
0.0831 |
0.019 |
39.4 |
0.011 |
0.821 |
|
BR-18-20 |
257 |
259 |
2 |
0.113 |
0.0544 |
0.013 |
25 |
0.022 |
0.106 |
|
BR-18-20 |
259 |
261 |
2 |
0.2 |
0.132 |
0.052 |
38.4 |
0.0327 |
0.243 |
|
BR-18-20 |
261 |
263 |
2 |
0.123 |
0.0807 |
0.083 |
16.9 |
0.0162 |
0.304 |
|
BR-18-20 |
263 |
265 |
2 |
0.237 |
0.0733 |
0.056 |
96.6 |
0.0296 |
0.396 |
|
BR-18-20 |
265 |
267 |
2 |
0.451 |
0.113 |
0.024 |
116 |
0.0433 |
0.228 |
|
BR-18-20 |
267 |
269 |
2 |
0.156 |
0.0504 |
0.024 |
28.2 |
0.0097 |
0.167 |
|
BR-18-20 |
269 |
271 |
2 |
0.0898 |
0.0391 |
0.013 |
4.8 |
0.0046 |
0.38 |
|
BR-18-20 |
271 |
272.5 |
1.5 |
0.0655 |
0.0184 |
<0.005 |
2.9 |
0.0015 |
0.426 |
|
BR-18-20 |
272.5 |
273.1 |
0.6 |
0.0568 |
0.0203 |
<0.005 |
4.1 |
0.0027 |
0.213 |
|
BR-18-20 |
273.1 |
275 |
1.9 |
0.0182 |
0.0048 |
0.005 |
2.6 |
0.0016 |
0.213 |
|
BR-18-20 |
275 |
277 |
2 |
0.0625 |
0.0164 |
<0.005 |
3.3 |
0.0018 |
0.365 |
|
BR-18-20 |
277 |
279 |
2 |
0.0837 |
0.021 |
<0.005 |
6 |
0.0028 |
0.183 |
|
BR-18-20 |
279 |
281 |
2 |
0.0317 |
0.0076 |
<0.005 |
4.4 |
0.0019 |
0.137 |
|
BR-18-20 |
281 |
283 |
2 |
0.0257 |
0.0061 |
<0.005 |
2.8 |
0.0013 |
0.137 |
|
BR-18-20 |
283 |
285 |
2 |
0.0394 |
0.0063 |
<0.005 |
5.2 |
0.0015 |
0.335 |
|
BR-18-20 |
285 |
287 |
2 |
0.0244 |
0.0069 |
<0.005 |
4.5 |
0.0016 |
0.183 |
|
BR-18-20 |
287 |
289 |
2 |
0.0339 |
0.0047 |
<0.005 |
3.4 |
0.0017 |
0.152 |
|
BR-18-20 |
289 |
291 |
2 |
0.0171 |
0.0041 |
<0.005 |
3.8 |
0.0012 |
0.517 |
|
BR-18-20 |
291 |
293 |
2 |
0.0143 |
0.0036 |
<0.005 |
4 |
0.0013 |
0.137 |
|
BR-18-20 |
293 |
294.5 |
1.5 |
0.023 |
0.0103 |
<0.005 |
2.7 |
0.0023 |
0.411 |
|
BR-18-20 |
294.5 |
296.5 |
2 |
0.0335 |
0.0216 |
<0.005 |
2.5 |
<0.005 |
0.198 |
|
BR-18-20 |
296.5 |
297.1 |
0.6 |
0.0345 |
0.016 |
<0.005 |
1 |
0.003 |
0.046 |
|
BR-18-20 |
297.1 |
299 |
1.9 |
0.0397 |
0.012 |
<0.005 |
<0.5 |
0.0027 |
0.122 |
|
BR-18-20 |
299 |
301 |
2 |
0.0152 |
0.005 |
<0.005 |
1.9 |
0.0022 |
0.198 |
|
BR-18-20 |
301 |
303 |
2 |
0.0491 |
0.021 |
<0.005 |
4.7 |
0.0026 |
0.396 |
|
BR-18-20 |
303 |
305 |
2 |
0.0224 |
0.0115 |
0.006 |
11.6 |
0.003 |
0.319 |
|
BR-18-20 |
305 |
307 |
2 |
0.0145 |
0.0143 |
<0.005 |
12.2 |
0.0021 |
0.35 |
|
BR-18-20 |
307 |
309 |
2 |
0.0279 |
0.0146 |
<0.005 |
7.8 |
0.0019 |
0.35 |
|
BR-18-20 |
309 |
311 |
2 |
0.0116 |
0.007 |
<0.005 |
9.9 |
0.0022 |
0.243 |
|
BR-18-20 |
311 |
313 |
2 |
0.042 |
0.0122 |
<0.005 |
6.5 |
0.0014 |
0.335 |
|
BR-18-20 |
313 |
315 |
2 |
0.0584 |
0.0284 |
<0.005 |
24 |
0.0051 |
1.019 |
|
BR-18-20 |
315 |
317 |
2 |
0.016 |
0.0061 |
<0.005 |
11.9 |
0.0031 |
0.487 |
|
BR-18-20 |
317 |
319 |
2 |
0.0133 |
0.007 |
0.005 |
6.8 |
0.0018 |
0.502 |
|
BR-18-20 |
319 |
321 |
2 |
0.0334 |
0.0129 |
<0.005 |
4.5 |
0.003 |
0.487 |
|
BR-18-20 |
321 |
323 |
2 |
0.0151 |
0.0039 |
<0.005 |
1.4 |
0.0016 |
0.198 |
|
BR-18-20 |
323 |
325 |
2 |
0.0324 |
0.0073 |
<0.005 |
2.4 |
0.0021 |
0.487 |
|
BR-18-20 |
325 |
327 |
2 |
0.0155 |
0.0047 |
<0.005 |
1.8 |
0.0018 |
0.304 |
|
BR-18-20 |
327 |
329 |
2 |
0.0204 |
0.0085 |
<0.005 |
2.4 |
0.0029 |
0.365 |
|
BR-18-20 |
329 |
331 |
2 |
0.0271 |
0.0078 |
<0.005 |
1.9 |
<0.005 |
0.335 |
|
BR-18-20 |
331 |
333 |
2 |
0.0338 |
0.0077 |
<0.005 |
2.4 |
0.0018 |
0.472 |
|
BR-18-20 |
333 |
335 |
2 |
0.0337 |
0.0117 |
<0.005 |
2 |
0.0015 |
0.441 |
|
BR-18-20 |
335 |
337 |
2 |
0.0239 |
0.0725 |
0.005 |
4.9 |
0.003 |
0.989 |
|
BR-18-20 |
337 |
338 |
1 |
0.0243 |
0.0607 |
0.009 |
14.6 |
0.0069 |
0.958 |
|
BR-18-20 |
338 |
339 |
1 |
0.161 |
0.0736 |
0.011 |
13.1 |
0.0023 |
1.491 |
|
BR-18-20 |
339 |
340 |
1 |
0.291 |
0.142 |
0.057 |
39.8 |
0.0059 |
4.168 |
|
BR-18-20 |
340 |
341 |
1 |
0.257 |
0.107 |
0.025 |
18.8 |
0.0028 |
1.582 |
|
BR-18-20 |
341 |
342.4 |
1.4 |
0.176 |
0.109 |
0.008 |
36.4 |
0.0067 |
0.776 |
|
BR-18-20 |
342.4 |
344 |
1.6 |
0.0467 |
0.01 |
0.005 |
7.9 |
0.0029 |
0.274 |
|
BR-18-20 |
344 |
346 |
2 |
0.0094 |
0.0029 |
<0.005 |
1.5 |
0.0024 |
0.183 |
|
BR-18-20 |
346 |
348 |
2 |
0.0121 |
0.0007 |
<0.005 |
<0.5 |
0.0003 |
0.076 |
|
BR-18-20 |
348 |
350 |
2 |
0.0108 |
0.0016 |
<0.005 |
<0.5 |
0.0038 |
0.091 |
|
BR-18-20 |
350 |
352 |
2 |
0.0083 |
0.0012 |
<0.005 |
<0.5 |
0.0018 |
0.228 |
|
BR-18-20 |
352 |
354 |
2 |
0.0081 |
0.0014 |
<0.005 |
<0.5 |
0.0036 |
0.076 |
|
BR-18-20 |
354 |
356 |
2 |
0.0071 |
0.0008 |
<0.005 |
<0.5 |
0.001 |
0.076 |
|
BR-18-20 |
356 |
357 |
1 |
0.0069 |
0.001 |
<0.005 |
<0.5 |
0.0028 |
0.091 |
|
BR-18-20 |
357 |
358.8 |
1.8 |
0.0074 |
0.0008 |
<0.005 |
<0.5 |
0.0005 |
0.137 |
|
BR-18-20 |
358.8 |
360 |
1.2 |
0.0071 |
0.0008 |
<0.005 |
<0.5 |
0.0013 |
0.076 |
|
BR-18-20 |
360 |
361 |
1 |
0.0077 |
0.0008 |
0.007 |
<0.5 |
0.0035 |
0.046 |
|
BR-18-20 |
361 |
362.2 |
1.2 |
0.0073 |
0.0009 |
<0.005 |
<0.5 |
0.0018 |
0.091 |
|
BR-18-20 |
362.2 |
364 |
1.8 |
0.0073 |
0.0009 |
<0.005 |
<0.5 |
0.001 |
0.076 |
|
BR-18-20 |
364 |
366 |
2 |
0.0062 |
0.0008 |
<0.005 |
<0.5 |
0.0024 |
0.061 |
|
BR-18-20 |
366 |
368 |
2 |
0.0057 |
0.0006 |
<0.005 |
<0.5 |
0.001 |
0.076 |
|
BR-18-20 |
368 |
370 |
2 |
0.0054 |
0.0006 |
<0.005 |
<0.5 |
0.0016 |
0.061 |
|
BR-18-20 |
370 |
372 |
2 |
0.0068 |
0.0005 |
<0.005 |
<0.5 |
0.0065 |
0.106 |
|
BR-18-20 |
372 |
374 |
2 |
0.0071 |
0.0005 |
<0.005 |
<0.5 |
0.0022 |
0.122 |
|
BR-18-20 |
374 |
376 |
2 |
0.0052 |
0.0006 |
<0.005 |
<0.5 |
0.0012 |
0.106 |
|
BR-18-20 |
376 |
378 |
2 |
0.0058 |
0.0007 |
0.007 |
<0.5 |
0.0005 |
0.091 |
|
BR-18-20 |
378 |
380 |
2 |
0.0058 |
0.0008 |
0.006 |
<0.5 |
0.0011 |
0.091 |
|
BR-18-20 |
380 |
380.9 |
0.9 |
0.0046 |
0.0005 |
0.007 |
<0.5 |
