Adriatic Metals PLC
("Adriatic Metals" or the "Company")
DRILLING SUCCESS AT KIZEVAK CONTINUES. ADRIATIC DISCOVERS MINERALISED GOLD ZONE AT SASTAVCI
To view the press release with all images, please visit https://bit.ly/37ujwgP
KIZEVAK HIGHLIGHTS
KZDD-020 intercepted a broad, high-grade zone of mineralisation down dip and outside the historically defined mineralisation:
· 53 metres at 4.2% zinc, 2.0% lead, 21g/t silver and 0.4/t gold from 100 metres, including
o 18 metres at 9.0% zinc, 4.1% lead, 43g/t silver and 0.6g/t gold
KZDD-018 intercepted two broad and high-grade mineralised zones, demonstrating excellent grade continuity between previously reported, widely spaced holes:
· 22 metres at 4.3% zinc, 1.7% lead, 28g/t silver and 0.4g/t gold from 48m, including
o 5 metres at 8.4% zinc, 2.9% lead, 59g/t silver and 0.7g/t gold, and
o 4 metres at 9.4% zinc, 3.6% lead, 57g/t silver and 0.6g/t gold
· 33.5 metres at 3.0% zinc, 1.5% lead, 23g/t silver and 0.2g/t gold from 106m, including
o 14.4 metres at 5.1% zinc, 2.7% lead, 45g/t silver and 0.2g/t gold
KZDD-017 was collared in mineralisation and intercepted two mineralised zones near surface in an area with no historic drilling:
· 18.5 metres at 2.4% zinc, 0.2% lead from 2m
· 34.5 metres at 2.2% zinc, 1.1% lead, 13g/t silver and 0.1g/t gold from 30.5m, including
o 7 metres at 4.9% zinc, 2.7% lead, 31g/t silver and 0.2g/t gold
KZDD-021 intercepted a narrow, but high-grade structure along strike to the southeast from KZDD-017:
· 5.9 metres at 4.5% zinc, 2.2% lead, 26g/t silver and 0.3g/t gold from 29.5 metres
SASTAVCI HIGHLIGHTS
SSDD-002 has confirmed the presence of near surface polymetallic mineralisation reported historically, as well as a newly discovered, broad gold anomalous structure at depth:
· 9 metres at 4.4% zinc, 1.2% lead, 18g/t silver and 0.4g/t gold from 6m, including
o 1.9 metres at 12.5% zinc, 4.8% lead, 72g/t silver and 1.7g/t gold
· 10 metres at 3.0% zinc, 1.0% lead, 17g/t silver and 0.5g/t gold from 28 metres, including
o 1.8 metres at 10.7% zinc, 3.8% lead, 64g/t silver and 0.4g/t gold
· 31 metres at 1.3 g/t gold from 279 metres, including
o 1.0 metre at 13.6 g/t gold
Adriatic Metals PLC (ASX:ADT, LSE:ADT1) is pleased to report assay results from seven diamond core holes (Tables 1 to 3) at Kizevak (Figures 1 to 3) and Adriatic's first drill hole at Sastavci (Figure 4). Kizevak continues to yield thick zones of polymetallic mineralisation, and confirmation drilling at Sastavci has been complemented by the discovery of a separate, large gold bearing structure.
Paul Cronin, Adriatic's Managing Director and CEO, commented "Our first true exploration holes at the Raska project in Serbia (Figure 5) have shown the potential scale of this high grade, shallow deposit. At Sastavci our first hole encountered strong near surface mineralisation, but the additional gold intercept has added further excitement to this historically significant deposit. With both Kizevak and Sastavci to be fully tested, our recent LIDAR and micro gravity survey's offer significant possibilities for targeted expansion. We are delighted that this acquisition is demonstrating such value for our shareholders at such an early stage in its development." .
KIZEVAK DRILLING RESULTS
The latest drill results have continued to define broad, sub-parallel, near-surface zones of mineralisation and holes KZDD-017 and KZDD-020 prove that significant mineralisation exists outside of the historically defined resource limits. The drilling at Kizevak by Adriatic to date is over a strike length of 300 metres to a depth of 170 metres, and has defined at least two subparallel, 15 to >50 metre thick zones of mineralisation which remain open in all directions. Drilling will continue to focus on the along strike and down dip extents of this zone and the whole 1200 metre strike length as defined by historic work.
Hole KZDD-020 was drilled to test 50 metres along strike from KZDD-001 (previously reported by Tethyan) and both have returned broad zones of moderate grade polymetallic mineralisation which include well defined, high grade domains.
KZDD-018 was drilled between two previously reported drill holes (KZDD-002 and KZDD-013), and has demonstrated excellent grade continuity between intercepts. Like hole KZDD-002, this hole also intercepted gold mineralisation of a higher tenor, suggesting that there is potential for more gold-rich parts to the system in this part of the deposit.
KZDD-017 intercepted two broad zones of moderate to high grade mineralisation from surface, and is open down dip in an area of no historic drilling. This hole was drilled in the same area as KZDD-004, KZDD-005 and KZDD-010, all of which intercepted mineralisation at or near surface over broad intervals, and open to depth.
Sastavci DRILLING RESULTS
SSDD-002 is the first hole to be drilled by Adriatic at the Sastavci past-producing open pit located 3.5 km north of Kizevak (drill hole SSDD-001 was abandoned due to drilling difficulties, and not sampled). The results from SSDD-002 confirm the presence of polymetallic mineralisation at surface and have also resulted in the discovery of a gold-bearing sheeted pyrite-arsenopyrite vein zone at depth. The near surface polymetallic mineralisation occurs over a broader interval than reported historically, and represents an excellent exploration target.
The gold bearing zone in SSDD-002 is significant as it is located approximately 500 metres south of a gold soil anomaly associated with vuggy silica and silica-flooded andesite representing a possible high-sulphidation type gold target, which has never been drill tested (Figure 4). Review of historical data indicate that silica alteration at surface is coincident with a large 1500 by 800 metre, northwest striking IP chargeability anomaly, and that the Sastavci historic open pit sits on the southern flank of the chargeability and gold soil anomaly.
Figure 1: Plan view map of the Kizevak project showing historic and Tethyan exploration drilling and adits, including highlighted results from recent drilling. The inactive Kizevak open pit is visible to the northwest, and mineralisation extending to the southeast and northwest is entirely open for expansion through further drilling.
Figure 2: Cross-section (A'-A) through the Kizevak deposit (KZDD-018).
Figure 3: Cross-section (B'-B) through the Kizevak deposit (KZDD-020).
Figure 4: Plan view map of the Sastavci project showing historic and Tethyan exploration drilling and adits, including highlighted results from recent drilling and the northern gold in soil anomaly.
Figure 5: Plan view map of the Raska District showing permits, Kizevak and Sastavci past-producing mines.
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 |
|
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Tavistock Communications Limited |
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Charles Vivian |
Tel: +44 (0) 7977 297903 |
Edward Lee |
Tel: +44 (0) 7736 220565 |
Gareth Tredway |
Tel: +44 (0) 7785 974264 |
|
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The Capital Network |
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Julia Maguire/Lelde Smits |
Tel: +61 2 8999 3699 |
COMPETENT PERSONS REPORT
The information in this report which relates to Exploration Results is based on 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.
ABOUT ADRIATIC METALS
Adriatic Metals Plc (ASX:ADT, LSE:ADT1) is a precious and base metals explorer and developer that owns the world-class Vares Silver Project in Bosnia & Herzegovina and holds licences across the Raska District in Serbia.
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 pre-feasibility study announced on 15 October 2020 indicate a post-tax NPV8% of US$1,040 million and IRR of 113%. Leveraging its first-mover advantage, Adriatic is rapidly advancing the project into the development phase and through to production with significant cornerstone investment of US$28 million from Queen's Road Capital Investment and EBRD.
There have been no material changes to the assumptions underpinning the forecast financial information derived from the production target in the 15 October 2020 announcement and these assumptions continue to apply. There have been no material changes to the assumptions and technical parameters on the updated Mineral Resource Estimate announced on 1 September 2020 and these assumptions continue to apply.
Adriatic Metals acquired TSX-listed Tethyan Resource Corp in 2020, to advance the former Kizevak and Sastavci polymetallic mines in the Raska District, southern Serbia.
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.
APPENDIX 1- ASSAY TABLES
Table 1- Significant intercepts for reported drill holes
Hole ID |
From (m) |
To (m) |
Interval (m) |
ZnEq (%) |
Zn (%) |
Pb (%) |
Ag (g/t) |
Au (g/t) |
Pb+Zn (%) |
KZDD-015 |
2.0 |
7.0 |
5.0 |
2.1 |
1.8 |
0.5 |
4.6 |
0.0 |
2.3 |
|
47.6 |
65.5 |
17.9 |
1.9 |
1.2 |
0.6 |
7.4 |
0.1 |
1.8 |
including |
50.5 |
52.5 |
2.0 |
5.6 |
3.6 |
2.4 |
26.5 |
0.2 |
6.0 |
|
79.0 |
82.0 |
3.0 |
9.2 |
6.4 |
2.9 |
43.8 |
0.3 |
9.4 |
KZDD-016 |
28.0 |
36.9 |
8.9 |
1.0 |
0.8 |
0.3 |
2.7 |
0.0 |
1.1 |
KZDD-017 |
2.0 |
20.5 |
18.5 |
2.3 |
2.4 |
0.2 |
1.8 |
0.0 |
2.6 |
|
30.5 |
65.0 |
34.5 |
3.2 |
2.2 |
1.1 |
13.0 |
0.1 |
3.3 |
including |
52.8 |
60.0 |
7.2 |
7.1 |
4.9 |
2.7 |
30.8 |
0.2 |
7.6 |
KZDD-018 |
48.0 |
70.0 |
22.0 |
6.2 |
4.3 |
1.7 |
27.9 |
0.4 |
6.0 |
including |
48.0 |
53.0 |
5.0 |
11.9 |
8.4 |
2.9 |
58.8 |
0.7 |
11.3 |
and |
66.0 |
70.0 |
4.0 |
13.0 |
9.4 |
3.6 |
56.5 |
0.6 |
13.1 |
|
105.8 |
139.3 |
33.5 |
4.4 |
3.0 |
1.5 |
23.1 |
0.2 |
4.5 |
including |
109.6 |
124.0 |
14.4 |
7.5 |
5.1 |
2.7 |
44.5 |
0.2 |
7.8 |
KZDD-020 |
100.8 |
154.0 |
53.2 |
6.1 |
4.2 |
2.0 |
21.1 |
0.4 |
6.1 |
including |
102.4 |
120.6 |
18.2 |
12.7 |
9.0 |
4.1 |
42.5 |
0.6 |
13.0 |
KZDD-021 |
29.5 |
35.4 |
5.9 |
6.5 |
4.5 |
2.2 |
26.2 |
0.3 |
6.8 |
SSDD-002 |
6.0 |
15.0 |
9.0 |
5.8 |
4.4 |
1.2 |
18.0 |
0.4 |
5.6 |
including |
13.1 |
15.0 |
1.9 |
18.9 |
12.5 |
4.8 |
72.3 |
1.7 |
17.2 |
|
28.0 |
38.0 |
10.0 |
4.7 |
3.0 |
1.0 |
17.1 |
0.5 |
4.0 |
including |
31.7 |
33.5 |
1.8 |
13.8 |
10.7 |
3.8 |
64.0 |
0.3 |
14.5 |
|
279* |
310.0 |
31.0 |
N/A |
0.0 |
0.1 |
3.8 |
1.3 |
0.1 |
Notes 1. Significant intervals are estimated using a 1% Pb+Zn cut off and 5 metres consecutive internal dilution. 2. ZnEq grades are based on the following metal prices: $1850/oz gold, $22/oz silver, $1900/t lead, $2350/t zinc. 3. The following metal recoveries were derived from preliminary testing: 75% silver, 85% lead and 85 % zinc. Gold recovery of 80% was estimated as there have been no gold recovery tests conducted to date. 4. A 100% payability was assumed for each metal and requires further investigation. 5. The zinc equivalent calculation is as follows: ZnEq = 100*(((Au grade g/t *Au recovery %*Au price $/g)+((Ag grade g/t *Ag recovery %)*Ag price $/g)+((Pb grade % *Pb recovery %)*Pb price ($/t)/100)+((Zn grade % *Zn recovery %)*Zn price ($/t)/100))/Zn price ($/t). *The gold only interval was estimated using a 0.2g/t gold cut off and 5 metres consecutive internal dilution.
