SOVEREIGN METALS LIMITED
NEWS RELEASE | 15 MARCH 2022
Spectacular Rutile Drill Results See Mineralised Footprint Increase By 28%
· |
Latest drill results increase the drill-defined rutile mineralised envelope by 28% to 165km2 |
· |
Kasiya and Nsaru deposits have now coalesced into the Kasiya-Nsaru rutile deposit - a single, very large, coherent, high-grade body of near surface rutile and graphite mineralisation |
· |
New drilling has encountered the highest-grade rutile results to date at Nsaru and at a new extension east of Kasiya. Highlights include: |
· |
11m @ 1.34% inc. 2m @ 3.00% rutile |
· |
12m @ 1.27% inc. 3m @ 2.16% rutile |
· |
8m @ 1.36% inc. 2m @ 2.66% rutile |
· |
7m @ 1.84% inc. 4m @ 2.71% rutile |
· |
12m @ 1.46% inc. 4m @ 2.42% rutile |
· |
13m @ 1.48% inc. 5m @ 2.23% rutile |
· |
Discovery of numerous extensions and new blocks of mineralisation expected to add substantially to upcoming Mineral Resource Estimate update |
· |
Results affirm the strategic and global significance of Kasiya as the largest undeveloped natural rutile project in the world and first major rutile discovery in over half a century |
· |
Updated Scoping Study underway focused on incorporating the growing resource base |
Sovereign Metals Limited (ASX:SVM; AIM:SVML) (Sovereign or the Company) is pleased to report results from its H2 2021 drilling program at Kasiya-Nsaru, the Company's flagship, very large, high-grade rutile deposit in Malawi.
The results, including numerous spectacular intercepts, will underpin the pending Mineral Resource Estimate (MRE) upgrade which is expected to significantly increase in both the Indicated and Inferred categories.
The most recent core and auger drilling has now expanded the total mineralised envelope to 165km2, up 28%. The previous MRE included just 49km2 of the mineralised envelope, hence significant resource tonnage growth can be expected.
Sovereign's Managing Director Dr Julian Stephens commented : "The results of the latest drilling program have surpassed all of our expectations. Not only did we encounter the highest rutile grades to date, but the coalescing of the Kasiya and Nsaru deposits supports our belief that we have the single largest rutile deposit in the world on our hands. We are looking forward to announcing the updated Mineral Resource Estimate in the coming weeks."
ENQUIRIES
Dr Julian Stephens (Perth) +61(8) 9322 6322 |
Sam Cordin (Perth) |
Sapan Ghai (London)
|
Nominated Adviser on AIM |
|
RFC Ambrian |
|
Bhavesh Patel / Andrew Thomson |
+44 20 3440 6800 |
|
|
Joint Brokers |
|
Berenberg |
+44 20 3207 7800 |
Matthew Armitt |
|
Jennifer Lee |
|
Varun Talwar |
|
|
|
Optiva Securities |
+44 20 3137 1902 |
Daniel Ingrams |
|
Mariela Jaho |
|
Christian Dennis |
|
KASIYA-NSARU
Sovereign now has a total of ~165km2 of drilled, high-grade rutile mineralisation with the latest results succeeding in joining Kasiya and Nsaru into a single deposit.
Rutile mineralisation lies in laterally extensive, near surface, flat "blanket" style bodies in areas where the weathering profile is preserved and not significantly eroded. The Kasiya-Nsaru deposit is expansive with high-grade mineralisation commonly grading 1.2% to 2.0% rutile in the top 3-5m from surface. Moderate grade mineralisation generally grading 0.5% to 1.2% rutile commonly extends from 5m to end of hole where it remains open at depths >10m in numerous areas.
Kasiya-Nsaru is a strategic and globally significant natural rutile deposit with substantial additional resource growth expected. Kasiya's current Mineral Resource Estimate is 605Mt at 0.98% rutile (0.7% cut-off, Indicated + Inferred, Table 1).