0.0031 |
0.03 |
|
BR-18-20 |
380.9 |
382.4 |
1.5 |
0.0065 |
0.0008 |
0.008 |
<0.5 |
0.0013 |
0.076 |
|
BR-18-20 |
382.4 |
384 |
1.6 |
0.0048 |
0.0004 |
0.009 |
<0.5 |
0.0018 |
0.183 |
|
BR-18-20 |
384 |
386 |
2 |
0.005 |
0.0003 |
<0.005 |
<0.5 |
0.0006 |
0.076 |
|
BR-18-20 |
386 |
388 |
2 |
0.0072 |
0.0011 |
0.009 |
<0.5 |
0.0034 |
0.061 |
|
BR-18-20 |
388 |
390 |
2 |
0.006 |
0.0012 |
0.014 |
<0.5 |
0.0006 |
0.046 |
|
BR-18-20 |
390 |
392 |
2 |
0.0055 |
0.0009 |
0.009 |
<0.5 |
0.0019 |
0.046 |
|
BR-18-20 |
392 |
394 |
2 |
0.0046 |
0.0006 |
0.02 |
<0.5 |
0.0023 |
0.046 |
|
BR-18-20 |
394 |
396 |
2 |
0.0064 |
0.0006 |
0.022 |
<0.5 |
0.0016 |
0.046 |
|
BR-18-20 |
396 |
398 |
2 |
0.0067 |
0.0007 |
0.009 |
<0.5 |
0.0011 |
0.046 |
|
BR-18-20 |
398 |
400 |
2 |
0.0056 |
0.0006 |
0.015 |
<0.5 |
0.0005 |
0.046 |
|
BR-18-20 |
400 |
402 |
2 |
0.0057 |
0.0003 |
0.009 |
<0.5 |
0.0012 |
0.03 |
|
BR-18-20 |
402 |
404 |
2 |
0.0062 |
0.0003 |
0.008 |
<0.5 |
0.0006 |
0.046 |
|
BR-18-20 |
404 |
406 |
2 |
0.0061 |
0.0005 |
0.008 |
<0.5 |
0.0006 |
0.091 |
|
BR-18-20 |
406 |
408 |
2 |
0.0081 |
0.0005 |
0.009 |
<0.5 |
0.002 |
0.03 |
|
BR-18-20 |
408 |
410 |
2 |
0.0072 |
0.0006 |
0.006 |
<0.5 |
0.0021 |
0.091 |
|
BR-18-20 |
410 |
412 |
2 |
0.0079 |
0.0006 |
0.005 |
<0.5 |
0.002 |
0.076 |
|
BR-18-20 |
412 |
414 |
2 |
0.007 |
0.001 |
0.005 |
<0.5 |
0.0021 |
0.046 |
|
BR-18-20 |
414 |
416 |
2 |
0.011 |
0.0017 |
0.043 |
<0.5 |
0.0041 |
0.152 |
|
BR-18-20 |
416 |
418 |
2 |
0.0084 |
0.0017 |
0.018 |
<0.5 |
0.0026 |
0.319 |
|
BR-18-20 |
418 |
420 |
2 |
0.0102 |
0.0021 |
0.009 |
<0.5 |
0.0019 |
0.137 |
|
BR-18-20 |
420 |
422 |
2 |
0.0168 |
0.0019 |
0.015 |
<0.5 |
0.0011 |
0.046 |
|
BR-18-20 |
422 |
432 |
10 |
No sample |
|||||
|
BR-18-20 |
432 |
434 |
2 |
0.0091 |
0.0009 |
0.008 |
<0.5 |
0.001 |
0.03 |
|
BR-18-20 |
434 |
435 |
1 |
0.0268 |
0.0012 |
0.005 |
<0.5 |
0.0006 |
0.122 |
|
BR-18-20 |
435 |
436.3 |
1.3 |
0.0307 |
0.0017 |
0.007 |
<0.5 |
0.0008 |
0.578 |
|
BR-18-20 |
436.3 |
437 |
0.7 |
0.0085 |
0.0076 |
0.046 |
<0.5 |
0.002 |
0.106 |
|
BR-18-20 |
437 |
438.3 |
1.3 |
0.0141 |
0.0033 |
0.022 |
<0.5 |
0.0006 |
0.091 |
|
BR-18-20 |
438.3 |
440 |
1.7 |
0.0113 |
0.0028 |
0.011 |
<0.5 |
0.0012 |
0.046 |
|
BR-18-20 |
440 |
442 |
2 |
0.0161 |
0.0018 |
0.005 |
<0.5 |
0.0009 |
0.228 |
|
BR-18-20 |
442 |
444 |
2 |
0.0119 |
0.0017 |
0.011 |
<0.5 |
0.0013 |
0.091 |
|
BR-18-20 |
444 |
446 |
2 |
0.0104 |
0.0018 |
0.005 |
<0.5 |
0.0011 |
0.091 |
|
BR-18-20 |
446 |
448 |
2 |
0.0121 |
0.0045 |
<0.005 |
<0.5 |
0.0014 |
0.076 |
|
BR-18-20 |
448 |
450 |
2 |
0.0121 |
0.0106 |
0.022 |
0.5 |
0.0017 |
0.106 |
|
BR-18-20 |
450 |
451 |
1 |
0.0171 |
0.0042 |
0.014 |
<0.5 |
0.0008 |
0.502 |
|
BR-18-20 |
451 |
452.6 |
1.6 |
0.215 |
0.0088 |
0.017 |
0.8 |
0.0066 |
0.167 |
|
BR-18-20 |
452.6 |
454 |
1.4 |
0.0165 |
0.0078 |
0.01 |
0.5 |
0.0203 |
0.441 |
|
BR-18-20 |
454 |
456 |
2 |
0.0089 |
0.0027 |
0.009 |
<0.5 |
0.004 |
0.122 |
|
BR-18-20 |
456 |
457 |
1 |
0.0088 |
0.0008 |
<0.005 |
<0.5 |
0.0002 |
0.122 |
|
BR-18-20 |
457 |
458.4 |
1.4 |
0.0101 |
0.0008 |
<0.005 |
<0.5 |
0.0078 |
0.198 |
|
BR-18-20 |
458.4 |
460 |
1.6 |
0.0086 |
0.0009 |
0.008 |
<0.5 |
0.0002 |
0.076 |
|
BR-18-20 |
460 |
461 |
1 |
0.0094 |
0.0006 |
0.007 |
<0.5 |
0.0001 |
0.152 |
|
BR-18-20 |
461 |
462.3 |
1.3 |
0.0094 |
0.0011 |
<0.005 |
<0.5 |
0.0001 |
0.122 |
|
BR-18-20 |
462.3 |
464 |
1.7 |
0.0108 |
0.0012 |
<0.005 |
<0.5 |
0.0012 |
0.152 |
|
BR-18-20 |
464 |
466 |
2 |
0.0083 |
0.0036 |
0.009 |
<0.5 |
0.002 |
0.091 |
|
BR-18-20 |
466 |
468 |
2 |
0.0088 |
0.0027 |
<0.005 |
<0.5 |
0.0018 |
0.076 |
|
BR-18-20 |
468 |
469 |
1 |
0.0182 |
0.0045 |
0.042 |
0.5 |
0.0021 |
0.152 |
|
BR-18-20 |
469 |
470.2 |
1.2 |
0.0317 |
0.0033 |
0.019 |
<0.5 |
0.0015 |
0.213 |
|
BR-18-20 |
470.2 |
471.4 |
1.2 |
No sample |
|||||
|
BR-18-20 |
471.4 |
472.5 |
1.1 |
0.0085 |
0.0005 |
<0.005 |
<0.5 |
0.0002 |
0.046 |
|
BR-18-20 |
472.5 |
474.5 |
2 |
0.0111 |
0.0008 |
<0.005 |
<0.5 |
0.0002 |
0.091 |
|
BR-18-20 |
474.5 |
476.5 |
2 |
0.0101 |
0.001 |
<0.005 |
<0.5 |
0.0003 |
0.106 |
|
BR-18-20 |
476.5 |
478.5 |
2 |
0.009 |
0.0011 |
<0.005 |
<0.5 |
0.0018 |
0.183 |
|
BR-18-20 |
478.5 |
480.5 |
2 |
0.0107 |
0.0015 |
0.007 |
<0.5 |
0.0008 |
0.152 |
|
BR-18-20 |
480.5 |
482.5 |
2 |
0.0101 |
0.0021 |
0.009 |
<0.5 |
0.0015 |
0.411 |
|
BR-18-20 |
482.5 |
484.5 |
2 |
0.0296 |
0.0163 |
0.01 |
1.2 |
0.0044 |
0.122 |
|
BR-18-20 |
484.5 |
485.1 |
0.6 |
0.013 |
0.0029 |
<0.005 |
<0.5 |
0.0037 |
0.046 |
|
BR-18-20 |
485.1 |
486.5 |
1.4 |
0.0108 |
0.0037 |
<0.005 |
<0.5 |
0.0032 |
0.061 |
|
BR-18-20 |
486.5 |
488.5 |
2 |
0.0135 |
0.001 |
<0.005 |
<0.5 |
0.0013 |
0.046 |
|
BR-18-20 |
488.5 |
490.5 |
2 |
0.0121 |
0.0057 |
0.005 |
<0.5 |
0.0227 |
0.213 |
|
BR-18-20 |
490.5 |
492.5 |
2 |
0.0103 |
0.0053 |
0.005 |
<0.5 |
0.0011 |
0.122 |
|
BR-18-20 |
492.5 |
494.5 |
2 |
0.0112 |
0.0059 |
<0.005 |
<0.5 |
0.0046 |
0.091 |
|
BR-18-20 |
494.5 |
496.5 |
2 |
0.0103 |
0.0008 |
<0.005 |
<0.5 |
0.0012 |
0.061 |
|
BR-18-20 |
496.5 |
498.5 |
2 |
0.0124 |
0.0005 |
<0.005 |
<0.5 |
0.0007 |
0.076 |
|
BR-18-20 |
498.5 |
500 |
1.5 |
0.0136 |
0.0049 |
0.006 |
<0.5 |
0.0081 |
0.061 |
|
BR-18-20 |
500 |
501 |
1 |
0.0138 |
0.0019 |
<0.005 |
<0.5 |
0.0114 |
0.106 |
|
BR-18-20 |
501 |
502.1 |
1.1 |
0.0093 |
0.0035 |
<0.005 |
1 |
0.163 |
0.061 |
|
BR-18-20 |
502.1 |
504 |
1.9 |
0.0106 |
0.0013 |
<0.005 |
<0.5 |
0.066 |
0.076 |
|
BR-18-20 |
504 |
506 |
2 |
0.0116 |
0.0009 |
<0.005 |
<0.5 |
0.0119 |
0.152 |
|
BR-18-20 |
506 |
508 |
2 |
0.0124 |