|
Table 2 - Collar information for reported drill holes
Hole ID |
Easting (m) |
Northing (m) |
Elevation (m) |
Depth (m) |
Azimuth (°) |
Inclination (°) |
KZDD-015 |
475854 |
4792976 |
741 |
137.6 |
215 |
-54.1 |
KZDD-016 |
475868 |
4792932 |
752 |
101.6 |
203.4 |
-54.7 |
KZDD-017 |
475939 |
4792897 |
756 |
140.6 |
218.9 |
-54.1 |
KZDD-018 |
475804 |
4793006 |
734 |
155.6 |
236.3 |
-53.6 |
KZDD-019 |
475717 |
4793195 |
710 |
163.3 |
250.9 |
-54.6 |
KZDD-020 |
475787 |
4793091 |
718 |
237.2 |
240.9 |
-54.4 |
KZDD-021 |
476005 |
4792814 |
779 |
128.5 |
207.6 |
-56.1 |
SSDD-002 |
476687 |
4796557 |
1000 |
374.7 |
31.9 |
-55.5 |
Note: Coordinates are shown using the UTM WGS84 projection, Zone 34 Northern Hemisphere |
Table 3 - Assay data for reported drill holes
Hole ID |
From (m) |
To (m) |
Interval (m) |
Zn (%) |
Pb (%) |
Ag (g/t) |
Au (g/t) |
KZDD-015 |
0 |
0.3 |
0.3 |
Not Sampled |
|||
KZDD-015 |
0.3 |
1 |
0.7 |
0.28 |
0.602 |
14 |
0.204 |
KZDD-015 |
1 |
2 |
1 |
0.597 |
0.036 |
<1 |
0.006 |
KZDD-015 |
2 |
3 |
1 |
1.035 |
0.189 |
1 |
0.018 |
KZDD-015 |
3 |
4 |
1 |
0.717 |
0.355 |
3 |
0.03 |
KZDD-015 |
4 |
5 |
1 |
0.196 |
0.09 |
1 |
0.009 |
KZDD-015 |
5 |
6 |
1 |
1.12 |
0.481 |
4 |
0.054 |
KZDD-015 |
6 |
7 |
1 |
5.77 |
1.555 |
14 |
0.136 |
KZDD-015 |
7 |
8 |
1 |
0.378 |
0.211 |
2 |
0.057 |
KZDD-015 |
8 |
9 |
1 |
0.218 |
0.151 |
1 |
0.007 |
KZDD-015 |
9 |
10 |
1 |
0.219 |
0.092 |
<1 |
0.01 |
KZDD-015 |
10 |
11 |
1 |
0.468 |
0.27 |
2 |
0.042 |
KZDD-015 |
11 |
11.6 |
0.6 |
0.739 |
0.354 |
3 |
0.063 |
KZDD-015 |
11.6 |
13 |
1.4 |
0.031 |
0.015 |
<1 |
0.005 |
KZDD-015 |
13 |
15 |
2 |
0.078 |
0.032 |
<1 |
<0.005 |
KZDD-015 |
15 |
17 |
2 |
0.157 |
0.076 |
<1 |
0.008 |
KZDD-015 |
17 |
18.3 |
1.3 |
0.044 |
0.015 |
<1 |
0.007 |
KZDD-015 |
18.3 |
19 |
0.7 |
0.272 |
0.095 |
<1 |
0.005 |
KZDD-015 |
19 |
20.6 |
1.6 |
0.015 |
0.005 |
<1 |
0.011 |
KZDD-015 |
20.6 |
22 |
1.4 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
22 |
24 |
2 |
0.009 |
<0.005 |
<1 |
0.008 |
KZDD-015 |
24 |
25.3 |
1.3 |
0.019 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
25.3 |
26.6 |
1.3 |
0.216 |
0.082 |
1 |
0.022 |
KZDD-015 |
26.6 |
29 |
2.4 |
0.297 |
0.126 |
<1 |
0.032 |
KZDD-015 |
29 |
31 |
2 |
0.269 |
0.135 |
1 |
0.081 |
KZDD-015 |
31 |
32 |
1 |
0.459 |
0.195 |
3 |
0.099 |
KZDD-015 |
32 |
33 |
1 |
0.067 |
0.063 |
<1 |
0.012 |
KZDD-015 |
33 |
34 |
1 |
0.062 |
0.028 |
<1 |
0.01 |
KZDD-015 |
34 |
35 |
1 |
0.017 |
0.006 |
<1 |
0.006 |
KZDD-015 |
35 |
35.6 |
0.6 |
0.018 |
0.005 |
<1 |
<0.005 |
KZDD-015 |
35.6 |
36.9 |
1.3 |
0.021 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
36.9 |
38 |
1.1 |
0.012 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
38 |
40 |
2 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
40 |
42 |
2 |
0.015 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
42 |
44 |
2 |
0.016 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
44 |
46 |
2 |
0.014 |
0.011 |
<1 |
0.006 |
KZDD-015 |
46 |
47.6 |
1.6 |
0.12 |
0.075 |
<1 |
0.015 |
KZDD-015 |
47.6 |
48.5 |
0.9 |
1.255 |
0.571 |
7 |
0.158 |
KZDD-015 |
48.5 |
49.5 |
1 |
0.585 |
0.303 |
2 |
0.094 |
KZDD-015 |
49.5 |
50.5 |
1 |
0.52 |
0.261 |
2 |
0.069 |
KZDD-015 |
50.5 |
51.5 |
1 |
3.6 |
3.15 |
32 |
0.192 |
KZDD-015 |
51.5 |
52.5 |
1 |
3.58 |
1.6 |
21 |
0.132 |
KZDD-015 |
52.5 |
53.5 |
1 |
0.953 |
0.493 |
6 |
0.088 |
KZDD-015 |
53.5 |
54.5 |
1 |
0.564 |
0.404 |
4 |
0.053 |
KZDD-015 |
54.5 |
55.5 |
1 |
1.13 |
0.511 |
7 |
0.156 |
KZDD-015 |
55.5 |
56.5 |
1 |
0.486 |
0.234 |
3 |
0.112 |
KZDD-015 |
56.5 |
57.5 |
1 |
0.378 |
0.188 |
2 |
0.072 |
KZDD-015 |
57.5 |
58 |
0.5 |
0.372 |
0.13 |
1 |
0.021 |
KZDD-015 |
58 |
59 |
1 |
0.093 |
0.056 |
<1 |
0.033 |
KZDD-015 |
59 |
60 |
1 |
0.321 |
0.149 |
2 |
0.128 |
KZDD-015 |
60 |
61 |
1 |
0.952 |
0.557 |
5 |
0.087 |
KZDD-015 |
61 |
62 |
1 |
1.36 |
0.657 |
8 |
0.118 |
KZDD-015 |
62 |
63 |
1 |
1.93 |
0.854 |
13 |
0.228 |
KZDD-015 |
63 |
63.5 |
0.5 |
3.49 |
1.75 |
23 |
0.685 |
KZDD-015 |
63.5 |
64.5 |
1 |
0.237 |
0.125 |
<1 |
0.088 |
KZDD-015 |
64.5 |
65.5 |
1 |
1.36 |
0.611 |
7 |
0.171 |
KZDD-015 |
65.5 |
67 |
1.5 |
0.029 |
0.013 |
<1 |
0.027 |
KZDD-015 |
67 |
68 |
1 |
0.03 |
0.015 |
<1 |
0.007 |
KZDD-015 |
68 |
69 |
1 |
0.21 |
0.097 |
1 |
0.022 |
KZDD-015 |
69 |
70 |
1 |
0.084 |
0.039 |
1 |
0.012 |
KZDD-015 |
70 |
71 |
1 |
0.351 |
0.166 |
<1 |
0.035 |
KZDD-015 |
71 |
72 |
1 |
0.022 |
0.011 |
<1 |
0.007 |
KZDD-015 |
72 |
73 |
1 |
0.107 |
0.069 |
1 |
0.042 |
KZDD-015 |
73 |
74 |
1 |
0.2 |
0.086 |
1 |
0.027 |
KZDD-015 |
74 |
75 |
1 |
0.053 |
0.029 |
<1 |
0.014 |
KZDD-015 |
75 |
76 |
1 |
0.478 |
0.246 |
5 |
0.08 |
KZDD-015 |
76 |
77 |
1 |
0.112 |
0.041 |
<1 |
0.017 |
KZDD-015 |
77 |
78 |
1 |
0.102 |
0.029 |
1 |
0.053 |
KZDD-015 |
78 |
79 |
1 |
0.224 |
0.224 |
3 |
0.148 |
KZDD-015 |
79 |
80 |
1 |
4.59 |
1.99 |
33 |
0.271 |
KZDD-015 |
80 |
80.6 |
0.6 |
8.99 |
3.89 |
58 |
0.321 |
KZDD-015 |
80.6 |
81.3 |
0.7 |
12 |
5.7 |
82 |
0.509 |
KZDD-015 |
81.3 |
82 |
0.7 |
1.355 |
0.633 |
9 |
0.272 |
KZDD-015 |
82 |
84 |
2 |
0.207 |
0.072 |
<1 |
0.027 |
KZDD-015 |
84 |
86 |
2 |
0.012 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
86 |
87.5 |
1.5 |
0.015 |
0.012 |
<1 |
0.011 |
KZDD-015 |
87.5 |
88.5 |
1 |
0.117 |
0.085 |
<1 |
0.027 |
KZDD-015 |
88.5 |
89.3 |
0.8 |
0.019 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
89.3 |
91 |
1.7 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
91 |
93 |
2 |
0.012 |
<0.005 |
1 |
<0.005 |
KZDD-015 |
93 |
95 |
2 |
0.008 |
<0.005 |
<1 |
0.01 |
KZDD-015 |
95 |
96 |
1 |
0.006 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
96 |
97 |
1 |
0.01 |
<0.005 |
<1 |
0.007 |
KZDD-015 |
97 |
98 |
1 |
0.016 |
<0.005 |
<1 |
0.032 |
KZDD-015 |
98 |
98.6 |
0.6 |
0.016 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
98.6 |
100 |
1.4 |
0.017 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
100 |
102 |
2 |
0.009 |
<0.005 |
<1 |
0.007 |
KZDD-015 |
102 |
104 |
2 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
104 |
105 |
1 |
0.011 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
105 |
106 |
1 |
0.018 |
<0.005 |
<1 |
0.005 |
KZDD-015 |
106 |
108 |
2 |
0.014 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
108 |
109 |
1 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
109 |
110 |
1 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
110 |
112 |
2 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
112 |
114 |
2 |
0.015 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
114 |
115 |
1 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
115 |
116 |
1 |
0.012 |
<0.005 |
<1 |
0.006 |
KZDD-015 |
116 |
118 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
118 |
120 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
120 |
121.8 |
1.8 |
0.012 |
<0.005 |
<1 |
<0.005 |
KZDD-015 |
121.8 |
122.6 |
0.8 |
2.1 |
1.05 |
20 |
0.185 |
KZDD-015 |
122.6 |
123.5 |
0.9 |
0.024 |
0.015 |
<1 |
0.012 |
KZDD-015 |
123.5 |
124.5 |
1 |
0.012 |
<0.005 |
<1 |
0.007 |
KZDD-015 |
124.5 |
125.5 |
1 |
0.011 |
<0.005 |
<1 |
0.009 |
KZDD-015 |
125.5 |
126.5 |
1 |
0.013 |
<0.005 |
<1 |
0.005 |
KZDD-015 |
126.5 |
127.5 |
1 |
0.119 |
0.075 |
2 |
0.036 |
KZDD-015 |
127.5 |
129.5 |
2 |
0.063 |
0.039 |
<1 |
0.015 |
KZDD-015 |
129.5 |
131.5 |
2 |
0.008 |
<0.005 |
<1 |
0.008 |
KZDD-015 |
131.5 |
133.5 |
2 |
0.007 |
<0.005 |
<1 |
0.019 |
KZDD-015 |
133.5 |
135.5 |
2 |
0.007 |
<0.005 |
<1 |
0.006 |
KZDD-015 |
135.5 |
137.5 |
2 |
0.008 |
<0.005 |
<1 |
0.007 |
KZDD-016 |
0 |
1 |
1 |
0.571 |
0.301 |
6 |
0.045 |
KZDD-016 |
1 |
2 |
1 |
0.426 |
0.161 |
1 |
0.026 |
KZDD-016 |
2 |
3 |
1 |
0.255 |
0.009 |
<1 |
0.014 |
KZDD-016 |
3 |
5 |
2 |
0.041 |
0.008 |
<1 |
0.013 |
KZDD-016 |
5 |
7 |
2 |
0.06 |
0.047 |
<1 |
0.008 |
KZDD-016 |
7 |
8 |
1 |
0.974 |
0.523 |
3 |
0.117 |
KZDD-016 |
8 |
8.5 |
0.5 |
8.32 |
4.58 |
43 |
0.279 |
KZDD-016 |
8.5 |
9 |
0.5 |
1.205 |
0.747 |
7 |
0.198 |
KZDD-016 |
9 |
10 |
1 |
0.149 |
0.089 |
3 |
0.019 |
KZDD-016 |
10 |
10.7 |
0.7 |
0.098 |
0.043 |
<1 |
0.012 |
KZDD-016 |
10.7 |
11.2 |
0.5 |
0.137 |
0.014 |
1 |
0.005 |
KZDD-016 |
11.2 |
12 |
0.8 |
0.033 |
0.018 |
<1 |
<0.005 |
KZDD-016 |
12 |
13 |
1 |
0.082 |
0.055 |
1 |
0.01 |
KZDD-016 |
13 |
14 |
1 |
0.065 |
0.054 |
1 |
0.009 |
KZDD-016 |
14 |
14.6 |
0.6 |
0.036 |
0.03 |
<1 |
0.008 |
KZDD-016 |
14.6 |
16.6 |
2 |
0.038 |
0.02 |
1 |
0.006 |
KZDD-016 |
16.6 |
17.5 |
0.9 |
0.049 |
0.041 |
<1 |
0.005 |
KZDD-016 |
17.5 |
18 |
0.5 |
0.407 |
0.25 |
2 |
0.037 |
KZDD-016 |
18 |
18.6 |
0.6 |
1.615 |
0.837 |
6 |
0.121 |
KZDD-016 |
18.6 |
19.2 |
0.6 |
0.279 |
0.196 |
2 |
0.088 |
KZDD-016 |
19.2 |
20 |
0.8 |
0.926 |
0.482 |
5 |
0.087 |
KZDD-016 |
20 |
21 |
1 |
0.043 |
0.05 |
1 |
0.005 |
KZDD-016 |
21 |
22 |
1 |
0.017 |
0.007 |
<1 |
0.005 |
KZDD-016 |
22 |
24 |
2 |
0.017 |
<0.005 |
<1 |
0.006 |
KZDD-016 |
24 |
26 |
2 |
0.053 |
0.02 |
<1 |
0.016 |
KZDD-016 |
26 |
28 |
2 |
0.017 |
<0.005 |
1 |
<0.005 |
KZDD-016 |
28 |
29 |
1 |
0.95 |
0.227 |
1 |
0.026 |
KZDD-016 |
29 |
30 |
1 |
1.335 |
0.59 |
6 |
0.05 |
KZDD-016 |
30 |
31 |
1 |
0.224 |
0.145 |
2 |
0.01 |
KZDD-016 |
31 |
32 |
1 |
0.027 |
<0.005 |
<1 |
0.006 |
KZDD-016 |
32 |
32.8 |
0.8 |
0.025 |
0.006 |
<1 |
<0.005 |
KZDD-016 |
32.8 |
33.3 |
0.5 |
1.19 |
0.616 |
5 |
0.079 |
KZDD-016 |
33.3 |
33.8 |
0.5 |
2.88 |
0.821 |
7 |
0.139 |
KZDD-016 |
33.8 |
34.5 |
0.7 |
0.672 |
0.294 |
2 |