The core and auger drilling program at the Kasiya-Nsaru rutile deposit was completed from July to September 2021. This very large and expansive drilling program targeted significant MRE expansion as well as infill core drilling designed to bring known high-grade areas into the Indicated resource category. A total of 712 drill-holes for 6,832m are reported. Of these, 96 were core holes for 999m, and 616 are hand-auger holes for 5,833m.
SPECTACULAR RESULTS
Results from significant new extensions including the eastern portion of Kasiya as per below, with full results listed in Table 2:
· 11m @ 1.34% inc. 2m @ 3.00% rutile · 8m @ 1.36% inc. 2m @ 2.66% rutile · 12m @ 1.46% inc. 3m @ 2.42% rutile |
· 12m @ 1.27% inc. 3m @ 2.16% rutile · 12m @ 1.26% inc. 5m @ 1.67% rutile · 12m @ 1.34% inc. 5m @ 1.65% rutile |
Results from 400m x 400m core and auger resource drilling at the large and high-grade Nsaru deposit including those listed below, with full results listed in Table 2:
· 7m @ 1.84% inc. 4m @ 2.71% rutile · 12m @ 1.44% inc. 3m @ 2.47% rutile · 10m @ 1.28% inc. 2m @ 2.36% rutile · 13m @ 1.48% inc. 5m @ 2.23% rutile · 10m @ 1.49% inc. 4m @ 2.01% rutile · 10m @ 1.44% inc. 4m @ 2.01% rutile |
· 13m @ 1.29% inc. 4m @ 1.94% rutile · 12m @ 1.35% inc. 4m @ 1.90% rutile · 12m @ 1.38% inc. 6m @ 1.83% rutile · 13m @ 1.35% inc. 4m @ 1.81% rutile · 11m @ 1.35% inc. 4m @ 1.74% rutile · 9m @ 1.35% inc. 4m @ 1.71% rutile |
DRILLING RESULTS
The Kasiya and Nsaru rutile deposits have now coalesced into one very large, coherent, high-grade zone of near surface rutile and graphite mineralisation believed to be the single largest rutile deposit in the world.
The drilled mineralised footprint has now grown to 165km2, an increase overall of 28% from previously. Importantly, the drilling has also substantially increased the area of mineralisation drilled at 400 x 400m or greater density and thus it is expected that substantial tonnages will be able to be added in the upcoming MRE, due to be reported in the coming weeks. For reference, the previous MRE covered just 49km2 of the mineralised footprint.
Numerous new areas have also received drilling at 400 x 400m or greater density and are expected to be able to be incorporated into the upcoming the MRE upgrade.
In many of the high-grade zones identified by drilling rutile mineralisation persists and remains open at depth, at the limit of the current drilling. It is therefore considered likely that rutile mineralisation should occur down to approximately the base of the saprolite zone, which is estimated to lie at about 25m vertical depth. These deeper zones represent the key targets for the planned 2022 air-core drilling program.
Coarse flake graphite is present in all holes in broad association with rutile mineralisation. Graphite grades average about 1% TGC through the mineralised area.
CONCLUSION
The significant 2021 H2 drilling program at Kasiya and Nsaru accomplished the following;
· Achieved a substantial 28% increase in the overall mineralised envelope to 165km2
· Brought a significant portion of the mineralised envelope to 400 x 400m drill spacing or greater density in order to be considered for the upcoming MRE update
· Identified numerous new areas of high-grade rutile mineralisation not previously known or not previously included in the prior MRE
The updated JORC MRE is due in the coming weeks and will serve as the basis for an updated Scoping Study targeted for completion in Q2 2022. This updated Study will build on the December 2021 Study, with the new MRE likely to allow higher grades to be mined, or increased production rates or increased mine life, or a combination.