0.0012 |
0.007 |
<0.5 |
0.0005 |
0.076 |
|
BR-18-20 |
508 |
510 |
2 |
0.0214 |
0.0144 |
0.005 |
<0.5 |
0.028 |
0.152 |
|
BR-18-20 |
510 |
512 |
2 |
0.0205 |
0.0154 |
0.007 |
0.7 |
0.0093 |
0.426 |
|
BR-18-20 |
512 |
513.4 |
1.4 |
0.0114 |
0.0028 |
0.01 |
<0.5 |
0.0112 |
0.106 |
|
BR-18-20 |
513.4 |
514.1 |
0.7 |
0.0119 |
0.0008 |
0.013 |
<0.5 |
0.0004 |
0.228 |
|
BR-18-20 |
514.1 |
515.7 |
1.6 |
0.0133 |
0.0013 |
0.006 |
<0.5 |
0.0014 |
0.122 |
|
BR-18-20 |
515.7 |
517 |
1.3 |
0.0093 |
0.0009 |
<0.005 |
<0.5 |
0.0002 |
0.061 |
|
BR-18-20 |
517 |
519 |
2 |
0.0091 |
0.0005 |
0.007 |
<0.5 |
0.0003 |
0.076 |
|
BR-18-20 |
519 |
521 |
2 |
0.0081 |
0.0007 |
0.006 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
521 |
522.6 |
1.6 |
0.0081 |
0.0005 |
<0.005 |
<0.5 |
0.0001 |
0.152 |
|
BR-18-20 |
522.6 |
524 |
1.4 |
0.0049 |
0.0012 |
0.006 |
<0.5 |
0.0004 |
0.137 |
|
BR-18-20 |
524 |
526 |
2 |
0.0122 |
0.0011 |
0.019 |
<0.5 |
0.002 |
0.106 |
|
BR-18-20 |
526 |
528 |
2 |
0.0132 |
0.0034 |
<0.005 |
<0.5 |
0.0018 |
0.061 |
|
BR-18-20 |
528 |
530 |
2 |
0.0136 |
0.0057 |
0.033 |
<0.5 |
0.0372 |
0.076 |
|
BR-18-20 |
530 |
532 |
2 |
0.0133 |
0.0028 |
0.009 |
<0.5 |
0.0021 |
0.167 |
|
BR-18-20 |
532 |
534 |
2 |
0.0112 |
0.0015 |
0.006 |
<0.5 |
0.0013 |
0.076 |
|
BR-18-20 |
534 |
536 |
2 |
0.0107 |
0.0012 |
<0.005 |
<0.5 |
0.0014 |
0.046 |
|
BR-18-20 |
536 |
537.7 |
1.7 |
0.0131 |
0.0022 |
0.007 |
<0.5 |
0.0023 |
0.274 |
|
BR-18-20 |
537.7 |
539 |
1.3 |
0.0079 |
0.0241 |
0.012 |
0.8 |
0.005 |
0.106 |
|
BR-18-20 |
539 |
541 |
2 |
0.0049 |
0.0026 |
0.011 |
<0.5 |
0.0004 |
0.061 |
|
BR-18-20 |
541 |
543 |
2 |
0.0079 |
0.0007 |
<0.005 |
<0.5 |
0.0002 |
0.061 |
|
BR-18-20 |
543 |
545 |
2 |
0.0099 |
0.0009 |
<0.005 |
<0.5 |
0.0002 |
0.061 |
|
BR-18-20 |
545 |
547 |
2 |
0.0051 |
0.0006 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
547 |
549 |
2 |
0.0059 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
549 |
551 |
2 |
0.004 |
0.0007 |
0.007 |
<0.5 |
0.0005 |
0.046 |
|
BR-18-20 |
551 |
553 |
2 |
0.0049 |
0.0018 |
<0.005 |
<0.5 |
0.0002 |
0.152 |
|
BR-18-20 |
553 |
555 |
2 |
0.0055 |
0.0008 |
<0.005 |
<0.5 |
0.0016 |
0.061 |
|
BR-18-20 |
555 |
557 |
2 |
0.005 |
0.001 |
<0.005 |
<0.5 |
0.0122 |
0.046 |
|
BR-18-20 |
557 |
558 |
1 |
0.0067 |
0.0018 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-18-20 |
558 |
560 |
2 |
0.0081 |
0.001 |
0.006 |
<0.5 |
0.0001 |
0.046 |
|
BR-18-20 |
560 |
562 |
2 |
0.0056 |
0.0026 |
0.014 |
<0.5 |
0.0019 |
0.076 |
|
BR-18-20 |
562 |
564 |
2 |
0.0843 |
0.0281 |
0.144 |
1 |
0.0142 |
0.259 |
|
BR-18-20 |
564 |
566 |
2 |
0.0035 |
0.0012 |
0.019 |
<0.5 |
0.0004 |
0.076 |
|
BR-18-20 |
566 |
568 |
2 |
0.0045 |
0.0014 |
0.007 |
<0.5 |
0.0012 |
0.122 |
|
BR-18-20 |
568 |
570 |
2 |
0.004 |
0.0011 |
0.005 |
<0.5 |
0.0003 |
0.091 |
|
BR-18-20 |
570 |
572 |
2 |
0.004 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
572 |
574 |
2 |
0.0062 |
0.0106 |
<0.005 |
1.6 |
0.0202 |
0.137 |
|
BR-18-20 |
574 |
576 |
2 |
0.0026 |
0.0031 |
0.017 |
0.6 |
0.0044 |
0.304 |
|
BR-18-20 |
576 |
578 |
2 |
0.0029 |
0.006 |
0.008 |
0.7 |
0.0091 |
0.122 |
|
BR-18-20 |
578 |
580 |
2 |
0.0114 |
0.0206 |
0.005 |
1.5 |
0.054 |
0.563 |
|
BR-18-20 |
580 |
582 |
2 |
0.0036 |
0.0023 |
0.006 |
<0.5 |
0.0009 |
0.137 |
|
BR-18-20 |
582 |
584 |
2 |
0.0059 |
0.0013 |
0.005 |
<0.5 |
0.0002 |
0.091 |
|
BR-18-20 |
584 |
586 |
2 |
0.005 |
0.001 |
<0.005 |
<0.5 |
0.0001 |
0.061 |
|
BR-18-20 |
586 |
587 |
1 |
0.0039 |
0.0009 |
0.007 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
587 |
588.3 |
1.3 |
0.0036 |
0.0016 |
0.022 |
<0.5 |
0.0002 |
0.076 |
|
BR-18-20 |
588.3 |
590 |
1.7 |
0.0058 |
0.0023 |
<0.005 |
<0.5 |
0.0001 |
0.167 |
|
BR-18-20 |
590 |
592 |
2 |
0.0057 |
0.0008 |
0.011 |
<0.5 |
0.0001 |
0.228 |
|
BR-18-20 |
592 |
594 |
2 |
0.0062 |
0.0008 |
0.008 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
594 |
596 |
2 |
0.0047 |
0.0008 |
0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
596 |
598 |
2 |
0.0034 |
0.0007 |
<0.005 |
<0.5 |
0.0001 |
0.091 |
|
BR-18-20 |
598 |
600 |
2 |
0.0056 |
0.0022 |
0.006 |
<0.5 |
0.0001 |
0.228 |
|
BR-18-20 |
600 |
602 |
2 |
0.0093 |
0.0016 |
0.026 |
<0.5 |
0.0001 |
0.228 |
|
BR-18-20 |
602 |
604 |
2 |
0.0055 |
0.0009 |
<0.005 |
<0.5 |
<0.0001 |
0.106 |
|
BR-18-20 |
604 |
606 |
2 |
0.0063 |
0.0028 |
<0.005 |
<0.5 |
0.0001 |
0.076 |
|
BR-18-20 |
606 |
607 |
1 |
0.0073 |
0.0019 |
0.014 |
<0.5 |
0.0001 |
0.122 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-20-20 |
225 |
227 |
2 |
0.0094 |
0.0049 |
0.054 |
2.9 |
0.0033 |
0.122 |
|
BR-20-20 |
227 |
228.2 |
1.2 |
0.0346 |
0.0852 |
0.024 |
7.1 |
0.0201 |
1.871 |
|
BR-20-20 |
228.2 |
229 |
0.8 |
1.56 |
1.58 |
0.537 |
112 |
0.291 |
53.091 |
|
BR-20-20 |
229 |
230 |
1 |
0.116 |
1.01 |
0.6 |
75.9 |
0.157 |
54.004 |
|
BR-20-20 |
230 |
231 |
1 |
0.739 |
1.55 |
0.618 |
85.2 |
0.424 |
38.335 |
|
BR-20-20 |
231 |
232 |
1 |
1.305 |
0.851 |
0.5 |
141 |
0.612 |
11.577 |
|
BR-20-20 |
232 |
233.2 |
1.2 |
1.105 |
0.423 |
0.4 |
46 |
0.0431 |
4.853 |
|
BR-20-20 |
233.2 |
234 |
0.8 |
1.505 |
2.64 |
0.666 |
164 |
0.796 |
31.185 |
|
BR-20-20 |
234 |
235 |
1 |
3.35 |
2.74 |
0.858 |
229 |
0.993 |
28.295 |
|
BR-20-20 |
235 |
235.5 |
0.5 |
2.64 |
2.33 |
0.719 |
226 |
0.931 |
30.197 |
|
BR-20-20 |
235.5 |
237 |
1.5 |
1.4 |
0.929 |
0.327 |
50.2 |
0.185 |
8.291 |
|
BR-20-20 |
237 |
238 |
1 |
3.14 |
2.07 |
0.502 |
40.7 |
0.562 |
1.323 |
|
BR-20-20 |
238 |
239 |
1 |
0.259 |
0.181 |
0.109 |
7.6 |
0.0662 |
2.647 |
|
BR-20-20 |
239 |
240 |
1 |
0.488 |