0.02 |
KZDD-016 |
34.5 |
35.2 |
0.7 |
0.519 |
0.327 |
3 |
0.011 |
KZDD-016 |
35.2 |
35.9 |
0.7 |
0.74 |
0.467 |
4 |
0.021 |
KZDD-016 |
35.9 |
36.9 |
1 |
0.785 |
0.382 |
2 |
0.035 |
KZDD-016 |
36.9 |
38 |
1.1 |
0.505 |
0.271 |
3 |
0.03 |
KZDD-016 |
38 |
39 |
1 |
0.048 |
0.026 |
<1 |
0.005 |
KZDD-016 |
39 |
40 |
1 |
0.289 |
0.173 |
1 |
0.006 |
KZDD-016 |
40 |
41 |
1 |
0.081 |
0.036 |
2 |
0.013 |
KZDD-016 |
41 |
41.6 |
0.6 |
0.491 |
0.223 |
2 |
0.042 |
KZDD-016 |
41.6 |
42.1 |
0.5 |
0.873 |
0.413 |
4 |
0.058 |
KZDD-016 |
42.1 |
43 |
0.9 |
0.295 |
0.155 |
3 |
0.078 |
KZDD-016 |
43 |
43.5 |
0.5 |
0.074 |
0.039 |
<1 |
0.081 |
KZDD-016 |
43.5 |
44 |
0.5 |
0.023 |
0.021 |
<1 |
0.051 |
KZDD-016 |
44 |
45 |
1 |
0.482 |
0.189 |
2 |
0.041 |
KZDD-016 |
45 |
46 |
1 |
1.575 |
0.693 |
8 |
0.083 |
KZDD-016 |
46 |
47 |
1 |
0.266 |
0.139 |
2 |
0.031 |
KZDD-016 |
47 |
48 |
1 |
0.558 |
0.287 |
4 |
0.075 |
KZDD-016 |
48 |
49 |
1 |
0.014 |
<0.005 |
<1 |
0.011 |
KZDD-016 |
49 |
51 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
51 |
53 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
53 |
55 |
2 |
0.007 |
<0.005 |
<1 |
0.008 |
KZDD-016 |
55 |
57 |
2 |
0.006 |
<0.005 |
<1 |
0.008 |
KZDD-016 |
57 |
59 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
59 |
67 |
8 |
Not Sampled |
|||
KZDD-016 |
67 |
69 |
2 |
0.007 |
<0.005 |
<1 |
0.009 |
KZDD-016 |
69 |
71 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
71 |
73 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
73 |
75 |
2 |
0.01 |
<0.005 |
<1 |
0.008 |
KZDD-016 |
75 |
76 |
1 |
0.013 |
<0.005 |
<1 |
0.005 |
KZDD-016 |
76 |
77 |
1 |
0.016 |
0.015 |
1 |
0.014 |
KZDD-016 |
77 |
77.6 |
0.6 |
2.93 |
1.1 |
8 |
0.039 |
KZDD-016 |
77.6 |
78.1 |
0.5 |
0.028 |
0.009 |
<1 |
0.007 |
KZDD-016 |
78.1 |
78.9 |
0.8 |
1.975 |
0.876 |
9 |
0.04 |
KZDD-016 |
78.9 |
80 |
1.1 |
0.028 |
0.027 |
<1 |
0.016 |
KZDD-016 |
80 |
81 |
1 |
0.02 |
0.005 |
<1 |
0.008 |
KZDD-016 |
81 |
83 |
2 |
0.014 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
83 |
85 |
2 |
0.011 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
85 |
87 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
87 |
89 |
2 |
0.022 |
<0.005 |
<1 |
<0.005 |
KZDD-016 |
89 |
91 |
2 |
0.017 |
<0.005 |
<1 |
0.008 |
KZDD-016 |
91 |
101.6 |
10.6 |
Not Sampled |
|||
KZDD-017 |
0 |
1 |
1 |
0.359 |
0.275 |
2 |
0.022 |
KZDD-017 |
1 |
2 |
1 |
0.566 |
0.057 |
1 |
0.011 |
KZDD-017 |
2 |
3 |
1 |
1.86 |
0.018 |
<1 |
0.007 |
KZDD-017 |
3 |
4 |
1 |
1.225 |
0.133 |
1 |
0.013 |
KZDD-017 |
4 |
5 |
1 |
1.305 |
0.009 |
1 |
0.005 |
KZDD-017 |
5 |
6 |
1 |
2.45 |
0.196 |
2 |
0.015 |
KZDD-017 |
6 |
7 |
1 |
2.37 |
0.072 |
1 |
0.011 |
KZDD-017 |
7 |
8 |
1 |
3.34 |
0.011 |
<1 |
0.006 |
KZDD-017 |
8 |
9 |
1 |
3.9 |
0.005 |
<1 |
0.007 |
KZDD-017 |
9 |
10 |
1 |
3.61 |
0.006 |
<1 |
0.014 |
KZDD-017 |
10 |
11 |
1 |
3.67 |
0.011 |
<1 |
0.005 |
KZDD-017 |
11 |
11.6 |
0.6 |
2.52 |
0.032 |
<1 |
0.014 |
KZDD-017 |
11.6 |
12.5 |
0.9 |
2.41 |
0.231 |
2 |
0.074 |
KZDD-017 |
12.5 |
13.5 |
1 |
2.59 |
0.226 |
2 |
0.094 |
KZDD-017 |
13.5 |
14.5 |
1 |
2.15 |
0.309 |
2 |
0.056 |
KZDD-017 |
14.5 |
15.5 |
1 |
2.48 |
0.137 |
<1 |
0.02 |
KZDD-017 |
15.5 |
16 |
0.5 |
3.22 |
0.031 |
<1 |
0.011 |
KZDD-017 |
16 |
16.7 |
0.7 |
1.625 |
0.364 |
3 |
0.064 |
KZDD-017 |
16.7 |
17.6 |
0.9 |
4.32 |
1.48 |
12 |
0.11 |
KZDD-017 |
17.6 |
18.5 |
0.9 |
2.32 |
0.391 |
3 |
0.116 |
KZDD-017 |
18.5 |
19.5 |
1 |
0.801 |
0.325 |
<1 |
0.037 |
KZDD-017 |
19.5 |
20.5 |
1 |
0.739 |
0.27 |
2 |
0.061 |
KZDD-017 |
20.5 |
21.5 |
1 |
0.528 |
0.17 |
<1 |
0.034 |
KZDD-017 |
21.5 |
22.5 |
1 |
0.376 |
0.203 |
1 |
0.022 |
KZDD-017 |
22.5 |
24.5 |
2 |
0.039 |
<0.005 |
<1 |
<0.005 |
KZDD-017 |
24.5 |
26.5 |
2 |
0.017 |
<0.005 |
<1 |
<0.005 |
KZDD-017 |
26.5 |
28.5 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
KZDD-017 |
28.5 |
29.6 |
1.1 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-017 |
29.6 |
30.5 |
0.9 |
0.447 |
0.242 |
1 |
0.009 |
KZDD-017 |
30.5 |
31.3 |
0.8 |
1.71 |
0.18 |
1 |
0.041 |
KZDD-017 |
31.3 |
32 |
0.7 |
0.05 |
0.018 |
<1 |
0.013 |
KZDD-017 |
32 |
33 |
1 |
0.222 |
0.094 |
<1 |
0.013 |
KZDD-017 |
33 |
34 |
1 |
0.925 |
0.362 |
3 |
0.047 |
KZDD-017 |
34 |
35 |
1 |
0.561 |
0.422 |
3 |
0.037 |
KZDD-017 |
35 |
36 |
1 |
0.94 |
0.465 |
5 |
0.067 |
KZDD-017 |
36 |
37 |
1 |
0.51 |
0.301 |
4 |
0.084 |
KZDD-017 |
37 |
38 |
1 |
0.756 |
0.323 |
9 |
0.167 |
KZDD-017 |
38 |
38.9 |
0.9 |
0.63 |
0.221 |
4 |
0.072 |
KZDD-017 |
38.9 |
39.5 |
0.6 |
0.541 |
0.218 |
5 |
0.048 |
KZDD-017 |
39.5 |
40.3 |
0.8 |
5.47 |
1.94 |
23 |
0.157 |
KZDD-017 |
40.3 |
41 |
0.7 |
1.54 |
0.754 |
12 |
0.078 |
KZDD-017 |
41 |
42 |
1 |
2 |
0.816 |
11 |
0.119 |
KZDD-017 |
42 |
43 |
1 |
2.09 |
0.854 |
11 |
0.142 |
KZDD-017 |
43 |
43.6 |
0.6 |
2.8 |
1.845 |
23 |
0.245 |
KZDD-017 |
43.6 |
44.6 |
1 |
1.79 |
0.577 |
7 |
0.096 |
KZDD-017 |
44.6 |
45.5 |
0.9 |
1.24 |
0.968 |
11 |
0.08 |
KZDD-017 |
45.5 |
46.2 |
0.7 |
2.78 |
0.996 |
14 |
0.069 |
KZDD-017 |
46.2 |
47.6 |
1.4 |
0.095 |
0.038 |
<1 |
0.007 |
KZDD-017 |
47.6 |
48.4 |
0.8 |
0.11 |
0.067 |
<1 |
0.015 |
KZDD-017 |
48.4 |
49.4 |
1 |
1.965 |
1.09 |
12 |
0.195 |
KZDD-017 |
49.4 |
50.2 |
0.8 |
0.8 |
0.403 |
4 |
0.069 |
KZDD-017 |
50.2 |
51 |
0.8 |
1.44 |
0.851 |
9 |
0.11 |
KZDD-017 |
51 |
52 |
1 |
3.12 |
1.47 |
17 |
0.128 |
KZDD-017 |
52 |
52.8 |
0.8 |
0.804 |
0.488 |
6 |
0.031 |
KZDD-017 |
52.8 |
53.6 |
0.8 |
11.7 |
8.28 |
109 |
0.459 |
KZDD-017 |
53.6 |
54.3 |
0.7 |
7.93 |
7.09 |
81 |
0.377 |
KZDD-017 |
54.3 |
55 |
0.7 |
2.55 |
1.375 |
14 |
0.206 |
KZDD-017 |
55 |
56 |
1 |
2.34 |
1.14 |
13 |
0.187 |
KZDD-017 |
56 |
57 |
1 |
1.52 |
0.69 |
8 |
0.102 |
KZDD-017 |
57 |
58 |
1 |
4.97 |
1.145 |
11 |
0.093 |
KZDD-017 |
58 |
59 |
1 |
4.96 |
1.995 |
17 |
0.078 |
KZDD-017 |
59 |
60 |
1 |
4.44 |
2.14 |
19 |
0.116 |
KZDD-017 |
60 |
61 |
1 |
0.446 |
0.24 |
2 |
0.078 |
KZDD-017 |
61 |
62 |
1 |
0.474 |
0.232 |
4 |
0.12 |
KZDD-017 |
62 |
63 |
1 |
2.97 |
1.305 |
18 |
0.369 |
KZDD-017 |
63 |
64 |
1 |
2.42 |
1.065 |
11 |
0.135 |
KZDD-017 |
64 |
65 |
1 |
4.72 |
2.04 |
26 |
0.353 |
KZDD-017 |
65 |
67 |
2 |
0.024 |
0.008 |
<1 |
0.008 |
KZDD-017 |
67 |
69 |
2 |
0.017 |
<0.005 |
<1 |
0.007 |
KZDD-017 |
69 |
71 |
2 |
0.01 |
<0.005 |
<1 |
0.014 |
KZDD-017 |
71 |
73 |
2 |
0.01 |
0.005 |
1 |
0.02 |
KZDD-017 |
73 |
75 |
2 |
0.01 |
<0.005 |
<1 |
0.005 |
KZDD-017 |
75 |
77 |
2 |
0.012 |
0.005 |
<1 |
0.014 |
KZDD-017 |
77 |
79 |
2 |
0.011 |
<0.005 |
<1 |
0.011 |
KZDD-017 |
79 |
80.6 |
1.6 |
0.01 |
<0.005 |
<1 |
0.023 |
KZDD-017 |
80.6 |
81.3 |
0.7 |
0.038 |
0.012 |
<1 |
0.006 |
KZDD-017 |
81.3 |
82 |
0.7 |
0.036 |
0.011 |
1 |
0.008 |
KZDD-017 |
82 |
84 |
2 |
0.013 |
<0.005 |
<1 |
0.012 |
KZDD-017 |
84 |
86 |
2 |
0.015 |
<0.005 |
<1 |
0.017 |
KZDD-017 |
86 |
88 |
2 |
0.01 |
<0.005 |
<1 |
0.012 |
KZDD-017 |
88 |
90 |
2 |
0.007 |
<0.005 |
<1 |
0.005 |
KZDD-017 |
90 |
92 |
2 |
0.008 |
<0.005 |
<1 |
0.011 |
KZDD-018 |
0 |
33.5 |
33.5 |
Not Sampled |
|||
KZDD-018 |
33.5 |
35.5 |
2 |
0.006 |
<0.005 |
<1 |
0.019 |
KZDD-018 |
35.5 |
37.5 |
2 |
0.008 |
<0.005 |
<1 |
0.007 |
KZDD-018 |
37.5 |
39.5 |
2 |
0.006 |
<0.005 |
<1 |
0.013 |
KZDD-018 |
39.5 |
41.5 |
2 |
0.006 |
<0.005 |
<1 |
0.007 |
KZDD-018 |
41.5 |
43.5 |
2 |
0.008 |
<0.005 |
<1 |
0.01 |
KZDD-018 |
43.5 |
44.2 |
0.7 |
0.232 |
0.119 |
1 |
0.082 |
KZDD-018 |
44.2 |
45 |
0.8 |
0.012 |
<0.005 |
<1 |
0.007 |
KZDD-018 |
45 |
46 |
1 |
0.015 |
<0.005 |
<1 |
0.01 |
KZDD-018 |
46 |
47 |
1 |
0.017 |
<0.005 |
<1 |
0.01 |
KZDD-018 |
47 |
48 |
1 |
0.361 |
0.265 |
4 |
0.121 |
KZDD-018 |
48 |
49.2 |
1.2 |
18.35 |
6.14 |
143 |
1.32 |
KZDD-018 |
49.2 |
50 |
0.8 |
4.03 |
2.02 |
37 |
0.815 |
KZDD-018 |
50 |
50.7 |
0.7 |
13.7 |
4.21 |
84 |
0.795 |
KZDD-018 |
50.7 |
52 |
1.3 |
1.935 |
0.823 |
10 |
0.215 |
KZDD-018 |
52 |
53 |
1 |
4.48 |
1.74 |
21 |
0.397 |
KZDD-018 |
53 |
54 |
1 |
2.89 |
1.14 |
13 |
0.366 |
KZDD-018 |
54 |
55 |
1 |
0.585 |
0.261 |
4 |
0.164 |
KZDD-018 |
55 |
56 |
1 |
2.49 |
1.235 |
17 |
0.299 |
KZDD-018 |
56 |
57 |
1 |
0.716 |
0.308 |
4 |
0.159 |
KZDD-018 |
57 |
58 |
1 |
2.14 |
1.28 |
15 |
0.296 |
KZDD-018 |
58 |
59 |
1 |
1.49 |
0.744 |
12 |
0.199 |
KZDD-018 |
59 |
60 |
1 |
2.36 |
0.99 |
12 |
0.196 |
KZDD-018 |
60 |
61 |
1 |
0.211 |
0.196 |
3 |
0.071 |
KZDD-018 |
61 |
62 |
1 |
0.797 |
0.296 |
3 |
0.125 |
KZDD-018 |
62 |
63 |
1 |
0.045 |
0.021 |
<1 |
0.025 |
KZDD-018 |
63 |
64 |
1 |
0.088 |
0.029 |
<1 |
0.081 |
KZDD-018 |
64 |
65 |
1 |
0.594 |
0.271 |
5 |
0.253 |
KZDD-018 |
65 |
66 |
1 |
0.59 |
0.417 |
5 |
0.232 |
KZDD-018 |
66 |
67 |
1 |
5.34 |
2.67 |
39 |
0.772 |
KZDD-018 |
67 |
68 |
1 |
12.65 |
2.71 |
39 |
0.579 |
KZDD-018 |
68 |
69 |
1 |
16.05 |
7.13 |
122 |
0.542 |
KZDD-018 |
69 |
70 |
1 |
3.72 |
2.03 |
26 |
0.427 |
KZDD-018 |
70 |
71 |
1 |
0.317 |
0.195 |
2 |
0.19 |
KZDD-018 |
71 |
72 |
1 |
0.453 |
0.166 |
2 |
0.199 |
KZDD-018 |
72 |
73 |
1 |
0.198 |
0.142 |
1 |
0.039 |
KZDD-018 |
73 |
75 |
2 |
0.03 |
0.022 |
<1 |
0.013 |
KZDD-018 |
75 |
77 |
2 |
0.011 |
<0.005 |
<1 |
0.008 |
KZDD-018 |
77 |
79 |
2 |
0.014 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
79 |
81 |
2 |
0.008 |
<0.005 |
<1 |
0.009 |
KZDD-018 |
81 |
83 |
2 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
83 |
95.8 |
12.8 |
Not Sampled |
|||
KZDD-018 |
95.8 |
97.8 |
2 |
0.008 |
0.008 |
<1 |
<0.005 |
KZDD-018 |
97.8 |
99.8 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
99.8 |
101.8 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
101.8 |
103.8 |
2 |
0.016 |
0.007 |
<1 |
<0.005 |
KZDD-018 |
103.8 |
105.8 |
2 |
0.013 |
<0.005 |
<1 |
0.006 |
KZDD-018 |
105.8 |
106.5 |
0.7 |
1.715 |
0.676 |
9 |
0.163 |
KZDD-018 |
106.5 |
107.1 |
0.6 |
1.96 |
0.916 |
14 |
0.215 |
KZDD-018 |
107.1 |
108 |
0.9 |
3.31 |
1.405 |
17 |
0.365 |
KZDD-018 |
108 |
109 |
1 |
0.619 |
0.332 |
4 |
0.057 |
KZDD-018 |
109 |
109.6 |
0.6 |
0.688 |
0.347 |
4 |
0.145 |
KZDD-018 |
109.6 |
110.1 |
0.5 |
8.13 |
3.21 |
37 |
0.391 |
KZDD-018 |
110.1 |
111 |
0.9 |
2.35 |
0.753 |
8 |
0.126 |
KZDD-018 |
111 |
112 |
1 |
3.91 |
1.885 |
21 |
0.126 |
KZDD-018 |
112 |
113 |
1 |
2.4 |
1.925 |
24 |
0.068 |
KZDD-018 |
113 |
114 |
1 |
2.87 |
1.89 |
38 |
0.067 |
KZDD-018 |
114 |
115 |
1 |
3.6 |
1.405 |
27 |
0.14 |
KZDD-018 |
115 |
116 |
1 |
1.21 |
0.34 |
4 |
0.084 |
KZDD-018 |
116 |
117 |
1 |
0.251 |
0.14 |
2 |
0.082 |
KZDD-018 |
117 |
117.9 |
0.9 |
0.391 |
0.216 |
1 |
0.181 |
KZDD-018 |
117.9 |
118.4 |
0.5 |
0.922 |
0.449 |
4 |
0.049 |
KZDD-018 |
118.4 |
119.05 |
0.65 |
17.95 |
5.55 |
81 |
0.306 |
KZDD-018 |
119.05 |
120 |
0.95 |
6.28 |
2.4 |
37 |
0.275 |
KZDD-018 |
120 |
121 |
1 |
9.49 |
11.3 |
262 |
0.25 |
KZDD-018 |
121 |
122 |
1 |
9.71 |
4.38 |
67 |
0.217 |
KZDD-018 |
122 |
123 |
1 |
6.66 |
2.95 |
34 |
0.149 |
KZDD-018 |
123 |
124 |
1 |
8.61 |
4.08 |
45 |
0.195 |
KZDD-018 |
124 |
125 |
1 |
2.02 |
0.94 |
10 |
0.103 |
KZDD-018 |
125 |
126 |
1 |
0.695 |
0.379 |
4 |
0.092 |
KZDD-018 |
126 |
127 |
1 |
1.145 |
0.493 |
5 |
0.067 |
KZDD-018 |
127 |
128 |
1 |
0.789 |
0.52 |
7 |
0.094 |
KZDD-018 |
128 |
129 |
1 |
2.61 |
1.27 |
11 |
0.146 |
KZDD-018 |
129 |
130 |
1 |
1.645 |
0.708 |
9 |
0.111 |
KZDD-018 |
130 |
131 |
1 |
0.334 |
0.164 |
<1 |
0.03 |
KZDD-018 |
131 |
132 |
1 |
0.437 |
0.247 |
2 |
0.065 |
KZDD-018 |
132 |
133 |
1 |
2.53 |
0.945 |
10 |
0.167 |
KZDD-018 |
133 |
133.8 |
0.8 |
1.165 |
0.588 |
5 |
0.172 |
KZDD-018 |
133.8 |
134.3 |
0.5 |
0.4 |
0.187 |
1 |
0.199 |
KZDD-018 |
134.3 |
135.3 |
1 |
2.44 |
1.165 |
14 |
0.197 |
KZDD-018 |
135.3 |
136.3 |
1 |
0.851 |
0.39 |
3 |
0.209 |
KZDD-018 |
136.3 |
137.3 |
1 |
0.052 |
0.038 |
<1 |
0.116 |
KZDD-018 |
137.3 |
138.3 |
1 |
1.65 |
0.753 |
7 |
0.27 |
KZDD-018 |
138.3 |
139.3 |
1 |
2.36 |
0.999 |
10 |
0.15 |
KZDD-018 |
139.3 |
140 |
0.7 |
0.071 |
0.029 |
1 |
0.007 |
KZDD-018 |
140 |
141 |
1 |
0.022 |
0.014 |
<1 |
0.014 |
KZDD-018 |
141 |
142 |
1 |
0.037 |
0.016 |
<1 |
0.017 |
KZDD-018 |
142 |
144 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
144 |
146 |
2 |
0.045 |
0.026 |
<1 |
0.01 |
KZDD-018 |
146 |
148 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-018 |
148 |
150 |
2 |
0.005 |
<0.005 |
<1 |
0.021 |
KZDD-018 |
150 |
152 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
0 |
46 |
46 |
Not Sampled |
|||
KZDD-019 |
46 |
48 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
48 |
50 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
50 |
52 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
52 |
54 |
2 |
0.008 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
54 |
56 |
2 |
0.01 |
<0.005 |
<1 |
0.005 |
KZDD-019 |
56 |
57 |
1 |
0.008 |
<0.005 |
<1 |
0.012 |
KZDD-019 |
57 |
58 |
1 |
0.013 |
0.008 |
<1 |
0.009 |
KZDD-019 |
58 |
60 |
2 |
0.019 |
0.007 |
<1 |
0.008 |
KZDD-019 |
60 |
62 |
2 |
0.013 |
0.018 |
<1 |
0.01 |
KZDD-019 |
62 |
62.6 |
0.6 |
0.02 |
0.037 |
<1 |
0.019 |
KZDD-019 |
62.6 |
63.5 |
0.9 |
0.037 |
0.025 |
<1 |
0.028 |
KZDD-019 |
63.5 |
65 |
1.5 |
0.02 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
65 |
67 |
2 |
0.019 |
<0.005 |
<1 |
0.015 |
KZDD-019 |
67 |
69 |
2 |
0.01 |
<0.005 |
<1 |
0.012 |
KZDD-019 |
69 |
71 |
2 |
0.009 |
<0.005 |
<1 |
0.005 |
KZDD-019 |
71 |
73 |
2 |
0.01 |
<0.005 |
<1 |
0.01 |
KZDD-019 |
73 |
75 |
2 |
0.008 |
<0.005 |
<1 |
0.013 |
KZDD-019 |
75 |
77 |
2 |
0.006 |
<0.005 |
<1 |
0.007 |
KZDD-019 |
77 |
78.2 |
1.2 |
0.01 |
<0.005 |
<1 |
0.006 |
KZDD-019 |
78.2 |
79 |
0.8 |
0.298 |
0.112 |
1 |
0.064 |
KZDD-019 |
79 |
81 |
2 |
<0.005 |
<0.005 |
<1 |
0.005 |
KZDD-019 |
81 |
83 |
2 |
0.006 |
<0.005 |
<1 |
0.006 |
KZDD-019 |
83 |
85 |
2 |
<0.005 |
<0.005 |
<1 |
0.005 |
KZDD-019 |
85 |
87 |
2 |
<0.005 |
<0.005 |
<1 |
0.009 |
KZDD-019 |
87 |
89 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-019 |
89 |
159 |
70 |
Not Sampled |
|||
KZDD-020 |
0 |
39.1 |
39.1 |
Not Sampled |
|||
KZDD-020 |
39.1 |
41.1 |
2 |
0.005 |
<0.005 |
<1 |
0.012 |
KZDD-020 |
41.1 |
43.1 |
2 |
0.008 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
43.1 |
45.1 |
2 |
0.006 |
<0.005 |
<1 |
0.006 |
KZDD-020 |
45.1 |
47.1 |
2 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
47.1 |
49.1 |
2 |
0.015 |
<0.005 |
<1 |
0.006 |
KZDD-020 |
49.1 |
49.6 |
0.5 |
1.105 |
2.89 |
19 |
0.14 |
KZDD-020 |
49.6 |
50.4 |
0.8 |
0.059 |
0.035 |
<1 |
0.025 |
KZDD-020 |
50.4 |
51.1 |
0.7 |
0.053 |
0.032 |
<1 |
0.016 |
KZDD-020 |
51.1 |
51.6 |
0.5 |
1.89 |
0.401 |
3 |
0.167 |
KZDD-020 |
51.6 |
53.6 |
2 |
0.01 |
0.006 |
<1 |
0.006 |
KZDD-020 |
53.6 |
55.6 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
55.6 |
56.7 |
1.1 |
0.008 |
<0.005 |
<1 |
0.007 |
KZDD-020 |
56.7 |
57.4 |
0.7 |
0.011 |
0.025 |
<1 |
0.006 |
KZDD-020 |
57.4 |
59.4 |
2 |
0.009 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
59.4 |
60.4 |
1 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
60.4 |
62.4 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
62.4 |
63.4 |
1 |
0.014 |
0.005 |
<1 |
0.006 |
KZDD-020 |
63.4 |
65.4 |
2 |
0.006 |
<0.005 |
<1 |
0.02 |
KZDD-020 |
65.4 |
67 |
1.6 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
67 |
69 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
69 |
71 |
2 |
<0.005 |
<0.005 |
<1 |
0.012 |
KZDD-020 |
71 |
73 |
2 |
<0.005 |
<0.005 |
1 |
0.009 |
KZDD-020 |
73 |
88.9 |
15.9 |
Not Sampled |
|||
KZDD-020 |
88.9 |
90.9 |
2 |
0.017 |
0.009 |
<1 |
0.018 |
KZDD-020 |
90.9 |
92.9 |
2 |
0.015 |
0.005 |
<1 |
0.018 |
KZDD-020 |
92.9 |
94.9 |
2 |
0.011 |
<0.005 |
<1 |
0.025 |
KZDD-020 |
94.9 |
96.9 |
2 |
0.01 |
<0.005 |
<1 |
0.013 |
KZDD-020 |
96.9 |
98.9 |
2 |
0.007 |
<0.005 |
<1 |
0.006 |
KZDD-020 |
98.9 |
99.5 |
0.6 |
0.017 |
0.011 |
<1 |
0.072 |
KZDD-020 |
99.5 |
100.2 |
0.7 |
0.058 |
0.053 |
<1 |
0.106 |
KZDD-020 |
100.2 |
100.8 |
0.6 |
0.181 |
0.248 |
2 |
0.058 |
KZDD-020 |
100.8 |
101.5 |
0.7 |
0.83 |
0.204 |
3 |
0.146 |
KZDD-020 |
101.5 |
102.4 |
0.9 |
2.29 |
1.01 |
11 |
0.206 |
KZDD-020 |
102.4 |
103 |
0.6 |
8.64 |
3.29 |
35 |
0.323 |
KZDD-020 |
103 |
103.8 |
0.8 |
11.4 |
3.73 |
40 |
1 |
KZDD-020 |
103.8 |
104.5 |
0.7 |
18.6 |
8.42 |
91 |
1.03 |
KZDD-020 |
104.5 |
105.25 |
0.75 |
22.2 |
8.49 |
99 |
0.694 |
KZDD-020 |
105.25 |
106 |
0.75 |
30.5 |
14.3 |
151 |
0.46 |
KZDD-020 |
106 |
106.7 |
0.7 |
24.2 |
10.05 |
100 |
0.246 |
KZDD-020 |
106.7 |
107.3 |
0.6 |
21.7 |
9.8 |
100 |
0.467 |
KZDD-020 |
107.3 |
108 |
0.7 |
5.56 |
3.26 |
35 |
0.622 |
KZDD-020 |
108 |
109 |
1 |
10.05 |
3.98 |
41 |
0.979 |
KZDD-020 |
109 |
110 |
1 |
10.95 |
3.14 |
33 |
0.367 |
KZDD-020 |
110 |
110.5 |
0.5 |
3.13 |
1.12 |
10 |
0.257 |
KZDD-020 |
110.5 |
112 |
1.5 |
0.428 |
0.543 |
4 |
0.216 |
KZDD-020 |
112 |
112.7 |
0.7 |
1.48 |
6.13 |
68 |
1.645 |
KZDD-020 |
112.7 |
113.5 |
0.8 |
1.19 |
1.455 |
19 |
0.626 |
KZDD-020 |
113.5 |
114.5 |
1 |
1.15 |
0.881 |
13 |
0.833 |
KZDD-020 |
114.5 |
115.5 |
1 |
0.622 |
0.326 |
1 |
0.207 |
KZDD-020 |
115.5 |
116.5 |
1 |
1.61 |
0.554 |
5 |
0.195 |
KZDD-020 |
116.5 |
117.3 |
0.8 |
0.795 |
0.421 |
3 |
0.164 |
KZDD-020 |
117.3 |
118 |
0.7 |
4.76 |
2.16 |
19 |
0.534 |
KZDD-020 |
118 |
119 |
1 |
7.24 |
4.21 |
42 |
0.684 |
KZDD-020 |
119 |
120 |
1 |
15.45 |
6.65 |
64 |
0.636 |
KZDD-020 |
120 |
120.6 |
0.6 |
11.65 |
4.91 |
45 |
0.347 |
KZDD-020 |
120.6 |
121.5 |
0.9 |
1.08 |
0.831 |
12 |
0.532 |
KZDD-020 |
121.5 |
122.5 |
1 |
0.31 |
0.141 |
4 |
0.424 |
KZDD-020 |
122.5 |
123.2 |
0.7 |
0.131 |
0.087 |
3 |
0.353 |
KZDD-020 |
123.2 |
123.9 |
0.7 |
0.352 |
0.177 |
1 |
0.917 |
KZDD-020 |
123.9 |
124.6 |
0.7 |
0.753 |
0.451 |
3 |
0.361 |
KZDD-020 |
124.6 |
125.5 |
0.9 |
1.355 |
0.378 |
18 |
0.42 |
KZDD-020 |
125.5 |
126 |
0.5 |
0.498 |
0.392 |
4 |
0.152 |
KZDD-020 |
126 |
127 |
1 |
0.217 |
0.29 |
<1 |
0.715 |
KZDD-020 |
127 |
128 |
1 |
0.106 |
0.097 |
<1 |
0.215 |
KZDD-020 |
128 |
128.5 |
0.5 |
1.7 |
0.606 |
5 |
0.425 |
KZDD-020 |
128.5 |
129.5 |
1 |
1.565 |
0.834 |
8 |
0.336 |
KZDD-020 |
129.5 |
130.1 |
0.6 |
3.85 |
3.6 |
46 |
0.651 |
KZDD-020 |
130.1 |
130.7 |
0.6 |
3.68 |
0.944 |
9 |
0.431 |
KZDD-020 |
130.7 |
131.5 |
0.8 |
0.58 |
0.322 |
4 |
0.334 |
KZDD-020 |
131.5 |
132 |
0.5 |
1.33 |
0.601 |
4 |
0.269 |
KZDD-020 |
132 |
133 |
1 |
2.07 |
0.829 |
9 |
0.424 |
KZDD-020 |
133 |
134 |
1 |
11.1 |
4.57 |
52 |
0.356 |
KZDD-020 |
134 |
135 |
1 |
2.85 |
1.015 |
8 |
0.259 |
KZDD-020 |
135 |
136 |
1 |
3.12 |
1.165 |
14 |
0.191 |
KZDD-020 |
136 |
137 |
1 |
4.34 |
2.13 |
24 |
0.279 |
KZDD-020 |
137 |
138 |
1 |
2.46 |
1.07 |
12 |
0.256 |
KZDD-020 |
138 |
139 |
1 |
1.015 |
0.41 |
1 |
0.112 |
KZDD-020 |
139 |
140 |
1 |
5.37 |
2.71 |
28 |
0.275 |
KZDD-020 |
140 |
141 |
1 |
1.975 |
0.932 |
10 |
0.18 |
KZDD-020 |
141 |
142 |
1 |
2.69 |
1.91 |
22 |
0.251 |
KZDD-020 |
142 |
143 |
1 |
0.393 |
0.159 |
2 |
0.057 |
KZDD-020 |
143 |
143.9 |
0.9 |
0.352 |
0.145 |
2 |
0.035 |
KZDD-020 |
143.9 |
144.8 |
0.9 |
1.36 |
0.645 |
9 |
0.257 |