0.366 |
0.15 |
8.1 |
0.0676 |
0.761 |
|
BR-20-20 |
240 |
241 |
1 |
0.395 |
0.303 |
0.111 |
7.9 |
0.154 |
0.046 |
|
BR-20-20 |
241 |
241.5 |
0.5 |
0.207 |
0.0326 |
0.076 |
2 |
0.0117 |
1.552 |
|
BR-20-20 |
241.5 |
243 |
1.5 |
0.0125 |
0.0073 |
0.007 |
<0.5 |
0.004 |
0.882 |
|
BR-20-20 |
243 |
245 |
2 |
0.0109 |
0.0051 |
0.009 |
<0.5 |
0.0034 |
0.213 |
|
BR-20-20 |
245 |
247 |
2 |
0.0114 |
0.0127 |
0.007 |
<0.5 |
0.0037 |
0.122 |
|
BR-20-20 |
247 |
248.7 |
1.7 |
0.0097 |
0.0089 |
0.011 |
<0.5 |
0.0033 |
0.061 |
|
BR-20-20 |
248.7 |
250.2 |
1.5 |
0.0159 |
0.0015 |
<0.005 |
<0.5 |
0.0028 |
0.03 |
|
BR-20-20 |
250.2 |
252.2 |
2 |
0.0245 |
0.0018 |
<0.005 |
<0.5 |
0.0086 |
0.015 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-22-20 |
0 |
184 |
No sample |
||||||
|
BR-22-20 |
184 |
186 |
2 |
0.0409 |
0.0069 |
0.039 |
0.9 |
0.03 |
0.426 |
|
BR-22-20 |
186 |
188 |
2 |
0.0227 |
0.0035 |
0.018 |
<0.5 |
0.0011 |
0.517 |
|
BR-22-20 |
188 |
190 |
2 |
0.41 |
0.1795 |
0.109 |
4.8 |
0.001 |
3.21 |
|
BR-22-20 |
190 |
192 |
2 |
0.031 |
0.002 |
0.016 |
<0.5 |
0.0012 |
0.152 |
|
BR-22-20 |
192 |
194 |
2 |
0.0232 |
0.0008 |
0.011 |
<0.5 |
0.001 |
0.03 |
|
BR-22-20 |
194 |
196 |
2 |
0.0103 |
0.0016 |
0.01 |
<0.5 |
0.0006 |
0.046 |
|
BR-22-20 |
196 |
198 |
2 |
0.0179 |
0.0008 |
0.017 |
<0.5 |
0.0006 |
0.008 |
|
BR-22-20 |
198 |
200 |
2 |
0.004 |
0.0053 |
0.02 |
<0.5 |
0.0009 |
0.046 |
|
BR-22-20 |
200 |
202 |
2 |
0.0092 |
0.0017 |
0.018 |
<0.5 |
0.0007 |
0.015 |
|
BR-22-20 |
202 |
204 |
2 |
0.0097 |
0.0032 |
0.038 |
<0.5 |
0.0015 |
0.015 |
|
BR-22-20 |
204 |
206 |
2 |
0.0102 |
0.0045 |
0.101 |
<0.5 |
<0.005 |
0.015 |
|
BR-22-20 |
206 |
208 |
2 |
0.0197 |
0.0031 |
0.09 |
<0.5 |
0.0013 |
0.03 |
|
BR-22-20 |
208 |
210 |
2 |
0.0085 |
0.0058 |
0.12 |
<0.5 |
0.0022 |
0.183 |
|
BR-22-20 |
210 |
212 |
2 |
0.0072 |
0.0211 |
0.176 |
0.7 |
0.0091 |
0.624 |
|
BR-22-20 |
212 |
214 |
2 |
0.0139 |
0.0082 |
0.113 |
0.6 |
0.0019 |
0.106 |
|
BR-22-20 |
214 |
216 |
2 |
0.143 |
0.246 |
0.329 |
2.1 |
0.0418 |
1.263 |
|
BR-22-20 |
216 |
218 |
2 |
0.0387 |
0.0358 |
0.4 |
2.1 |
0.133 |
0.046 |
|
BR-22-20 |
218 |
219.7 |
1.7 |
0.177 |
0.0265 |
0.256 |
1.5 |
0.0204 |
0.106 |
|
BR-22-20 |
219.7 |
220.7 |
1 |
0.169 |
0.291 |
0.905 |
8.6 |
0.472 |
0.046 |
|
BR-22-20 |
220.7 |
221.7 |
1 |
0.0183 |
0.009 |
0.178 |
1.3 |
0.0041 |
0.015 |
|
BR-22-20 |
221.7 |
222.7 |
1 |
0.0176 |
0.0111 |
0.143 |
0.8 |
0.0037 |
0.03 |
|
BR-22-20 |
222.7 |
223.7 |
1 |
0.0787 |
0.307 |
0.575 |
5.1 |
0.16 |
0.228 |
|
BR-22-20 |
223.7 |
224.7 |
1 |
0.104 |
0.1335 |
0.481 |
3.8 |
0.0502 |
1.187 |
|
BR-22-20 |
224.7 |
225.7 |
1 |
0.236 |
0.1465 |
0.921 |
7.8 |
0.117 |
1.719 |
|
BR-22-20 |
225.7 |
226.3 |
0.6 |
0.221 |
0.182 |
1.185 |
7.9 |
0.0752 |
0.7 |
|
BR-22-20 |
226.3 |
227 |
0.7 |
0.135 |
0.975 |
1.865 |
11.4 |
0.326 |
4.549 |
|
BR-22-20 |
227 |
228 |
1 |
0.211 |
0.0523 |
0.482 |
6.2 |
0.0829 |
6.648 |
|
BR-22-20 |
228 |
229 |
1 |
0.39 |
0.1055 |
0.652 |
16 |
0.281 |
4.853 |
|
BR-22-20 |
229 |
230 |
1 |
0.0372 |
0.0082 |
0.153 |
0.7 |
0.0108 |
0.122 |
|
BR-22-20 |
230 |
231 |
1 |
0.0518 |
0.0081 |
0.152 |
1 |
0.0092 |
0.624 |
|
BR-22-20 |
231 |
232 |
1 |
0.663 |
0.073 |
1.05 |
11.8 |
0.144 |
9.432 |
|
BR-22-20 |
232 |
233 |
1 |
0.209 |
0.0739 |
0.553 |
9 |
0.0355 |
3.453 |
|
BR-22-20 |
233 |
234 |
1 |
0.246 |
0.119 |
0.489 |
16.4 |
0.015 |
2.16 |
|
BR-22-20 |
234 |
235 |
1 |
0.0222 |
0.0223 |
0.502 |
5.1 |
0.0093 |
0.837 |
|
BR-22-20 |
235 |
236 |
1 |
0.0232 |
0.0127 |
0.555 |
2 |
0.0081 |
0.806 |
|
BR-22-20 |
236 |
237 |
1 |
0.0256 |
0.026 |
0.152 |
1.4 |
0.0051 |
0.061 |
|
BR-22-20 |
237 |
237.7 |
0.7 |
0.0294 |
0.051 |
0.383 |
3.7 |
0.0507 |
0.35 |
|
BR-22-20 |
237.7 |
238.2 |
0.5 |
0.281 |
0.169 |
1.83 |
33.3 |
2.19 |
1.78 |
|
BR-22-20 |
238.2 |
239.2 |
1 |
0.0196 |
0.0689 |
0.173 |
1.8 |
0.0493 |
0.685 |
|
BR-22-20 |
239.2 |
240.4 |
1.2 |
0.0983 |
0.131 |
0.927 |
7.6 |
0.122 |
2.464 |
|
BR-22-20 |
240.4 |
241.2 |
0.8 |
0.087 |
0.079 |
2.3 |
23.7 |
0.418 |
2.038 |
|
BR-22-20 |
241.2 |
242.1 |
0.9 |
0.0946 |
0.0209 |
0.414 |
3.8 |
0.175 |
5.218 |
|
BR-22-20 |
242.1 |
243.2 |
1.1 |
0.0034 |
0.0159 |
0.318 |
1.4 |
0.0057 |
1.917 |
|
BR-22-20 |
243.2 |
244.1 |
0.9 |
0.151 |
0.037 |
1.075 |
13.2 |
1.265 |
0.259 |
|
BR-22-20 |
244.1 |
245 |
0.9 |
0.141 |
0.0044 |
0.13 |
<0.5 |
0.0379 |
0.913 |
|
BR-22-20 |
245 |
246 |
1 |
0.231 |
0.0067 |
0.166 |
0.9 |
0.0107 |
2.951 |
|
BR-22-20 |
246 |
247 |
1 |
0.0472 |
0.0074 |
0.132 |
0.5 |
0.0038 |
0.898 |
|
BR-22-20 |
247 |
248 |
1 |
0.0043 |
0.0043 |
0.044 |
<0.5 |
0.0012 |
0.015 |
|
BR-22-20 |
248 |
249 |
1 |
0.0043 |
0.0087 |
0.203 |
0.6 |
0.0042 |
0.243 |
|
BR-22-20 |
249 |
250 |
1 |
0.0353 |
0.0115 |
0.189 |
<0.5 |
0.0101 |
0.137 |
|
BR-22-20 |
250 |
251 |
1 |
0.111 |
0.0125 |
0.237 |
1 |
0.0071 |
0.35 |
|
BR-22-20 |
251 |
252 |
1 |
0.0209 |
0.0055 |
0.107 |
<0.5 |
0.0014 |
0.167 |
|
BR-22-20 |
252 |
253 |
1 |
0.193 |
0.009 |
0.334 |
2 |
0.0116 |
4.944 |
|
BR-22-20 |
253 |
254 |
1 |
0.13 |
0.0073 |
0.337 |
1.1 |
0.0042 |
10.497 |
|
BR-22-20 |
254 |
255.2 |
1.2 |
0.12 |
0.0125 |
0.488 |
1.6 |
0.0153 |
5.431 |
|
BR-22-20 |
255.2 |
256 |
0.8 |
0.213 |
0.0086 |
0.178 |
<0.5 |
0.0031 |
0.091 |
|
BR-22-20 |
256 |
257 |
1 |
0.21 |
0.0156 |
0.345 |
<0.5 |
0.0044 |
0.396 |
|
BR-22-20 |
257 |
258 |
1 |
0.216 |
0.0056 |
0.138 |
<0.5 |
0.0029 |
0.243 |
|
BR-22-20 |
258 |
259 |
1 |
0.651 |
0.0522 |
0.279 |
2.5 |
0.0286 |
0.061 |
|
BR-22-20 |
259 |
260 |
1 |
0.928 |
0.439 |
2.42 |
17.9 |
0.1115 |
0.958 |
|
BR-22-20 |
260 |
261 |