KZDD-020 |
144.8 |
145.5 |
0.7 |
0.69 |
0.55 |
7 |
0.119 |
KZDD-020 |
145.5 |
146.5 |
1 |
0.428 |
0.493 |
5 |
0.087 |
KZDD-020 |
146.5 |
147.4 |
0.9 |
0.013 |
0.005 |
<1 |
0.013 |
KZDD-020 |
147.4 |
148 |
0.6 |
1.305 |
0.565 |
7 |
0.078 |
KZDD-020 |
148 |
149 |
1 |
1.265 |
0.569 |
9 |
0.124 |
KZDD-020 |
149 |
150 |
1 |
1.79 |
0.872 |
12 |
0.112 |
KZDD-020 |
150 |
151 |
1 |
0.347 |
0.159 |
3 |
0.014 |
KZDD-020 |
151 |
152 |
1 |
0.216 |
0.168 |
2 |
0.01 |
KZDD-020 |
152 |
153 |
1 |
0.632 |
0.373 |
6 |
0.052 |
KZDD-020 |
153 |
154 |
1 |
0.703 |
0.55 |
10 |
0.103 |
KZDD-020 |
154 |
155 |
1 |
0.026 |
0.007 |
1 |
0.009 |
KZDD-020 |
155 |
156 |
1 |
0.05 |
0.03 |
<1 |
0.014 |
KZDD-020 |
156 |
157 |
1 |
0.025 |
0.013 |
1 |
0.013 |
KZDD-020 |
157 |
157.5 |
0.5 |
1.885 |
0.767 |
17 |
0.047 |
KZDD-020 |
157.5 |
158.1 |
0.6 |
0.077 |
0.023 |
1 |
0.036 |
KZDD-020 |
158.1 |
159.4 |
1.3 |
0.199 |
0.11 |
1 |
0.017 |
KZDD-020 |
159.4 |
161 |
1.6 |
0.01 |
<0.005 |
<1 |
0.016 |
KZDD-020 |
161 |
163 |
2 |
0.009 |
<0.005 |
<1 |
0.006 |
KZDD-020 |
163 |
165 |
2 |
0.005 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
165 |
167 |
2 |
0.006 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
167 |
169 |
2 |
<0.005 |
<0.005 |
<1 |
0.007 |
KZDD-020 |
169 |
200.5 |
31.5 |
Not Sampled |
|||
KZDD-020 |
200.5 |
202.5 |
2 |
0.006 |
<0.005 |
<1 |
0.006 |
KZDD-020 |
202.5 |
204.5 |
2 |
<0.005 |
<0.005 |
<1 |
0.007 |
KZDD-020 |
204.5 |
206.5 |
2 |
<0.005 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
206.5 |
208.5 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
208.5 |
210.5 |
2 |
0.006 |
<0.005 |
<1 |
0.007 |
KZDD-020 |
210.5 |
211.5 |
1 |
<0.005 |
0.009 |
<1 |
0.028 |
KZDD-020 |
211.5 |
213.5 |
2 |
0.007 |
<0.005 |
<1 |
0.008 |
KZDD-020 |
213.5 |
215.5 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
215.5 |
217.5 |
2 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
217.5 |
219.5 |
2 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-020 |
219.5 |
221.5 |
2 |
0.009 |
<0.005 |
<1 |
0.005 |
KZDD-020 |
221.5 |
237.2 |
15.7 |
Not Sampled |
|||
KZDD-021 |
0 |
3 |
3 |
Not Sampled |
|||
KZDD-021 |
3 |
5 |
2 |
0.011 |
0.005 |
<1 |
<0.005 |
KZDD-021 |
5 |
7.5 |
2.5 |
0.037 |
0.016 |
<1 |
0.006 |
KZDD-021 |
7.5 |
9.5 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
9.5 |
11.5 |
2 |
0.011 |
<0.005 |
<1 |
0.012 |
KZDD-021 |
11.5 |
12.7 |
1.2 |
0.008 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
12.7 |
14 |
1.3 |
0.011 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
14 |
14.5 |
0.5 |
0.422 |
0.233 |
<1 |
0.012 |
KZDD-021 |
14.5 |
15.7 |
1.2 |
0.477 |
0.271 |
2 |
0.057 |
KZDD-021 |
15.7 |
17.5 |
1.8 |
0.012 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
17.5 |
19.6 |
2.1 |
0.123 |
<0.005 |
<1 |
0.007 |
KZDD-021 |
19.6 |
20.5 |
0.9 |
0.083 |
<0.005 |
<1 |
0.008 |
KZDD-021 |
20.5 |
22.5 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
22.5 |
24 |
1.5 |
0.013 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
24 |
25 |
1 |
0.006 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
25 |
26.5 |
1.5 |
0.077 |
0.005 |
<1 |
<0.005 |
KZDD-021 |
26.5 |
29.5 |
3 |
0.322 |
0.354 |
11 |
0.135 |
KZDD-021 |
29.5 |
30.2 |
0.7 |
4.25 |
2.69 |
39 |
0.365 |
KZDD-021 |
30.2 |
31 |
0.8 |
6.7 |
3.2 |
43 |
0.368 |
KZDD-021 |
31 |
32 |
1 |
5.36 |
2.28 |
26 |
0.318 |
KZDD-021 |
32 |
33 |
1 |
7.85 |
3.78 |
41 |
0.294 |
KZDD-021 |
33 |
34.8 |
1.8 |
2.35 |
1.205 |
12 |
0.215 |
KZDD-021 |
34.8 |
35.4 |
0.6 |
1.62 |
0.921 |
7 |
0.087 |
KZDD-021 |
35.4 |
36.6 |
1.2 |
0.204 |
0.109 |
<1 |
0.024 |
KZDD-021 |
36.6 |
38 |
1.4 |
0.009 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
38 |
41.5 |
3.5 |
0.01 |
<0.005 |
<1 |
<0.005 |
KZDD-021 |
41.5 |
43 |
1.5 |
0.005 |
<0.005 |
<1 |
0.006 |
KZDD-021 |
43 |
45 |
2 |
0.008 |
<0.005 |
<1 |
0.007 |
KZDD-021 |
45 |
47 |
2 |
0.009 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
0 |
2 |
2 |
0.93 |
0.013 |
1 |
0.109 |
SSDD-002 |
2 |
3 |
1 |
0.814 |
0.011 |
<1 |
0.099 |
SSDD-002 |
3 |
4 |
1 |
0.745 |
0.013 |
<1 |
0.148 |
SSDD-002 |
4 |
5 |
1 |
0.718 |
0.019 |
1 |
0.14 |
SSDD-002 |
5 |
6 |
1 |
0.871 |
0.016 |
<1 |
0.091 |
SSDD-002 |
6 |
7 |
1 |
1.035 |
0.02 |
1 |
0.135 |
SSDD-002 |
7 |
7.6 |
0.6 |
2 |
0.03 |
1 |
0.134 |
SSDD-002 |
7.6 |
8.6 |
1 |
2.07 |
0.02 |
1 |
0.184 |
SSDD-002 |
8.6 |
9.1 |
0.5 |
7.29 |
2.48 |
35 |
0.346 |
SSDD-002 |
9.1 |
10.1 |
1 |
0.735 |
0.008 |
<1 |
0.015 |
SSDD-002 |
10.1 |
11.1 |
1 |
1.985 |
0.008 |
1 |
0.018 |
SSDD-002 |
11.1 |
12.1 |
1 |
1.75 |
0.007 |
<1 |
0.007 |
SSDD-002 |
12.1 |
13.1 |
1 |
3.59 |
0.088 |
3 |
0.052 |
SSDD-002 |
13.1 |
13.8 |
0.7 |
11.5 |
5 |
79 |
3.92 |
SSDD-002 |
13.8 |
14.3 |
0.5 |
19.15 |
8.16 |
122 |
0.498 |
SSDD-002 |
14.3 |
15 |
0.7 |
8.63 |
2.11 |
30 |
0.26 |
SSDD-002 |
15 |
16 |
1 |
0.474 |
0.07 |
3 |
0.154 |
SSDD-002 |
16 |
17 |
1 |
0.316 |
0.075 |
4 |
0.322 |
SSDD-002 |
17 |
18 |
1 |
0.525 |
0.074 |
3 |
0.181 |
SSDD-002 |
18 |
19 |
1 |
0.217 |
0.022 |
1 |
0.047 |
SSDD-002 |
19 |
20 |
1 |
0.128 |
0.013 |
<1 |
0.067 |
SSDD-002 |
20 |
21 |
1 |
0.262 |
0.018 |
3 |
0.098 |
SSDD-002 |
21 |
22 |
1 |
0.295 |
0.031 |
2 |
0.084 |
SSDD-002 |
22 |
23 |
1 |
0.114 |
0.012 |
2 |
0.083 |
SSDD-002 |
23 |
23.9 |
0.9 |
0.13 |
0.029 |
2 |
0.125 |
SSDD-002 |
23.9 |
25 |
1.1 |
0.721 |
0.099 |
3 |
0.142 |
SSDD-002 |
25 |
26 |
1 |
0.081 |
0.017 |
2 |
0.098 |
SSDD-002 |
26 |
27 |
1 |
0.205 |
0.034 |
2 |
0.089 |
SSDD-002 |
27 |
28 |
1 |
0.143 |
0.049 |
4 |
0.167 |
SSDD-002 |
28 |
29 |
1 |
0.989 |
0.233 |
5 |
0.128 |
SSDD-002 |
29 |
30 |
1 |
0.385 |
0.177 |
5 |
0.152 |
SSDD-002 |
30 |
31 |
1 |
0.744 |
0.276 |
5 |
0.246 |
SSDD-002 |
31 |
31.7 |
0.7 |
0.94 |
0.555 |
9 |
0.212 |
SSDD-002 |
31.7 |
32.3 |
0.6 |
7.18 |
3.03 |
53 |
0.25 |
SSDD-002 |
32.3 |
33 |
0.7 |
11.3 |
4.01 |
67 |
0.358 |
SSDD-002 |
33 |
33.5 |
0.5 |
14 |
4.48 |
73 |
0.458 |
SSDD-002 |
33.5 |
34 |
0.5 |
3.72 |
0.6 |
10 |
1.875 |
SSDD-002 |
34 |
34.5 |
0.5 |
3.27 |
1.11 |
23 |
5.94 |
SSDD-002 |
34.5 |
35.5 |
1 |
3.03 |
0.942 |
9 |
0.117 |
SSDD-002 |
35.5 |
36.5 |
1 |
0.479 |
0.29 |
4 |
0.067 |
SSDD-002 |
36.5 |
37.5 |
1 |
0.059 |
0.024 |
2 |
0.022 |
SSDD-002 |
37.5 |
38 |
0.5 |
1.6 |
0.662 |
5 |
0.054 |
SSDD-002 |
38 |
39 |
1 |
0.029 |
0.02 |
<1 |
0.032 |
SSDD-002 |
39 |
40 |
1 |
0.459 |
0.132 |
1 |
0.032 |
SSDD-002 |
40 |
41 |
1 |
0.012 |
0.007 |
1 |
0.026 |
SSDD-002 |
41 |
42 |
1 |
0.013 |
0.026 |
<1 |
0.019 |
SSDD-002 |
42 |
43 |
1 |
0.03 |
0.005 |
1 |
0.022 |
SSDD-002 |
43 |
44 |
1 |
2.77 |
2.12 |
18 |
0.068 |
SSDD-002 |
44 |
46 |
2 |
0.018 |
0.009 |
1 |
0.01 |
SSDD-002 |
46 |
48 |
2 |
0.041 |
0.02 |
<1 |
0.029 |
SSDD-002 |
48 |
50 |
2 |
0.166 |
0.06 |
<1 |
0.042 |
SSDD-002 |
50 |
52 |
2 |
0.546 |
0.183 |
1 |
0.05 |
SSDD-002 |
52 |
54 |
2 |
0.034 |
0.01 |
<1 |
0.024 |
SSDD-002 |
54 |
55.3 |
1.3 |
0.051 |
0.018 |
<1 |
0.021 |
SSDD-002 |
55.3 |
56.8 |
1.5 |
0.059 |
0.017 |
<1 |
0.019 |
SSDD-002 |
56.8 |
57.7 |
0.9 |
0.024 |
0.006 |
<1 |
0.016 |
SSDD-002 |
57.7 |
58.7 |
1 |
0.201 |
0.198 |
3 |
0.021 |
SSDD-002 |
58.7 |
59.6 |
0.9 |
0.081 |
0.006 |
<1 |
<0.005 |
SSDD-002 |
59.6 |
60.6 |
1 |
0.132 |
0.05 |
<1 |
0.014 |
SSDD-002 |
60.6 |
62.5 |
1.9 |
0.015 |
0.005 |
<1 |
0.005 |
SSDD-002 |
62.5 |
63.5 |
1 |
0.045 |
0.03 |
1 |
0.029 |
SSDD-002 |
63.5 |
64.5 |
1 |
0.382 |
0.134 |
2 |
0.021 |
SSDD-002 |
64.5 |
66.5 |
2 |
0.02 |
0.011 |
<1 |
0.008 |
SSDD-002 |
66.5 |
68.5 |
2 |
0.012 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
68.5 |
70.5 |
2 |
0.014 |
<0.005 |
<1 |
0.006 |
SSDD-002 |
70.5 |
71.8 |
1.3 |
0.015 |
<0.005 |
<1 |
0.005 |
SSDD-002 |
71.8 |
74.8 |
3 |
0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
74.8 |
75.5 |
0.7 |
0.005 |
<0.005 |
1 |
0.008 |
SSDD-002 |
75.5 |
76.5 |
1 |
0.007 |
<0.005 |
<1 |
0.008 |
SSDD-002 |
76.5 |
77.5 |
1 |
0.01 |
<0.005 |
<1 |
0.015 |
SSDD-002 |
77.5 |
78.5 |
1 |
0.006 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
78.5 |
79.5 |
1 |
0.01 |
<0.005 |
<1 |
0.013 |
SSDD-002 |
79.5 |
80.5 |
1 |
0.007 |
<0.005 |
<1 |
0.015 |
SSDD-002 |
80.5 |
81.5 |
1 |
0.009 |
<0.005 |
<1 |
0.011 |
SSDD-002 |
81.5 |
82.5 |
1 |
0.013 |
0.005 |
<1 |
0.019 |
SSDD-002 |
82.5 |
83.5 |
1 |
0.008 |
0.005 |
1 |
0.03 |
SSDD-002 |
83.5 |
84.5 |
1 |
0.019 |
<0.005 |
1 |
0.021 |
SSDD-002 |
84.5 |
85.5 |
1 |
0.006 |
<0.005 |
<1 |
0.023 |
SSDD-002 |
85.5 |
86.5 |
1 |
<0.005 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
86.5 |
87.7 |
1.2 |
0.005 |
<0.005 |
<1 |
0.013 |
SSDD-002 |
87.7 |
88.6 |
0.9 |
<0.005 |
<0.005 |
<1 |
0.013 |
SSDD-002 |
88.6 |
89.6 |
1 |
<0.005 |
<0.005 |
<1 |
0.019 |
SSDD-002 |
89.6 |
90.6 |
1 |
<0.005 |
<0.005 |
<1 |
0.024 |
SSDD-002 |
90.6 |
92.6 |
2 |
0.01 |
<0.005 |
<1 |
0.035 |
SSDD-002 |
92.6 |
93.6 |
1 |
0.012 |
0.005 |
1 |
0.034 |
SSDD-002 |
93.6 |
94.6 |
1 |
0.006 |
<0.005 |
1 |
0.015 |
SSDD-002 |
94.6 |
95.6 |
1 |
0.006 |
<0.005 |
<1 |
0.029 |
SSDD-002 |
95.6 |
96.8 |
1.2 |
<0.005 |
<0.005 |
<1 |
0.03 |
SSDD-002 |
96.8 |
98.6 |
1.8 |
0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
98.6 |
100.6 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
100.6 |
102.4 |
1.8 |
0.01 |
<0.005 |
<1 |
0.008 |
SSDD-002 |
102.4 |
103 |
0.6 |
0.079 |
0.027 |
<1 |
0.027 |
SSDD-002 |
103 |
104 |
1 |
0.122 |
0.04 |
<1 |
0.015 |
SSDD-002 |
104 |
105 |
1 |
0.023 |
0.008 |
<1 |
0.039 |
SSDD-002 |
105 |
106 |
1 |