1 |
1.675 |
0.405 |
1.45 |
39.3 |
0.352 |
0.213 |
|
BR-22-20 |
261 |
262 |
1 |
0.606 |
0.201 |
0.395 |
11 |
0.047 |
1.141 |
|
BR-22-20 |
262 |
263 |
1 |
0.213 |
0.0807 |
0.32 |
3.6 |
0.0269 |
0.106 |
|
BR-22-20 |
263 |
264 |
1 |
0.34 |
0.132 |
0.751 |
5.1 |
0.0511 |
0.806 |
|
BR-22-20 |
264 |
265 |
1 |
0.0803 |
0.0116 |
0.537 |
2.6 |
0.249 |
0.578 |
|
BR-22-20 |
265 |
266 |
1 |
0.0218 |
0.0104 |
0.344 |
0.9 |
0.0047 |
0.259 |
|
BR-22-20 |
266 |
267 |
1 |
0.0746 |
0.0409 |
0.365 |
2.9 |
0.0275 |
0.7 |
|
BR-22-20 |
267 |
268 |
1 |
0.0517 |
0.0042 |
0.174 |
<0.5 |
0.0024 |
0.061 |
|
BR-22-20 |
268 |
269 |
1 |
0.022 |
0.0064 |
0.144 |
<0.5 |
0.0022 |
0.259 |
|
BR-22-20 |
269 |
270 |
1 |
0.109 |
0.0062 |
0.235 |
1.8 |
0.0034 |
0.274 |
|
BR-22-20 |
270 |
271 |
1 |
0.038 |
0.0045 |
0.153 |
1 |
0.0021 |
0.122 |
|
BR-22-20 |
271 |
272 |
1 |
0.137 |
0.0528 |
0.776 |
9.9 |
0.183 |
0.259 |
|
BR-22-20 |
272 |
273 |
1 |
0.0876 |
0.0763 |
0.626 |
5.9 |
0.073 |
0.106 |
|
BR-22-20 |
273 |
274 |
1 |
0.0695 |
0.0559 |
0.877 |
6.1 |
0.0096 |
0.152 |
|
BR-22-20 |
274 |
275 |
1 |
0.435 |
0.0184 |
0.619 |
4.3 |
0.0089 |
0.608 |
|
BR-22-20 |
275 |
276 |
1 |
0.596 |
0.0352 |
1.075 |
8.6 |
0.0222 |
0.289 |
|
BR-22-20 |
276 |
277 |
1 |
0.0539 |
0.0059 |
0.173 |
0.8 |
0.0044 |
0.243 |
|
BR-22-20 |
277 |
278 |
1 |
0.0724 |
0.0117 |
0.201 |
1.5 |
0.0086 |
0.319 |
|
BR-22-20 |
278 |
278.3 |
0.3 |
0.0113 |
0.0126 |
0.45 |
3.1 |
0.0074 |
0.958 |
|
BR-22-20 |
278.3 |
280 |
1.7 |
0.0168 |
0.0077 |
0.132 |
4.2 |
0.0026 |
0.152 |
|
BR-22-20 |
280 |
282 |
2 |
0.0135 |
0.0089 |
0.065 |
1.8 |
0.0024 |
0.122 |
|
BR-22-20 |
282 |
284 |
2 |
0.394 |
0.102 |
0.06 |
5.2 |
0.024 |
0.335 |
|
BR-22-20 |
284 |
286 |
2 |
0.237 |
0.0667 |
0.084 |
3.3 |
0.0073 |
1.232 |
|
BR-22-20 |
286 |
288 |
2 |
0.138 |
0.0371 |
0.04 |
2.1 |
0.0053 |
0.624 |
|
BR-22-20 |
288 |
290 |
2 |
0.0785 |
0.0155 |
0.032 |
0.7 |
0.0014 |
0.106 |
|
BR-22-20 |
290 |
292 |
2 |
0.208 |
0.0161 |
0.027 |
1.2 |
0.0047 |
0.715 |
|
BR-22-20 |
292 |
294 |
2 |
0.184 |
0.007 |
0.025 |
0.6 |
0.001 |
0.578 |
|
BR-22-20 |
294 |
295.6 |
1.6 |
0.0341 |
0.0031 |
0.023 |
0.5 |
0.0011 |
0.076 |
|
BR-22-20 |
295.6 |
297 |
1.4 |
0.0473 |
0.0115 |
0.022 |
<0.5 |
0.0022 |
0.076 |
|
BR-22-20 |
297 |
299 |
2 |
0.0093 |
0.005 |
0.03 |
0.5 |
0.0011 |
0.046 |
|
BR-22-20 |
299 |
301 |
2 |
0.0848 |
0.0092 |
0.025 |
<0.5 |
0.0008 |
0.046 |
|
BR-22-20 |
301 |
303 |
2 |
0.0683 |
0.0834 |
0.015 |
1 |
0.0006 |
0.076 |
|
BR-22-20 |
303 |
305 |
2 |
0.0654 |
0.0041 |
0.029 |
0.9 |
0.0009 |
0.091 |
|
BR-22-20 |
305 |
307 |
2 |
0.253 |
0.0385 |
0.033 |
6.9 |
0.0036 |
0.472 |
|
BR-22-20 |
307 |
309 |
2 |
1.57 |
0.392 |
0.041 |
30.7 |
0.0208 |
3.195 |
|
BR-22-20 |
309 |
311 |
2 |
0.996 |
0.238 |
0.036 |
24.5 |
0.0087 |
4.123 |
|
BR-22-20 |
311 |
312.7 |
1.7 |
0.592 |
0.0896 |
0.041 |
16.5 |
0.0097 |
2.495 |
|
Hole ID |
From |
To |
Interval |
Zn % |
Pb % |
Au g/t |
Ag g/t |
Cu % |
BaSO4 |
|
BR-23-20 |
0 |
320 |
No sample |
||||||
|
BR-23-20 |
320 |
322 |
2 |
0.0139 |
0.0024 |
0.01 |
<0.5 |
0.0038 |
0.243 |
|
BR-23-20 |
322 |
324 |
2 |
0.012 |
0.0029 |
0.005 |
<0.5 |
0.0007 |
0.548 |
|
BR-23-20 |
324 |
325.7 |
1.7 |
0.0182 |
0.578 |
0.381 |
6.9 |
0.0109 |
51.418 |
|
BR-23-20 |
325.7 |
326.4 |
0.7 |
0.0233 |
0.586 |
0.363 |
11.1 |
0.0109 |
90.057 |
|
BR-23-20 |
326.4 |
327 |
0.6 |
0.11 |
0.0411 |
0.353 |
3.1 |
0.0035 |
80.474 |
|
BR-23-20 |
327 |
328 |
1 |
0.0063 |
0.401 |
0.348 |
5.6 |
0.0052 |
80.93 |
|
BR-23-20 |
328 |
329 |
1 |
0.0209 |
0.844 |
2.5 |
123 |
0.0942 |
75.149 |
|
BR-23-20 |
329 |
330 |
1 |
4.33 |
12.9 |
1.105 |
963 |
0.973 |
68.152 |
|
BR-23-20 |
330 |
331 |
1 |
0.622 |
8.26 |
2.04 |
741 |
0.872 |
80.017 |
|
BR-23-20 |
331 |
332 |
1 |
3.49 |
5.12 |
2.48 |
829 |
1.045 |
76.823 |
|
BR-23-20 |
332 |
333 |
1 |
10.9 |
7.05 |
1.09 |
325 |
0.641 |
66.782 |
|
BR-23-20 |
333 |
334 |
1 |
10.2 |
4.08 |
1.075 |
211 |
0.389 |
59.328 |
|
BR-23-20 |
334 |
335 |
1 |
8.15 |
3.65 |
0.891 |
268 |
0.314 |
58.568 |
|
BR-23-20 |
335 |
336 |
1 |
5.26 |
2.17 |
0.95 |
242 |
0.443 |
49.897 |
|
BR-23-20 |
336 |
337 |
1 |
2.2 |
1.15 |
1.09 |
196 |
0.319 |
42.747 |
|
BR-23-20 |
337 |
338 |
1 |
1.86 |
2.97 |
0.899 |
200 |
0.498 |
38.335 |
|
BR-23-20 |
338 |
338.6 |
0.6 |
1.88 |
1.55 |
1.035 |
274 |
0.409 |
11.257 |
|
BR-23-20 |
338.6 |
339.1 |
0.5 |
0.586 |
0.603 |
0.591 |
40.9 |
0.423 |
11.181 |
|
BR-23-20 |
339.1 |
340 |
0.9 |
0.365 |
0.107 |
0.516 |
26.9 |
1.06 |
47.158 |
|
BR-23-20 |
340 |
340.7 |
0.7 |
0.0495 |
0.11 |
0.15 |
4.4 |
0.111 |
2.693 |
|
BR-23-20 |
340.7 |
341.3 |
0.6 |
0.031 |
0.019 |
0.096 |
10.9 |
0.14 |
11.729 |
|
BR-23-20 |
341.3 |
342.6 |
1.3 |
0.992 |
0.804 |
0.421 |
49.7 |
0.273 |
7.028 |
|
BR-23-20 |
342.6 |
344 |
1.4 |
0.0234 |
0.0288 |
0.054 |
1 |
0.0033 |
3.879 |
|
BR-23-20 |
344 |
346 |
2 |
0.0216 |
0.006 |
0.008 |
<0.5 |
0.0081 |
0.289 |
|
BR-23-20 |
346 |
368 |
22 |
No sample |
|||||
APPENDIX 1: RUPICE MRE JORC TABLES
|
Section 1 Sampling Techniques and Data |
||
|
(Criteria in this section apply to all succeeding sections.)
|
||
|
Criteria |
JORC Code Explanation |
Commentary |
|
Sampling techniques |
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling. |
PQ3 and HQ3 diamond core was cut in half to provide a sample for assay typically weighing around 4-6kg. Samples were submitted to the ALS facility in Bor, Serbia for industry standard analytical analysis.
|
|
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. |
The half core and weight of the sample is sufficiently representative.