0.02 |
0.008 |
<1 |
0.042 |
SSDD-002 |
106 |
106.5 |
0.5 |
0.011 |
0.013 |
1 |
0.01 |
SSDD-002 |
106.5 |
107.5 |
1 |
0.061 |
0.064 |
1 |
0.049 |
SSDD-002 |
107.5 |
108.5 |
1 |
0.075 |
0.038 |
2 |
0.041 |
SSDD-002 |
108.5 |
109.5 |
1 |
0.008 |
<0.005 |
<1 |
0.031 |
SSDD-002 |
109.5 |
110 |
0.5 |
0.214 |
0.112 |
1 |
0.022 |
SSDD-002 |
110 |
111 |
1 |
0.005 |
0.007 |
1 |
0.018 |
SSDD-002 |
111 |
112 |
1 |
0.008 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
112 |
113 |
1 |
<0.005 |
<0.005 |
1 |
0.024 |
SSDD-002 |
113 |
114 |
1 |
0.049 |
0.02 |
<1 |
0.026 |
SSDD-002 |
114 |
114.8 |
0.8 |
0.074 |
0.039 |
1 |
0.042 |
SSDD-002 |
114.8 |
115.8 |
1 |
0.006 |
0.008 |
1 |
0.09 |
SSDD-002 |
115.8 |
116.8 |
1 |
0.006 |
0.006 |
1 |
0.029 |
SSDD-002 |
116.8 |
117.8 |
1 |
0.043 |
0.015 |
<1 |
0.025 |
SSDD-002 |
117.8 |
119.8 |
2 |
0.006 |
0.005 |
<1 |
0.006 |
SSDD-002 |
119.8 |
121.8 |
2 |
<0.005 |
<0.005 |
<1 |
0.005 |
SSDD-002 |
121.8 |
123.8 |
2 |
<0.005 |
<0.005 |
1 |
<0.005 |
SSDD-002 |
123.8 |
125 |
1.2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
125 |
126 |
1 |
<0.005 |
<0.005 |
<1 |
0.015 |
SSDD-002 |
126 |
126.5 |
0.5 |
2.77 |
0.262 |
4 |
0.028 |
SSDD-002 |
126.5 |
127.5 |
1 |
0.007 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
127.5 |
129.6 |
2.1 |
0.703 |
0.118 |
1 |
<0.005 |
SSDD-002 |
129.6 |
130.5 |
0.9 |
0.027 |
0.024 |
<1 |
0.026 |
SSDD-002 |
130.5 |
131.1 |
0.6 |
0.013 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
131.1 |
133.1 |
2 |
0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
133.1 |
135.1 |
2 |
0.027 |
0.014 |
1 |
<0.005 |
SSDD-002 |
135.1 |
136.2 |
1.1 |
0.018 |
0.03 |
<1 |
0.009 |
SSDD-002 |
136.2 |
137.4 |
1.2 |
0.165 |
0.096 |
1 |
0.005 |
SSDD-002 |
137.4 |
138 |
0.6 |
6.37 |
3.09 |
49 |
0.044 |
SSDD-002 |
138 |
139 |
1 |
0.493 |
0.406 |
7 |
0.034 |
SSDD-002 |
139 |
140.2 |
1.2 |
0.046 |
0.026 |
<1 |
0.005 |
SSDD-002 |
140.2 |
141.2 |
1 |
0.017 |
0.011 |
<1 |
0.008 |
SSDD-002 |
141.2 |
141.7 |
0.5 |
0.025 |
0.009 |
<1 |
<0.005 |
SSDD-002 |
141.7 |
143.2 |
1.5 |
0.006 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
143.2 |
144.2 |
1 |
0.007 |
<0.005 |
<1 |
0.006 |
SSDD-002 |
144.2 |
146 |
1.8 |
0.228 |
0.046 |
<1 |
0.01 |
SSDD-002 |
146 |
146.7 |
0.7 |
0.447 |
0.201 |
<1 |
0.011 |
SSDD-002 |
146.7 |
147.3 |
0.6 |
14.25 |
4.72 |
74 |
0.272 |
SSDD-002 |
147.3 |
148.8 |
1.5 |
0.03 |
0.039 |
<1 |
0.015 |
SSDD-002 |
148.8 |
150.5 |
1.7 |
0.028 |
0.014 |
<1 |
0.007 |
SSDD-002 |
150.5 |
152 |
1.5 |
<0.005 |
<0.005 |
<1 |
0.013 |
SSDD-002 |
152 |
153.2 |
1.2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
153.2 |
153.9 |
0.7 |
0.253 |
0.154 |
<1 |
0.02 |
SSDD-002 |
153.9 |
154.7 |
0.8 |
0.009 |
0.01 |
<1 |
0.007 |
SSDD-002 |
154.7 |
155.2 |
0.5 |
11.3 |
4.86 |
109 |
0.075 |
SSDD-002 |
155.2 |
155.8 |
0.6 |
0.21 |
0.191 |
4 |
0.008 |
SSDD-002 |
155.8 |
156.5 |
0.7 |
0.28 |
0.143 |
4 |
0.012 |
SSDD-002 |
156.5 |
158.5 |
2 |
0.005 |
<0.005 |
1 |
<0.005 |
SSDD-002 |
158.5 |
160.5 |
2 |
0.007 |
0.007 |
<1 |
<0.005 |
SSDD-002 |
160.5 |
162.5 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
162.5 |
164.5 |
2 |
0.01 |
0.01 |
<1 |
<0.005 |
SSDD-002 |
164.5 |
166.5 |
2 |
<0.005 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
166.5 |
168.5 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
168.5 |
170.5 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
170.5 |
172.5 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
172.5 |
174.5 |
2 |
0.008 |
<0.005 |
<1 |
0.007 |
SSDD-002 |
174.5 |
176.5 |
2 |
0.005 |
<0.005 |
<1 |
0.005 |
SSDD-002 |
176.5 |
178.5 |
2 |
<0.005 |
<0.005 |
<1 |
0.074 |
SSDD-002 |
178.5 |
180.5 |
2 |
0.011 |
0.006 |
1 |
<0.005 |
SSDD-002 |
180.5 |
182.5 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
182.5 |
184.5 |
2 |
0.011 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
184.5 |
186.5 |
2 |
0.007 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
186.5 |
188.5 |
2 |
0.006 |
<0.005 |
<1 |
<0.005 |
SSDD-002 |
188.5 |
190.5 |
2 |
0.007 |
0.005 |
<1 |
<0.005 |
SSDD-002 |
190.5 |
191.5 |
1 |
0.045 |
0.03 |
<1 |
0.014 |
SSDD-002 |
191.5 |
192.5 |
1 |
0.312 |
0.181 |
4 |
0.014 |
SSDD-002 |
192.5 |
193 |
0.5 |
0.105 |
0.292 |
8 |
0.014 |
SSDD-002 |
193 |
194 |
1 |
0.881 |
0.499 |
10 |
0.035 |
SSDD-002 |
194 |
195 |
1 |
0.33 |
0.406 |
8 |
0.026 |
SSDD-002 |
195 |
196.5 |
1.5 |
0.22 |
0.126 |
2 |
0.024 |
SSDD-002 |
196.5 |
198 |
1.5 |
0.192 |
0.138 |
5 |
0.01 |
SSDD-002 |
198 |
198.9 |
0.9 |
0.835 |
0.687 |
22 |
0.019 |
SSDD-002 |
198.9 |
199.8 |
0.9 |
0.266 |
0.462 |
14 |
0.011 |
SSDD-002 |
199.8 |
200.6 |
0.8 |
0.124 |
0.285 |
9 |
0.041 |
SSDD-002 |
200.6 |
201.6 |
1 |
0.025 |
0.063 |
3 |
0.029 |
SSDD-002 |
201.6 |
202.6 |
1 |
0.021 |
0.054 |
3 |
0.024 |
SSDD-002 |
202.6 |
203.6 |
1 |
0.118 |
0.2 |
6 |
0.011 |
SSDD-002 |
203.6 |
204.6 |
1 |
0.556 |
0.481 |
12 |
0.016 |
SSDD-002 |
204.6 |
205.6 |
1 |
0.769 |
0.597 |
15 |
0.021 |
SSDD-002 |
205.6 |
206.6 |
1 |
0.127 |
0.133 |
3 |
0.023 |
SSDD-002 |
206.6 |
207.2 |
0.6 |
0.04 |
0.03 |
1 |
0.01 |
SSDD-002 |
207.2 |
208 |
0.8 |
0.018 |
0.012 |
1 |
0.006 |
SSDD-002 |
208 |
209 |
1 |
<0.005 |
0.006 |
1 |
0.015 |
SSDD-002 |
209 |
210 |
1 |
0.13 |
0.294 |
8 |
0.026 |
SSDD-002 |
210 |
212 |
2 |
0.119 |
0.131 |
5 |
0.018 |
SSDD-002 |
212 |
214 |
2 |
0.036 |
0.024 |
1 |
<0.005 |
SSDD-002 |
214 |
216 |
2 |
0.105 |
0.153 |
5 |
0.018 |
SSDD-002 |
216 |
216.7 |
0.7 |
0.101 |
0.362 |
12 |
0.016 |
SSDD-002 |
216.7 |
217.5 |
0.8 |
0.01 |
0.811 |
55 |
0.434 |
SSDD-002 |
217.5 |
218 |
0.5 |
0.01 |
0.048 |
5 |
0.867 |
SSDD-002 |
218 |
220 |
2 |
0.008 |
0.046 |
4 |
0.036 |
SSDD-002 |
220 |
222 |
2 |
0.215 |
0.339 |
12 |
0.035 |
SSDD-002 |
222 |
224 |
2 |
0.174 |
0.144 |
4 |
0.008 |
SSDD-002 |
224 |
226 |
2 |
0.051 |
0.043 |
<1 |
<0.005 |
SSDD-002 |
226 |
228 |
2 |
0.053 |
0.05 |
1 |
0.006 |
SSDD-002 |
228 |
228.9 |
0.9 |
0.717 |
0.638 |
16 |
0.528 |
SSDD-002 |
228.9 |
229.4 |
0.5 |
2.88 |
1.265 |
44 |
4 |
SSDD-002 |
229.4 |
230.4 |
1 |
0.206 |
0.299 |
9 |
0.101 |
SSDD-002 |
230.4 |
231.3 |
0.9 |
0.115 |
0.241 |
9 |
0.035 |
SSDD-002 |
231.3 |
232.3 |
1 |
0.275 |
0.227 |
5 |
0.023 |
SSDD-002 |
232.3 |
233.3 |
1 |
0.347 |
0.279 |
5 |
0.067 |
SSDD-002 |
233.3 |
235 |
1.7 |
0.023 |
0.02 |
1 |
0.007 |
SSDD-002 |
235 |
237 |
2 |
0.01 |
0.015 |
1 |
0.014 |
SSDD-002 |
237 |
239 |
2 |
0.009 |
0.016 |
1 |
0.019 |
SSDD-002 |
239 |
240.7 |
1.7 |
0.027 |
0.024 |
1 |
0.02 |
SSDD-002 |
240.7 |
241.7 |
1 |
0.076 |
0.081 |
2 |
0.007 |
SSDD-002 |
241.7 |
242.7 |
1 |
0.05 |
0.05 |
1 |
0.012 |
SSDD-002 |
242.7 |
244.7 |
2 |
0.013 |
0.016 |
<1 |
0.007 |
SSDD-002 |
244.7 |
246.7 |
2 |
0.035 |
0.062 |
3 |
0.015 |
SSDD-002 |
246.7 |
248.7 |
2 |
0.031 |
0.038 |
2 |
0.01 |
SSDD-002 |
248.7 |
250.7 |
2 |
0.014 |
0.023 |
1 |
0.017 |
SSDD-002 |
250.7 |
252.7 |
2 |
0.1 |
0.211 |
6 |
0.01 |
SSDD-002 |
252.7 |
254.15 |
1.45 |
0.092 |
0.323 |
11 |
0.081 |
SSDD-002 |
254.15 |
255.15 |
1 |
<0.005 |
0.058 |
2 |
0.103 |
SSDD-002 |
255.15 |
256.15 |
1 |
<0.005 |
0.332 |
1 |
0.244 |
SSDD-002 |
256.15 |
257.15 |
1 |
0.006 |
0.543 |
7 |
1.785 |
SSDD-002 |
257.15 |
258 |
0.85 |
<0.005 |
0.123 |
1 |
0.169 |
SSDD-002 |
258 |
259 |
1 |
0.005 |
0.304 |
1 |
0.135 |
SSDD-002 |
259 |
260 |
1 |
0.013 |
0.174 |
1 |
0.145 |
SSDD-002 |
260 |
261 |
1 |
<0.005 |
0.014 |
<1 |
0.187 |
SSDD-002 |
261 |
262.3 |
1.3 |
<0.005 |
0.017 |
<1 |
0.168 |
SSDD-002 |
262.3 |
263.3 |
1 |
0.072 |
0.071 |
3 |
0.297 |
SSDD-002 |
263.3 |
264 |
0.7 |
0.753 |
0.149 |
5 |
1.33 |
SSDD-002 |
264 |
265 |
1 |
0.043 |
0.119 |
7 |
3.19 |
SSDD-002 |
265 |
265.9 |
0.9 |
0.007 |
0.02 |
2 |
0.983 |
SSDD-002 |
265.9 |
266.9 |
1 |
0.005 |
0.011 |
<1 |
0.203 |
SSDD-002 |
266.9 |
267.9 |
1 |
<0.005 |
0.028 |
<1 |
0.176 |
SSDD-002 |
267.9 |
268.6 |
0.7 |
0.036 |
0.04 |
<1 |
0.111 |
SSDD-002 |
268.6 |
270.6 |
2 |
0.008 |
0.025 |
<1 |
0.06 |
SSDD-002 |
270.6 |
272.6 |
2 |
0.043 |
0.025 |
<1 |
0.049 |
SSDD-002 |
272.6 |
274 |
1.4 |
0.006 |
0.025 |
<1 |
0.057 |
SSDD-002 |
274 |
275 |
1 |
<0.005 |
0.023 |
<1 |
0.129 |
SSDD-002 |
275 |
276 |
1 |
<0.005 |
0.06 |
1 |
0.367 |
SSDD-002 |
276 |
277 |
1 |
0.006 |
0.031 |
1 |
0.147 |
SSDD-002 |
277 |
278 |
1 |
0.007 |
0.031 |
1 |
0.084 |
SSDD-002 |
278 |
279 |
1 |
0.006 |
0.148 |
2 |
0.153 |
SSDD-002 |
279 |
280 |
1 |
0.015 |
0.066 |
3 |
0.262 |
SSDD-002 |
280 |
281 |
1 |
0.005 |
0.116 |
2 |
0.762 |
SSDD-002 |
281 |
282 |
1 |
0.019 |
0.124 |
5 |
0.331 |
SSDD-002 |
282 |
283 |
1 |
0.005 |
0.022 |
<1 |
0.18 |
SSDD-002 |
283 |
284 |
1 |
0.018 |
2.2 |
22 |
4.69 |
SSDD-002 |
284 |
284.9 |
0.9 |
0.01 |
0.033 |
2 |
0.185 |
SSDD-002 |
284.9 |
285.9 |
1 |
0.012 |
0.053 |
2 |
0.155 |
SSDD-002 |
285.9 |
286.9 |
1 |
0.016 |
0.05 |
3 |
2.56 |
SSDD-002 |
286.9 |
287.9 |
1 |
<0.005 |
0.026 |
2 |
0.977 |
SSDD-002 |
287.9 |
288.9 |
1 |
<0.005 |
0.022 |
<1 |
0.992 |
SSDD-002 |
288.9 |
289.9 |
1 |
0.083 |
0.083 |
3 |
0.239 |
SSDD-002 |
289.9 |
290.9 |
1 |
0.007 |
0.098 |
10 |
3.37 |
SSDD-002 |
290.9 |
291.9 |
1 |
<0.005 |
0.036 |
4 |
0.411 |
SSDD-002 |
291.9 |
292.9 |
1 |
<0.005 |
0.098 |
5 |
1.67 |
SSDD-002 |
292.9 |
293.9 |
1 |
0.006 |
0.049 |
3 |
13.6 |
SSDD-002 |
293.9 |
294.9 |
1 |
<0.005 |
0.05 |
2 |
0.758 |
SSDD-002 |
294.9 |
295.8 |
0.9 |
<0.005 |
0.037 |
2 |
0.566 |
SSDD-002 |
295.8 |
296.3 |
0.5 |
0.013 |
0.134 |
3 |
2.2 |
SSDD-002 |
296.3 |
297 |
0.7 |
0.007 |
0.043 |
48 |
0.695 |
SSDD-002 |
297 |
298 |
1 |
0.005 |
0.15 |
7 |
2.01 |
SSDD-002 |
298 |
299 |
1 |
<0.005 |
0.071 |
3 |
0.316 |
SSDD-002 |
299 |
300 |
1 |
0.024 |
0.051 |
1 |
0.349 |
SSDD-002 |
300 |
302 |
2 |
0.019 |
0.041 |
2 |
0.191 |
SSDD-002 |
302 |
304 |
2 |
0.027 |
0.046 |
1 |
0.103 |
SSDD-002 |
304 |
305 |
1 |
<0.005 |
0.035 |
1 |
0.441 |
SSDD-002 |
305 |
306 |
1 |
0.007 |
0.032 |
2 |
2.94 |
SSDD-002 |
306 |
307 |
1 |
0.021 |
0.035 |
1 |
0.369 |
SSDD-002 |
307 |
308 |
1 |
0.009 |
0.025 |
<1 |
0.067 |
SSDD-002 |
308 |
309 |
1 |
0.01 |
0.027 |
<1 |
0.266 |
SSDD-002 |
309 |
310 |
1 |
<0.005 |
0.026 |
<1 |
0.803 |
SSDD-002 |
310 |
311 |
1 |
0.007 |
0.009 |
<1 |
0.163 |
SSDD-002 |
311 |
313 |
2 |
0.04 |
0.063 |
<1 |
0.102 |
SSDD-002 |
313 |
314 |
1 |
0.053 |
0.083 |
1 |
0.028 |
SSDD-002 |
314 |
315 |
1 |
0.017 |
0.013 |
<1 |
0.042 |
SSDD-002 |
315 |
317.1 |
2.1 |
0.021 |
0.007 |
<1 |
0.016 |
SSDD-002 |
317.1 |
318 |
0.9 |
0.053 |
0.02 |
<1 |
0.019 |
SSDD-002 |
318 |
318.8 |
0.8 |
0.011 |
0.005 |
<1 |
0.009 |
SSDD-002 |
318.8 |
319.8 |
1 |
0.015 |
0.04 |
<1 |
0.112 |
SSDD-002 |
319.8 |
321.8 |
2 |
0.006 |
0.005 |
<1 |
0.014 |
SSDD-002 |
321.8 |
322.8 |
1 |
0.013 |
0.019 |
<1 |
0.114 |
SSDD-002 |
322.8 |
323.8 |
1 |
0.006 |
<0.005 |
<1 |
0.021 |
SSDD-002 |
323.8 |
325.3 |
1.5 |
0.006 |
0.007 |
<1 |
0.013 |
SSDD-002 |
325.3 |
326 |
0.7 |
0.007 |
0.009 |
1 |
0.137 |
SSDD-002 |
326 |
326.5 |
0.5 |
0.026 |
0.015 |
12 |
0.35 |
SSDD-002 |
326.5 |
327.5 |
1 |
0.006 |
<0.005 |
<1 |
0.056 |
SSDD-002 |
327.5 |
328.5 |
1 |
0.005 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
328.5 |
329.5 |
1 |
0.013 |
<0.005 |
<1 |
0.02 |
SSDD-002 |
329.5 |
330.5 |
1 |
0.01 |
0.009 |
<1 |
0.02 |
SSDD-002 |
330.5 |
331 |
0.5 |
<0.005 |
<0.005 |
<1 |
0.014 |
SSDD-002 |
331 |
331.7 |
0.7 |
<0.005 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
331.7 |
332.7 |
1 |
0.045 |
0.04 |
<1 |
0.043 |
SSDD-002 |
332.7 |
333.7 |
1 |
0.012 |
0.432 |
16 |
0.098 |
SSDD-002 |
333.7 |
334.7 |
1 |
<0.005 |
0.017 |
<1 |
0.009 |
SSDD-002 |
334.7 |
335.7 |
1 |
<0.005 |
<0.005 |
<1 |
0.059 |
SSDD-002 |
335.7 |
336.7 |
1 |
0.029 |
0.044 |
1 |
0.128 |
SSDD-002 |
336.7 |
337.7 |
1 |
<0.005 |
<0.005 |
<1 |
0.018 |
SSDD-002 |
337.7 |
339.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.017 |
SSDD-002 |
339.7 |
341.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.026 |
SSDD-002 |
341.7 |
343.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.026 |
SSDD-002 |
343.7 |
345.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.064 |
SSDD-002 |
345.7 |
347.7 |
2 |
0.006 |
<0.005 |
<1 |
0.031 |
SSDD-002 |
347.7 |
349.7 |
2 |
0.007 |
<0.005 |
<1 |
0.051 |
SSDD-002 |
349.7 |
351.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.011 |
SSDD-002 |
351.7 |
353.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.014 |
SSDD-002 |
353.7 |
355.7 |
2 |
<0.005 |
<0.005 |
<1 |
0.013 |
SSDD-002 |
355.7 |
356.2 |
0.5 |
<0.005 |
<0.005 |
<1 |
0.072 |
SSDD-002 |
356.2 |
356.9 |
0.7 |
0.011 |
0.01 |
1 |
0.149 |
SSDD-002 |
356.9 |
357.6 |
0.7 |
0.025 |
0.074 |
8 |
2.14 |
SSDD-002 |
357.6 |
358.6 |
1 |
<0.005 |
0.023 |
1 |
0.063 |
SSDD-002 |
358.6 |
359.6 |
1 |
0.01 |
0.009 |
<1 |
0.07 |
SSDD-002 |
359.6 |
360.6 |
1 |
0.014 |
0.071 |
6 |
0.121 |
SSDD-002 |
360.6 |
362 |
1.4 |
0.009 |
0.008 |
<1 |
0.017 |
SSDD-002 |
362 |
363 |
1 |
0.013 |
0.035 |
<1 |
0.046 |
SSDD-002 |
363 |
364 |
1 |
0.008 |
<0.005 |
<1 |
0.016 |
SSDD-002 |
364 |
365 |
1 |
0.018 |
0.015 |
<1 |
0.043 |
SSDD-002 |
365 |
366 |
1 |
0.006 |
<0.005 |
<1 |
0.006 |
SSDD-002 |
366 |
367 |
1 |
0.037 |
0.029 |
1 |
0.013 |
SSDD-002 |
367 |
368 |
1 |
0.009 |
0.012 |
1 |
0.019 |
SSDD-002 |
368 |
369 |
1 |
0.006 |
0.039 |
1 |
0.11 |
SSDD-002 |
369 |
370 |
1 |
0.009 |
0.006 |
<1 |
0.02 |
SSDD-002 |
370 |
372 |
2 |
<0.005 |
<0.005 |
<1 |
0.005 |
SSDD-002 |
372 |
373.3 |
1.3 |
0.01 |
<0.005 |
<1 |
0.008 |
SSDD-002 |
373.3 |
374.7 |
1.4 |
0.009 |
<0.005 |
<1 |
0.011 |
APPENDIX 2: JORC TABLES
Section 1 Sampling Techniques and Data |
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(Criteria in this section apply to all succeeding sections.)
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Criteria |
JORC Code explanation |
Commentary |
Sampling techniques |
Nature and quality of sampling (eg 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. |
Drill core samples were collected from half cut PQ and HQ diametre core, where the core was sawn exactly in half along a pre-defined cutting line. Sample intervals were determined by the geologist and samples were placed into labelled and tagged sample bags prior to dispatch. A sample tag was also placed in the core box. A specific gravity sample was taken at 10 metre intervals, or at each change in lithology, using whole core prior to cutting and sampling for analysis. Specific gravity was measured using the Archimedes principle.
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Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used. |
For drill hole analyses, sample intervals were selected by the logging geologists based on geological criteria including presence of alteration and mineralisation, style of mineralisation and lithological contacts. Minimum sample lengths of 0.5 metres and maximum sample lengths of 2 metres were employed. Each sample weighed between 2 and 13 kg depending on the length of the sample and diametre of drill core. On silver-lead-zinc vein targets, sampling was only conducted on visually mineralised intervals, including 10 metres either side of the visually mineralised interval. On copper-gold porphyry targets, the entire hole was sampled.
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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 (eg '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 (eg submarine nodules) may warrant disclosure of detailed information. |
For drill hole analyses, diamond drilling was used to obtain 2 to 13kg samples, prepared at ALS Bor, Serbia. The sample pulps were sent to ALS Rosia Montana, Romania by air freight for gold analysis by 30 gram fire assay with AA finish (code FA-AA23), and multi-element analyses were conducted by ALS Loughrea, Ireland using a highly oxidising digestion with ICP-MS finish (code ME-ICPORE).
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Drilling techniques |
Drill type (eg core, reverse circulation, open-hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (eg core diametre, 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). |
All holes were drilled by coring producing PQ and HQ diametre core and recovered using triple tube. Downhole surveys were recorded by the drillers every 30m downhole and at the end of each hole using a Reflex EZ-trac tool. |
Drill sample recovery |
Method of recording and assessing core and chip sample recoveries and results assessed. |
All core was geotechnically logged to verify drillers blocks, record the run length, recovered length, core recovery (%), RQD and fracture index. Core recovery was maximised through drilling shorter drill runs in friable zones and zones of water loss. There is no observed relationship between sample recovery and grade.
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Measures taken to maximise sample recovery and ensure representative nature of the samples. |
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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. |
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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. |
Core samples were geologically logged to a level of detail that would support appropriate Mineral Resource estimation, mining and metallurgical studies. Basic geotechnical logging (RQD, fracture index, core recovery) was recorded and is sufficient for Mineral Resource estimation. Additional geotechnical logging would be required for mining studies. Core logging is qualitative and all core is photographed. All of the core (100%) is logged.
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Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc) photography. |
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The total length and percentage of the relevant intersections logged. |
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Sub-sampling techniques and sample preparation |
If core, whether cut or sawn and whether quarter, half or all core taken. |
Core samples were sawn exactly in half.
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If non-core, whether riffled, tube sampled, rotary split, etc and whether sampled wet or dry. |
Not applicable, as all samples are core. |
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For all sample types, the nature, quality and appropriateness of the sample preparation technique. |
Collection of around 2-13kg 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.
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Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples. |
Industry best practice was adopted by ALS for laboratory sub-sampling and the avoidance of any cross contamination. Tethyan inserted blind blanks at a rate of one per batch of 20 samples, typically sequentially following a mineralised sample.