No calibration of any equipment was required as all samples were sent for assay by a commercial laboratory. |
|
|
Aspects of the determination of mineralisation that are Material to the Public Report. In cases where 'industry standard' work has been done this would be relatively simple (e.g. 'reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay'). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information. |
PQ3 and HQ3 diamond core was used to obtain nominally 1m samples from which 4-6kg of material was pulverised to produce sample for fire assay, ICP-MS and X-ray Fluorescence (XRF). |
|
|
Drilling techniques |
Drill type (e.g. core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face-sampling bit or other type, whether core is oriented and if so, by what method, etc).
|
|
|
Drill sample recovery |
Method of recording and assessing core and chip sample recoveries and results assessed. |
All core was logged for geology and RQD with recovery in the mineralised and sampled zone greater than 90%. The PQ3 and HQ3 diameter and sampling of half core ensured the representative nature of the samples. There is no observed relationship between sample recovery and grade, and with little to no loss of material there is considered to be little to no sample bias. |
|
Measures taken to maximise sample recovery and ensure representative nature of the samples. |
||
|
Whether a relationship exists between sample recovery and grade and whether sample bias may have occurred due to preferential loss/gain of fine/coarse material. |
||
|
Logging |
Whether core and chip samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. |
Diamond drill core samples have been geologically and geotechnically logged to a level of detail to support appropriate Mineral Resource estimation, mining studies and metallurgical studies. Not all drill holes penetrated the massive sulphide mineralisation, but all were used to guide the geological interpretations supporting the Mineral Resource estimates. |
|
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography.
|
All core is photographed, and logging is qualitative. |
|
|
The total length and percentage of the relevant intersections logged. |
All core is logged. |
|
|
Sub-sampling techniques and sample preparation |
If core, whether cut or sawn and whether quarter, half or all core taken. |
The diamond core was cut in half using a diamond saw. Nominally 1 in 30 samples was cut in quarters, and both halves analysed (for purposes of field duplicates). |
|
If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. |
Not applicable, as all samples are core. |
|
|
For all sample types, the nature, quality and appropriateness of the sample preparation technique. |
Collection of around 4-6kg of half core material with subsequent pulverisation of the total charge provided an appropriate and representative sample for analysis. Sample preparation was undertaken at the ALS laboratory in Bor, to industry best practice. |
|
|
Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. |
Whole rock blanks and certified standards (~1 in 15) were introduced to the sample run to ensure laboratory QAQC. Additionally, industry best practice was adopted by ALS for laboratory sub-sampling and the avoidance of any cross contamination. |
|
|
Measures taken to ensure that the sampling is representative of the in-situ material collected, including for instance results for field duplicate/second-half sampling. |
The half core sampling is considered a reasonable representation of the in-situ material. Nominally 1 in 30 samples were cut in quarters, and both halves analyses (for purposes of field duplicates). |
|
|
Whether sample sizes are appropriate to the grain size of the material being sampled. |
Sample size of around 4-6kg is considered to be appropriate to reasonably represent the material being tested. |
|
|
Quality of assay data and laboratory tests |
The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. |
Analyses were undertaken at the accredited laboratory of ALS in Bor, Serbia which has full industry certification. Multi elements were assayed by an ICP-AES technique following a four-acid digest. Gold was determined using a fire assay on a nominal 50g charge. Barite was determined from a lithium borate fusion followed by dissolution and ICP-AES analysis. Total sulphur was determined by Leco. All techniques were appropriate for the elements being determined. Samples are considered a partial digestion when using an aqua regia digest. |
|
For geophysical tools, spectrometers, handheld XRF instruments, etc, the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc. |
There was no reliance on determination of analysis by geophysical tools. |
|
|
Nature of quality control procedures adopted (e.g. standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established. |
Certified Reference Material ("CRM") appropriate for the elements being analysed were added at a rate better than 1 in 15. All results reported by ALS on the CRMs were better than 2 standard deviations (2SD), it is considered that acceptable levels of accuracy have been achieved. Additional lab checks were sent to SGS in Bor. To date,154 samples were submitted for check assaying from within the mineralised drill intercepts. The check assays correlated within tolerance to the original ALS assays. |
|
|
Verification of sampling and assaying |
The verification of significant intersections by either independent or alternative company personnel. |
There has been no independent logging of mineralised intervals, however, it has been logged by several company personnel and verified by senior staff. |
|
The use of twinned holes. |
None of the reported holes are twin holes. |
|
|
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. |
Data is stored on the Virtual Cloud and at various locations including Vares, Bosnia & Herzegovina and Cheltenham, UK. And is managed by gDat data solutions in an acQuire database, which is regularly backed-up. |
|
|
Discuss any adjustment to assay data. |
No adjustments were necessary. |
|
|
Location of data points |
Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation. |
Sampling sites were surveyed using Total Station to better than 0.05m accuracy in the local BiH coordinate system. |
|
Specification of the grid system used. |
The grid system used MGI 1901 / Balkans Zone 6. |
|
|
Quality and adequacy of topographic control. |
The topographic surface of the immediate area was generated from a LiDAR survey to an accuracy of approximately 0.05m. It is considered sufficiently accurate for the Company's current activities. |
|
|
Data spacing and distribution |
Data spacing for reporting of Exploration Results. |
Results from two drill holes are being reported. All samples were collected at 2m intervals down hole. |
|
Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. |
Drill hole spacing is deemed sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource classifications applied. |
|
|
Whether sample compositing has been applied. |
Sample composite was not employed. |
|
|
Orientation of data in relation to geological structure |
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known, considering the deposit type. |
Reported holes were drilled at an average declination and azimuth as stated in Table 2 of the accompanying report. The drill holes are considered to be reasonably orthogonal to the interpreted dip of the mineralisation, or close to it. |
|
If the relationship between the drilling orientation and the orientation of key mineralised structures is considered to have introduced a sampling bias, this should be assessed and reported if material. |
It is not considered that the drilling orientation has introduced a sampling bias, as the drilling is considered to be orthogonal to the strata bound mineralisation, or close to it. |
|
|
Sample security |
The measures taken to ensure sample security. |
Chain of Custody of digital data is managed by the Company. Physical material was stored on site and, when necessary, delivered to the assay laboratory. Thereafter laboratory samples were controlled by the nominated laboratory. All sample collection was controlled by digital sample control file(s) and hard-copy ticket books. |
|
Audits or reviews |
The results of any audits or reviews of sampling techniques and data. |
A Site and Laboratory (ALS and SGS, Bor) visit was made by Dr Belinda van Lente, an employee of CSA Global in January 2018. There were no material issues found for the 2017 drill campaign. |
|
Section 2: Reporting of Exploration Results |
||
|
(Criteria listed in the preceding section also apply to this section)
|
||
|
Criteria |
JORC Code explanation |
Commentary |
|
Mineral tenement and land tenure status |
Type, reference name/number, location and ownership including agreements or material issues with third parties such as joint ventures, partnerships, overriding royalties, native title interests, historical sites, wilderness or national park and environmental settings. |
The Rupice deposit is located within the Company's 100% owned Concession, No. 04-18-21389-1/13, located 13km west of Vares in Bosnia. There are no known material issues with any third party other than normal royalties due to the State. |
|
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
The Concession is in good standing with the governing authority and there is no known impediment to the Concession remaining in force until 2038 (25 years), subject to meeting all necessary reporting requirements. |
|
|
Exploration done by other parties |
Acknowledgment and appraisal of exploration by other parties. |
Modern exploration commenced with the work of Energoinvest in the late 1960s. During 1968-1969 underground development of 455m of drives and cross cuts were made, and 11 surface trenches dug for a total length of 93.5mm. Between 1980 and 1989, 49 holes were drilled for an advance of 5,690.8m. Sample material from all of these programs was routinely analysed for lead, zinc, and barite, and on occasion silver and gold. The deposit was the subject of a number of reserve estimates in the 1980s. This work is documented in many reports which are certified by those geoscientists and Institutes that undertook the work.