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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. |
At Kizevak, two composite samples were collected from mineralised quarter cut core, and were prepared and analysed at MMI Bor. Comparison between the exploration assays and the MMI Bor and Tethyan results demonstrate that sampling is representative of the in-situ material collected. Tethyan routinely assay pulp duplicates which show excellent repeatability (R=>0.9). Tethyan also collect half core duplicate samples in every third batch. |
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Whether sample sizes are appropriate to the grain size of the material being sampled. |
Sample size of 2-13 kg is appropriate to the grain size of the material being tested.
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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. |
The sample pulps were sent to ALS Rosia Montana, Romania by air freight for gold analysis by 30-gram fire assay with AA finish (code FA-AA23). Multi-element analyses were conducted by ALS Loughrea, Ireland using a highly oxidising digestion with ICP-MS finish (code ME-ICPORE). All techniques were appropriate for the elements being determined. Samples are considered a partial digestion when using an aqua regia digest.
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For geophysical tools, spectrometres, handheld XRF instruments, etc, the parametres 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. |
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Nature of quality control procedures adopted (eg standards, blanks, duplicates, external laboratory checks) and whether acceptable levels of accuracy (ie lack of bias) and precision have been established. |
Quality Control is monitored through the insertion of one certified reference material (CRM) sample and one blank sample per batch of 20 samples. One pulp duplicate sample is also inserted per batch. The QC results are monitored in real-time, and any failed batches are re-assayed prior to inclusion in the final drill database. Failed batches are determined if a blank sample assays three times the lower detection limit of the element of interest, or if a CRM assays greater than +/-3 standard deviations from the mean, or if two consecutive CRMs assay +/_ 2 standard deviations from the mean. It is considered that acceptable levels of accuracy and precision have been achieved.
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Verification of sampling and assaying |
The verification of significant intersections by either independent or alternative company personnel. |
There has been no independent logging of significant intersections. Tethyan core was logged by geological staff and verified by the Exploration Manager. Tethyan's drilling has verified the position of historical mineralised intercepts although broader, lower grade intervals are observed relative to historic results. No historical core remains.
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The use of twinned holes. |
None of the reported holes are twin holes. |
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Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. |
Primary logging, survey and geotechnical data was entered by the logging geologist into excel sheets per drill hole, and verified and merged with a master acQuire database by the data manager. Data verification includes visual verification by the Database Manager, checking of detailed geological logs against core observations, core photographs and analytical results by the Exploration Manager, and automated data verification using industry standard software. Data is stored on the Virtual Cloud and is regularly backed-up.
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Discuss any adjustment to assay data. |
No adjustments were necessary. |
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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. |
Drill collars were surveyed using Total Station to better than 0.05m accuracy. Downhole surveys were related back to the surveyed collar.
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Specification of the grid system used. |
UTM WGS Zone 34, Northern Hemisphere
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Quality and adequacy of topographic control. |
Topography is derived from public 1:25,000 scale mapping. It is considered sufficiently accurate for the Company's current exploration activities. |
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Data spacing and distribution |
Data spacing for reporting of Exploration Results. |
Drill hole spacing is between 30 and 80 metres and is considered acceptable for reporting of exploration results.
The data spacing and distribution is sufficient for this first-stage metallurgical test work, with the 2 test samples representing the currently recognised main mineralisation styles. .
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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. |
Not applicable as no Mineral Resource or Ore Reserve estimation has been completed.
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Whether sample compositing has been applied. |
Sample compositing was not applied for the drill hole reporting.
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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. |
Holes were drilled at a high angle to mineralised structures. The true thickness of mineralised zones is estimated to vary between 70 to 95% of apparent width. |
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. |
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Sample security |
The measures taken to ensure sample security. |
Chain of Custody of digital data is managed by the Company. Core samples were stored on site in a locked facility and dispatched to the laboratory using a laboratory courier, at which point the laboratory assumed custody of the samples. Samples were examined and photographed on receipt by the laboratory. All sample collection was controlled by digital sample control file(s) and hard-copy ticket books.
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Audits or reviews |
The results of any audits or reviews of sampling techniques and data. |
There have been no audits or reviews of sampling techniques and data. |
Section 2: Reporting of Exploration Results |
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(Criteria listed in the preceding section also apply to this section)
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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. |
Adriatic Metal's subsidiary, Tethyan Resource Corp has rights to exploration on four contiguous exploration licences in southwest Serbia, located 250km from Belgrade and collectively referred to as the "Raska District". Drill holes KZDD-015 to KZDD-020 which are the subject of this press release are located on exploration licence 2345 "Kizevak". Licence 2345 "Kizevak" and 2346 "Sastavci" Exploration licences 2345 "Kizevak" and 2346 "Sastavci" are owned 100% by EFPP d.o.o., a private Serbian company. Licence 2345 covers an area of 1.8km2 and licence 2346 covers an area of 1.4km2. On 01 April 2020, Tethyan Resource Corp announced that it had entered into an arms-length agreement to purchase 100% of EFPP d.o.o. on 31 January 2020. The First Closing initially consists of a cash payment of €525,000 to acquire 10% of EFPP d.o.o. At any time within 12 months of First Closing, Tethyan Resource Corp may elect to acquire the remaining 90% of shares of EFPP d.o.o. on the Second Closing by: · Paying €1,375,000 to EFPP d.o.o.; · Granting to the Sellers a 2% Net Smelter Return over the Licences; · Issuing a total of 4 million ordinary shares of Adriatic, to be issued in four equal tranches of 1 million shares, with the first tranche issued on the Second Closing and each additional tranche issued each six months thereafter; and · Paying a deferred cash payment of €500,000 on the two-year anniversary of First Closing. There are no known native title interests, historical sites, wilderness or national park or environmental settings within the above licence holding. Royalties A non-negotiable 5% Net Smelter Return is payable to the Serbian government for metallic raw materials.
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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. |
Licence 2345 "Kizevak" and 2346 "Sastavci" are both in good standing and are in the first of a three-year exploration period. Both licences expire on 16.10.2022 and may be extended on application for a further six years prior to submission of an application for an Exploitation Licence. There are no known impediments to obtaining a licence to operate in the area.
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Exploration done by other parties |
Acknowledgment and appraisal of exploration by other parties. |
The Raska District has an extended exploration history, summarised below: · 1929-1932: Selection Trust Ltd conducted prospecting and developed underground drives for exploration sampling at Kizevak. · 1957-1958: Rudnik Bel Brdo company completed five drill holes at Kizevak, total metreage not known. · 1960-1964: Geozavod (Yugoslav state) completed 1:100,000 scale mapping and scout drilling (details not known). · 1973-2005: The Geoinstitut (Yugoslav state company) explored the Kizevak, Sastavci and Karadak prospects. At Kizevak, Geoinstitut completed 172 core drill holes totalling 26,727 metres and 29 adits with cross drifts for exploration sampling totalling 7,820m. Open pit mining occurred between 1986 and 2000 and produced 2Mt. At Sastavci, 30 drill holes (7113m) and three adits with cross drives (2626m) were completed leading to small scale open pit mining totalling 40kt of production in 1986. Six core holes (1068m) and 804m of adits and cross drives were completed at Karadak but no mining took place. A foreign resource estimate was reported in 1994 by the Geoinstitut as a combined estimate for the Kizevak, Sastavci and Karadak prospects in the A+B+C1+C2 categories in accordance with Yugoslav GKZ reporting requirements, for 8Mt at 45 g/t silver, 5.06 % zinc and 2.96 % lead. i. "Report on exploration for lead and zinc at the Kizevak-Karadak area in 1994" dated 1995 and authored by Mr B. Rudulovi ć (Izveštaj o istraživanju olova i cinka u podru č ju Ki ž evak - Karadak u 1994. godini). ii. Yugoslav GKZ mineral resource estimates were always stated as "reserves" and classified according to the A+B+C1+C2 or "alphabetical" classification, which was derived from the Russian system and is still applied throughout many countries in southeast Europe. The reserves had to be approved by the official Commission for Ore Reserves. The A, B, C1 and C2 categories reflect the levels of confidence in the actual tonnage exploited from a reserve, with confidence levels being - 95%, 80%, 70% and 35% respectively. Henley (2004) and others have evaluated the alphabetical classification system with respect to the compliant codes in Canada and Australia, and concluded that A+B is comparable to "measured", C1 to "indicated" and C2 to "inferred" in internationally acceptable codes for reporting resources. However, these comparisons are only an approximation, and cannot be considered as equivalents. iii. The Company is not treating the foreign estimate as current mineral resources or reserves and considers the foreign estimate to represent an exploration project that requires verification. iv. The foreign estimate is considered to be a useful guide to exploration but the company is not treating the foreign estimate as current mineral resources or ore reserves as defined by the JORC Code. The Company has reviewed and digitised original hard copy drill data, geology logs and assay data, but has not had access to drill core or core photographs; descriptions of sampling, sample preparation or analytical methodology; quality control data; core recovery data; downhole or collar survey data; or sample security information. v. The foreign estimate was based on the results of core drilling and underground sampling completed by the Geoinstitut between 1973-1994. It was estimated using the polygonal method assuming an open pit mining scenario and prevailing metal prices at the time. vi. No more recent estimates or data relevant to the foreign estimate are available to the Company except for the results of KSEDD001 to KSEDD014 drilled by Tethyan Resources during 2018-2019. vii. To verify the foreign estimate as mineral resources in accordance with Appendix 5A (JORC Code) the Company intends to perform geological mapping, geophysical surveys and core drilling. An initial 3000m of core drilling is planned to verify the presence and grade of mineralisation, and the results will be used to plan additional exploration programs to facilitate future mineral resource estimation in accordance with the JORC Code, if warranted. viii. The exploration work is proposed over a 12 month period commencing on the First Closing and enduring to the Second Closing, at which point the Company will elect whether or not to proceed with the option agreement with EFPP. The Company intends to fund this work using current cash resources. ix. The foreign estimate is not reported in accordance with the JORC Code. A competent person has not done sufficient work to classify the foreign estimate as mineral resources or ore reserves in accordance with the JORC Code. It is uncertain that following evaluation and/or further exploration that the foreign estimate will be able to be reported as mineral resources or ore reserves in accordance with the JORC Code. · 2005-2008: no work known to have occurred at the Kizevak-Sastavci prospects. · 2004-2007: Phelps Dodge explored the Rudnica copper-gold porphyry including seven core holes for at least 1310 m. · 2007-2009: Euromax drilled one hole at the Rudnica copper-gold porphyry · 2009-2015: Farmakom d.o.o. a private Serbian company explored the Kizevak, Sastavci and Rudnica prospects licences. Work completed not known. · 2016-2018: Licence 2176 "Kremice" was granted to Taor do.o.., a private Serbian company, who completed a desk-based remote sensing study prior to being acquired by Tethyan Resource Corp on 03.07.2018. · 2016: Licence 2150 "Raska" was granted to Deep Research d.o.o. · 2019: Licence 2345 "Kizevak" and 2346 "Sastavci" were granted to EFPP d.o.o.
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Geology |
Deposit type, geological setting and style of mineralisation. |
Mineralisation in the Raska District is hosted in andesite volcanics and volcaniclastics, intruded by coeval diorite dykes and post-mineral diorite and quartz latite dykes. The volcanic sequence unconformably overlies a serpentinised ophiolitic melange. A massive, grey to red limestone unit is juxtaposed against the andesite package to the south of the Kizevak prospect. The Kizevak, Sastavci and Karadak deposits are intermediate sulphidation, polymetallic (Ag-Pb-Zn) epithermal vein arrays hosted in an extensional fault setting. Kizevak occurs over a total strike length of >1.3km. Approximately 200m of the known strike length is within exploration licence 2176 "Kremice" which is the southeast extension of the past producing Kizevak open pit mine. Sastavci mineralisation has been defined by historical drilling over a strike length of 1.2km within a 250m wide zone, which contains several sub-parallel veins and lenses. Karadak has been defined by historical drilling over a strike length of 400m within one to four sub-parallel veins. Mineralisation comprises <1 to >5m thick, massive to semi-massive sulphide veins with broad (10-40m thick) zones of crackle breccia and stockwork veins in the hanging walls. All veins are composed of galena-sphalerite-pyrite-bournonite-chalcopyrite-tetrahedrite with intergrowths of Pb-As sulfosalts and quartz-carbonate (rhodochrosite) gangue. The veins are occasionally milled and brecciated as a result of fault reactivation, which forms clay rich, unconsolidated mineralised zones. Mineralisation is associated with an intense pyrite-clay (illite-smectite), magnetite destructive alteration. The Rudnica and Kremice Porphyry prospects are copper-gold porphyry deposits which display stockwork A, B and C-type veins composed of variable quartz, pyrite, chalcopyrite and magnetite. Stockwork veins are dominantly hosted within an early diorite porphyry intrusion (P10), an intermediate diorite dyke (P20) and country rocks (serpentinite and andesite). A late diorite dyke (P30) crosscuts mineralisation. At Rudnica, a 50 to 80m thick, gold-mineralised, copper-poor, leached and oxidised cap overlies a 10-50 m thick supergene copper enrichment zone (chalcocite blanket), which overprints the deeper hypogene mineralisation. Mineralisation has been defined over 400 by 250 m, to a depth of 550m below surface, and is open in most directions. At Kremice, mapping has defined an area of 450 by 450m with stockwork A and B type quartz-pyrite ± magnetite veins within a 1200 by 600 m soil anomaly.
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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. |
Drilling data for the reported drill holes is included in Tables 1-3 of Appendix 1 in this document. |
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. |
Significant intercepts were truncated by applying a lower cut-off grade of 1% Pb+Zn (see below assumptions for ZnEq calculation) and maximum internal dilution of 5m. No top-cutting was applied. Significant intercepts were reported as weighted averages. |
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. |
Short lengths of high-grade results were defined as >5% Pb+Zn and maximum internal dilution of 5m. Results are shown in Table 1 of the main reporting document. |
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The assumptions used for any reporting of metal equivalent values should be clearly stated. |
ZnEq grades are based on the following metal prices: $1850/oz gold, $22/oz silver, $1900/t lead, $2350/t zinc, and the following metal recoveries were used on the basis of preliminary testing inclusive of smelter charges and payabilities: 75% silver, 85% lead and 85 % zinc. Gold recovery of 80% was estimated as there have been no gold recovery tests conducted to date. The zinc equivalent calculation is as follows: ZnEq = 100*(((Au grade g/t *Au recovery %*Au price $/g)+((Ag grade g/t *Ag recovery %)*Ag price $/g)+((Pb grade % *Pb recovery %)*Pb price ($/t)/100)+((Zn grade % *Zn recovery %)*Zn price ($/t)/100))/Zn price ($/t). |
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Relationship between mineralisation widths and intercept lengths |
These relationships are particularly important in the reporting of Exploration Results.
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported.
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'). |
Only downhole lengths are reported, true widths are not known. True widths are estimated as between 75 and 90% of the apparent width. |
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. Metallurgical test work results being reported do not require maps and diagrams. |
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. |
All assay tables for all reported holes are included in the main reporting document. |
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 announcement or in this table have been used.
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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 will be undertaken for exploration along strike and down dip, the nature of which is dependent on exploration success and funding. Further drilling will be undertaken for geotechnical and metallurgical purposes, to include locked cycle tests, bulk samples and variability testing |
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 announcement. |