The work is considered to be of a standard equal to that prevalent within today's exploration industry. |
|
Geology |
Deposit type, geological setting and style of mineralisation. |
The host rocks at Rupice comprises Middle Triassic limestone, dolostone, calcareous and dolomitic marl, and a range of mostly fine-grained siliciclastic rocks including cherty mudstone, mudstone, siltstone and fine-grained sandstone. The main mineralised horizon is a brecciated dolomitic unit that dips at around 50o to the northeast and has been preferentially mineralised with base, precious and transitional metals. The Triassic sequence and has been intensely deformed both by early stage ductile shearing and late stage brittle faulting. The Rupice polymetallic mineralisation consists of sphalerite, galena, barite and chalcopyrite with gold, silver, tetrahedrite, boulangerite and bournonite, with pyrite. The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody. To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south. |
|
Drill hole information |
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: o easting and northing of the drill hole collar o elevation or RL (Reduced Level - elevation above sea level in metres) of the drill hole collar o dip and azimuth of the hole o downhole length and interception depth o hole length. If the exclusion of this information is justified on the basis that the information is not Material and this exclusion does not detract from the understanding of the report, the Competent Person should clearly explain why this is the case. |
167 diamond drill holes (38,134.65m) were used for the Mineral Resource estimate. This includes 46 historical holes (5,071.8m) not drilled by Adriatic Metals. All these holes were used to support the Mineral Resource estimate. The Mineral Resource estimate conveys the tenor of grade from the drill holes. |
|
Data aggregation methods |
In reporting Exploration Results, weighting averaging techniques, maximum and/or minimum grade truncations (e.g. cutting of high grades) and cut-off grades are usually Material and should be stated. |
No data aggregation methods were applied. |
|
Where aggregate intercepts incorporate short lengths of high-grade results and longer lengths of low-grade results, the procedure used for such aggregation should be stated and some typical examples of such aggregations should be shown in detail. |
Not applicable as no data aggregation methods were applied. |
|
|
The assumptions used for any reporting of metal equivalent values should be clearly stated. |
Equivalent explanations are described in the body of the text. |
|
|
Relationship between mineralisation widths and intercept lengths |
These relationships are particularly important in the reporting of Exploration Results. |
Exploration results are not being reported. |
|
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. |
The majority of the high-grade mineralisation is hosted within the brecciated dolomitic unit, which is offset and cut by northwest striking, westerly dipping syn-post mineral faulting. This faulting displaces the mineralised body up to 20 metres in places. Thickening of the central portion of the orebody occurs where these faults flexure and deform. Mineralised widths up to 65 metres true thickness are seen in the central portion of the orebody. To date, the massive sulphide mineralisation at Rupice has a defined strike length of 650 metres, with an average true-width thickness of around 20 metres. However, mineralisation at Rupice still remains open towards the north and down-dip to the south. Recent drilling by Eastern Mining was mostly inclined at between 70o and 80 o to the southwest, perpendicular to the deposit strike, and intersected the mineralisation reasonably orthogonally. |
|
|
If it is not known and only the downhole lengths are reported, there should be a clear statement to this effect (e.g. 'downhole length, true width not known'). |
True width intercepts in drill holes being reported are as follows - BR-10-20 - 1.7m BR-11-20 - 4.8m BR-12-20 - 2.9m BR-13-20 - 10.0m BR-17-20 - 1.4m BR-18-20 - 7.0m BR-20-20 - 9.8m BR-22-20 - 4.0m BR-23-20 - 7.0m |
|
|
Diagrams |
Appropriate maps and sections (with scales) and tabulations of intercepts should be included for any significant discovery being reported. These should include, but not be limited to a plan view of drill hole collar locations and appropriate sectional views. |
Relevant maps and diagrams are included in the body of the report. |
|
Balanced reporting |
Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high-grades and/or widths should be practiced to avoid misleading reporting of Exploration Results. |
Not applicable. All mineralised incepts are being reported. |
|
Other substantive exploration data |
Other exploration data, if meaningful and material, should be reported including (but not limited to): geological observations; geophysical survey results; geochemical survey results; bulk samples - size and method of treatment; metallurgical test results; bulk density, groundwater, geotechnical and rock characteristics; potential deleterious or contaminating substances. |
No substantive exploration data not already mentioned in the report has been used in the preparation of the Mineral Resource estimate. |
|
Further work |
The nature and scale of planned further work (e.g. tests for lateral extensions or depth extensions or large-scale step-out drilling). |
Further drilling is being undertaken for geotechnical and hydrological purposes, and extension exploration drilling. |
|
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
Diagrams have been included in the body of this report. |
|
|
Section 3: Estimation and Reporting of Mineral Resources |
||
|
(Criteria listed in section 1, and where relevant in section 2, also apply to this section)
|
||
|
Criteria |
JORC Code explanation |
Commentary |
|
Database integrity |
Measures taken to ensure that data has not been corrupted by, for example, transcription or keying errors, between its initial collection and its use for Mineral Resource estimation purposes. |
Data used in the Mineral Resource Estimate was provided as a validated Micromine database, which in turn was sourced from a validated database prepared by Adriatic Metals. The validation routines were employed to confirm validity of data. Key files (collar, survey, geology, assay) were validated to ensure that they were populated with the correct original data. All drill holes were logged to electronic logbooks. All drill hole collar, downhole survey and geological data are stored on the Virtual Cloud and at various locations including Vares, Bosnia & Herzegovina and Cheltenham, UK. And is managed by gDat data solutions in an acQuire database . The database is updated as new data become available. |
|
Data validation procedures used. |
The resultant database was validated for potential errors in Micromine software using specially designed processes. The following error checks were carried out during final database creation: · Missing collar coordinates. · Missing values in fields FROM and TO. · Cases when FROM values equal or exceed TO ones (FROM≥TO). · Data availability. The data availability was checked for each drill hole in the tables: - Collar coordinates - Sampling data - Downhole survey data - Lithological characteristics. · Duplicate drill hole numbers in the table of the drill hole collar coordinates. · Duplicate sampling intervals. · Duplicate downhole measurement data. · Duplicate intervals of the lithological column. · Sample "overlapping" (when the sample TO value exceeds FROM value of the next sample). · Negative-grade samples. Drill hole data was verified against source documentation. The surveyed drill holes were then also verified visually for consistency. The Competent Person is satisfied that database integrity is appropriate to support Mineral Resource estimation. |
|
|
Site visits |
Comment on any site visits undertaken by the Competent Person and the outcome of those visits. |
Phillip Fox is based on-site in Vares and was responsible for planning and implementation of the recent drilling programs, overseeing the preparation of the samples and their dispatch to the various laboratories. Mr. Fox assumes responsibility for the data components, QA/QC and geological interpretation. Dmitry Pertel assumes responsibility for the grade interpolation and reporting of the Mineral Resource estimate and has previously completed a site visit. |
|
If no site visits have been undertaken, indicate why this is the case. |
A site visit has been undertaken. |
|
|
Geological interpretation |
Confidence in (or conversely, the uncertainty of) the geological interpretation of the mineral deposit. |
Sufficient drilling has been conducted to reasonably interpret the geology and the polymetallic mineralisation. The mineralisation is traceable between numerous drill holes and drill sections. Interpretation of the deposit was based on the current understanding of the deposit geology. Each cross section generally spaced 20-30 m apart was displayed in Micromine software together with drill hole traces colour-coded according to grade values. The interpretation honoured modelled fault planes and interpretation of main geological structures. The mineralised structure of the deposit was interpreted and modelled using core logging data. The low-grade halo domain was interpreted to capture all mineralized samples, and based on the current understanding of the geological model. The fault zones were interpreted and modelled using geological logging. Cut-off grades for high grade domains were 10% for Zn, 3% for Pb, 25% for BaSO4, 1% for Cu, 2.5g/t for Au, and 110g/t for Ag. All cut-offs selected for interpretation were based on results of classical statistical analysis. The interpretation was independently reviewed by a consultant geologist. |
|
Nature of the data used and of any assumptions made. |
Geological logging in conjunction with assays has been used to interpret the mineralisation. The majority of holes were sampled at 2m intervals, with some more detailed sampling conducted. |
|
|
The effect, if any, of alternative interpretations on Mineral Resource estimation. |
Alternative interpretations are likely to materially impact on the Mineral Resource estimate on a local, but not global basis. No alternative interpretations were adopted at this stage of the project. |
|
|
The use of geology in guiding and controlling Mineral Resource estimation. |
Geological logging in conjunction with assays and results of the statistical analysis has been used to interpret the mineralisation. Available historical maps and sections have been used to guide interpretation. All internal waste was included into the interpreted mineralised bodies. |
|
|
The factors affecting continuity both of grade and geology. |
Continuity is affected by the nature of the host rocks, interpreted faults and limits of the drill holes. The Competent Person is satisfied that the geological interpretation is appropriate to support Mineral Resource estimation. |
|
|
Dimensions |
The extent and variability of the Mineral Resource expressed as length (along strike or otherwise), plan width, and depth below surface to the upper and lower limits of the Mineral Resource. |
The strike length is about 650m and width up to 250m. The combined thickness of the mineralised zones varies from several metres to 65m. Depth below surface is from 0 to 380 m, which is the lower limit of current drilling. The Competent Person is satisfied that the dimensions interpreted are appropriate to support Mineral Resource estimation. |
|
Estimation and modelling techniques |
The nature and appropriateness of the estimation technique(s) applied and key assumptions, including treatment of extreme grade values, domaining, interpolation parameters and maximum distance of extrapolation from data points. If a computer assisted estimation method was chosen include a description of computer software and parameters used. |
The Mineral Resource estimate was based on surface diamond drill core using ordinary kriging (OK) to form 5x5x5m blocks. The block model was constrained by wireframes modelled based on geology using sectional interpretation. Additional wireframing for each element for the high-grade domains within these geological wireframes (except for As, Sb and Hg) was completed. Weakly mineralised halos and fault zones used geological logging and multi-element assay data. The applied cut-off grades for high grade domains were:
Micromine software was used to generate the wireframes and for block modelling Hard boundaries were used between mineralised lenses at each domain. The drill hole data were composited to a target length of 2m based on the length analysis of raw intercepts. Geostatistical analysis was completed for all elements, and averaged long ranges were employed to justify the search ellipse - 102m along strike, 61m down dip and 31m across dip. Interpolation parameters were: Search pass 1: 2.5m by 2.5m by 2.5m. Minimum samples number - 1, minimum holes - 1, maximum samples number - 16. Search pass 1: 1/3 of the variogram log ranges. Minimum samples number - 3, minimum holes - 2, maximum samples number - 16. Search pass 2: 2/3 of the variogram log ranges. Minimum samples number - 3, minimum holes - 2, maximum samples number - 16. Search pass 3: Full semi-variogram ranges. Minimum samples - 3, maximum samples - 16, minimum holes 2. All subsequent search passes: incremented by full semi-variogram ranges in each direction. Minimum samples - 1, maximum samples - 16, minimum holes - 1. Block discretisation 2*2*2. The optimal parent cell size was selected in the course of block modelling based of 20x20m exploration drilling. Classical statistical analysis was used to identify grade domains for barite, gold and silver. The Competent Person is satisfied that estimation and modelling techniques are appropriate to support Mineral Resource estimation. |
|
The availability of check estimates, previous estimates and/or mine production records and whether the MRE takes appropriate account of such data. |
Previous JORC-compliant Mineral Resources were estimated by CSA Global in July 2019. The current estimate is about 32% higher in tonnage and about 22% lower grades due to the modelling methodology and domaining applied. Mine production results were not available. |
|
|
The assumptions made regarding recovery of by-products. |
The Rupice deposit is a silver-gold-zinc-lead-barite deposit. Previous mining and beneficiation over a four-year period have shown that a conventional sulphide flotation method is a suitable recovery method. Metallurgical test work is ongoing to optimise the process flowsheet. |
|
|
Estimation of deleterious elements or other non-grade variables of economic significance (e.g. sulphur for acid mine drainage characterisation). |
As, Sb and Hg have been estimated in the model using their own semi-variogram models and OK interpolation method. |
|
|
In the case of block model interpolation, the block size in relation to the average sample spacing and the search employed. |
The average exploration drilling spacing was 20x20m. The selected parent cell size was 5x5m (quarter the exploration density). The search was based on the results of geostatistical analysis with average for all elements long ranges of 102x61x31m. |
|
|
Any assumptions behind modelling of selective mining units. |
No assumptions were made for selective mining unit, apart from the assumption that the deposit is likely to be mined by underground method and that 5x5m parent cell approximately reflects SMU for underground mining. |
|
|
Any assumptions about correlation between variables. |
Correlation between some variables was very strong (for example, between silver and lead), but no assumptions were made for the modelling purposes. Correlation between bulk density and main elements (BaSO4, Pb, Zn and Cu) was used to calculate bulk density for all model domains except for the combined high-grade domain. |
|
|
Description of how the geological interpretation was used to control the resource estimates. |
Geological interpretation of the mineralised zone, weakly mineralised halo and fault zones was based on the geological logging. When grades within modelled wireframes for the mineralized zone had mixed populations, high-grade domain was modelled using cut-offs justified by statistical analysis. High grade domains for each element were modelled individually, except for As, Sb and Hg, which did not demonstrate mixed grade populations within the modelled mineralized zone. |
|
|
Discussion of basis for using or not using grade cutting or capping. |
Classical statistical analysis was carried out for each element and each domain. It was found that histograms and probability plots did not demonstrate any apparent mixed populations within the limits of corresponding modelled domains. Top-cuts were identified and applied as shown in the table below:
|
|
|
The process of validation, the checking process used, the comparison of model data to drill hole data, and use of reconciliation data if available. |
Grade estimation was validated using visual inspection of interpolated block grades versus underlying data, and swath plots. Swath plots demonstrated reasonable correlation of modelled grades with the sample composites. The Competent Person is satisfied that estimation and modelling techniques are appropriate to support Mineral Resource estimation. |
|
|
Moisture |
Whether the tonnages are estimated on a dry basis or with natural moisture, and the method of determination of the moisture content. |
The tonnages were estimated on an in-situ dry bulk density basis which includes natural moisture. Moisture content was not estimated. |
|
Cut-off parameters |
The basis of the adopted cut-off grade(s) or quality parameters applied. |
The reporting cut-off grade of 50g/t silver equivalent was supported by estimation of marginal cut-off for underground mining using input economic parameters and criteria. The Competent Person is satisfied that cut-off parameters were appropriately considered, to support Mineral Resource estimation. |
|
Mining factors or assumptions |
Assumptions made regarding possible mining methods, minimum mining dimensions and internal (or, if applicable, external) mining dilution. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential mining methods, but the assumptions made regarding mining methods and parameters when estimating Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the mining assumptions made. |
A scoping and on-going preliminary economic assessment studies were performed to ensure that there are reasonable prospects for the eventual economic extraction of the mineralisation, which demonstrated that the deposit is likely to be developed by underground mining method(s). Input parameters were provided by the Company as being typical for the commodity, mining method and costs for a Balkan silver-lead-zinc mining operation. |
|
Metallurgical factors or assumptions |
The basis for assumptions or predictions regarding metallurgical amenability. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider potential metallurgical methods, but the assumptions regarding metallurgical treatment processes and parameters made when reporting Mineral Resources may not always be rigorous. Where this is the case, this should be reported with an explanation of the basis of the metallurgical assumptions made. |
A number of flotation tests have recently been carried out on both Rupice and Veova č a (nearby deposit) bulk samples. Preliminary results indicate there is potential to produce Zn, Pb/Cu and barite concentrates via flotation processes, with good recoveries of all constituents reported in this Mineral Resource estimate. The test work also indicates that a barite product that meets market specification requirements of purity, specific gravity, and fineness of particle size can be achieved, which meets the requirements of Clause 49 of the JORC Code. This test work remains ongoing. The Competent Person is satisfied that metallurgical factors and assumptions were appropriately considered, to support Mineral Resource estimation. |
|
Environmental factors or assumptions |
Assumptions made regarding possible waste and process residue disposal options. It is always necessary as part of the process of determining reasonable prospects for eventual economic extraction to consider the potential environmental impacts of the mining and processing operation. While at this stage the determination of potential environmental impacts, particularly for a greenfield project, may not always be well advanced, the status of early consideration of these potential environmental impacts should be reported. Where these aspects have not been considered this should be reported with an explanation of the environmental assumptions made. |
No detailed assumptions regarding possible environmental impacts to the site area were considered. The general locality has a number of active mining operations and no environmental impediments are anticipated. |
|
Bulk density |
Whether assumed or determined. If assumed, the basis for the assumptions. If determined, the method used, whether wet or dry, the frequency of the measurements, the nature, size and representativeness of the samples. |
Bulk densities were determined on drill core every 2m in ore and every 5m in waste. At total of 5,864 determinations were used to calculate regression formulas using barite, lead zinc and copper grades vs bulk density or to interpolate bulk density values into the combined high-grade domain. |
|
The bulk density for bulk material must have been measured by methods that adequately account for void spaces (vugs, porosity, etc), moisture and differences between rock and alteration zones within the deposit. |
Bulk density determinations adopted the weight in air / weight in water method using a suspended or hanging scale. First the core billet was accurately weighed dry ("in air"), the core billet was removed, and the wire cage fully submerged in water and its tare set to "zero" mass. The billet of core was then fully submerged and weighed ("weight in water"). The bulk density is calculated by the formula BD = Md / Md - Mw, where Md = weight in air and Mw = weight in water. |
|
|
Discuss assumptions for bulk density estimates used in the evaluation process of the different materials. |
No assumptions were made for Bulk Density. The Competent Person is satisfied that density was appropriately considered, to support Mineral Resource estimation. |
|
|
Classification |
The basis for the classification of the Mineral Resources into varying confidence categories. |
Resource classification was based on confidence in the QA/QC data analysis, geological interpretation, drill spacing, geostatistical measures, a visual evaluation of cross sections and drill density, and manual interpretation of resource categories. The interpreted boundaries between categories were wireframed and used to code the block models. Generally, the Indicated category was assigned to the areas with reasonable continuity of mineralised lodes based on 20x20m and 40x40m exploration drilling. All other blocks were classified as Inferred. No blocks were classified as Measured |
|
Whether appropriate account has been taken of all relevant factors (i.e. relative confidence in tonnage/grade estimations, reliability of input data, confidence in continuity of geology and metal values, quality, quantity and distribution of the data). |
The classification has taken into account all available geological and sampling information as well as the structural information, and the classification level is considered appropriate for the current stage of this project. |
|
|
Whether the result appropriately reflects the Competent Person's view of the deposit. |
The Mineral Resource estimate appropriately reflects the view of the Competent Person. The Competent Person is satisfied that classification of this Mineral Resource estimate appropriately reflects the data and interpreted geological controls on mineralisation. |
|
|
Audits or reviews |
The results of any audits or reviews of MREs. |
The current model has not been audited by an independent third party but has been subject to CSA Global's internal peer review processes. |
|
Discussion of relative accuracy/ confidence |
Where appropriate a statement of the relative accuracy and confidence level in the MRE using an approach or procedure deemed appropriate by the Competent Person. For example, the application of statistical or geostatistical procedures to quantify the relative accuracy of the resource within stated confidence limits, or, if such an approach is not deemed appropriate, a qualitative discussion of the factors that could affect the relative accuracy and confidence of the estimate. |
Industry standard modelling techniques were used, including but not limited to: · Classical statistical analysis, cut-offs selection. · Interpretation and wireframing. · Top-cutting and interval compositing. · Geostatistical analysis. · Block modelling and grade interpolation techniques. · Model classification, validation and reporting. The relative accuracy of the estimate is reflected in the classification of the deposit. The relative accuracy of the Mineral Resource estimate is reflected in the reporting of the Mineral Resource to an Indicated and Inferred classification as per the guidelines of the 2012 JORC Code. |
|
The statement should specify whether it relates to global or local estimates, and, if local, state the relevant tonnages, which should be relevant to technical and economic evaluation. Documentation should include assumptions made and the procedures used. |
The statement refers to global estimation of tonnes and grade and is suitable for use in a subsequent PFS and further exploration at the deposit. |
|
|
These statements of relative accuracy and confidence of the estimate should be compared with production data, where available. |
No production data is available. The Competent Person is satisfied that classification of this Mineral Resource estimate appropriately reflects the data and interpreted geological controls on mineralisation. |
|
RNS may use your IP address to confirm compliance with the terms and conditions, to analyse how you engage with the information contained in this communication, and to share such analysis on an anonymised basis with others as part of our commercial services. For further information about how RNS and the London Stock Exchange use the personal data you provide us, please see our Privacy Policy.
Latest directors dealings
- 1 day ago The Renewables Infrastructure Group Limited
- 1 day ago The Renewables Infrastructure Group Limited
- 1 day ago Smurfit Westrock (DI)
- 1 day ago Menhaden Resource Efficiency
- 1 day ago BP