Competent Persons Statement
The information in this report that relates to Exploration Results is based on information compiled by Mr Samuel Moyle, a Competent Person who is a member of The Australasian Institute of Mining and Metallurgy (AusIMM). Mr Moyle is the Exploration Manager of Sovereign Metals Limited and a holder of ordinary shares and unlisted options in Sovereign Metals Limited. Mr Moyle has sufficient experience that is relevant to the style of mineralisation and type of deposit under consideration and to the activity being undertaken, to qualify as a Competent Person as defined in the 2012 Edition of the 'Australasian Code for Reporting of Exploration Results, Mineral Resources and Ore Reserves'. Mr Moyle consents to the inclusion in the report of the matters based on his information in the form and context in which it appears.
The information in this announcement that relates to Sovereign's Mineral Resource Estimate is extracted from the ASX announcement dated 16 December 2021 which is available to view at Sovereign's website at www.sovereignmetals.com.au. Sovereign confirms that a) it is not aware of any new information or data that materially affects the information included in the ASX announcement; b) all material assumptions included in the ASX announcement continue to apply and have not materially changed; and c) the form and context in which the relevant Competent Persons' findings are presented in this report have not been materially changed from the ASX announcement.
Table 1: Kasiya Mineral Resource Estimate at 0.7% Rutile Cut-off |
|||||
Mineral Resource Category |
Material Tonnes (millions) |
Rutile (%) |
Rutile Tonnes (millions) |
TGC (%) |
TGC Tonnes (millions) |
Indicated |
304 |
1.02 |
3.1 |
1.31 |
4.0 |
Inferred |
301 |
0.93 |
2.8 |
1.16 |
3.5 |
Total |
605 |
0.98 |
5.9 |
1.24 |
7.5 |
Cut-off: 0.7% rutile, TGC = total graphitic carbon
Forward Looking Statement
This release may include forward-looking statements, which may be identified by words such as "expects", "anticipates", "believes", "projects", "plans", and similar expressions. These forward-looking statements are based on Sovereign's expectations and beliefs concerning future events. Forward looking statements are necessarily subject to risks, uncertainties and other factors, many of which are outside the control of Sovereign, which could cause actual results to differ materially from such statements. There can be no assurance that forward-looking statements will prove to be correct. Sovereign makes no undertaking to subsequently update or revise the forward-looking statements made in this release, to reflect the circumstances or events after the date of that release.
To view this announcement in full, including all illustrations and figures, please refer to www.sovereignmetals.com.au .
Appendix I - DRILL RESULTS
Rutile and graphite drilling results from Kasiya and Nsaru are shown below in Table 2.
Hole ID |
Interval Thickness |
Rutile % |
TGC % |
From (m) Downhole |
Hole Type |
KYHA0537 |
12.0 |
1.05 |
1.87 |
0.0 |
HA |
incl |
4.0 |
1.44 |
|
0.0 |
HA |
KYHA0538 |
7.0 |
0.91 |
0.14 |
0.0 |
HA |
incl |
4.0 |
1.18 |
|
0.0 |
HA |
KYHA0541 |
6.0 |
0.59 |
2.40 |
0.0 |
HA |
KYHA0543 |
4.0 |
0.69 |
NSR |
0.0 |
HA |
KYHA0544 |
4.0 |
0.55 |
0.30 |
0.0 |
HA |
KYHA0547 |
7.0 |
1.04 |
0.56 |
0.0 |
HA |
incl |
3.0 |
1.49 |
|
0.0 |
HA |
KYHA0548 |
4.0 |
1.25 |
NSR |
0.0 |
HA |
KYHA0549 |
4.0 |
0.60 |
0.40 |
0.0 |
HA |
KYHA0550 |
4.0 |
1.42 |
0.05 |
0.0 |
HA |
incl |
2.0 |
2.11 |
|
0.0 |
HA |
KYHA0552 |
6.0 |
1.29 |
NSR |
0.0 |
HA |
incl |
2.0 |
2.20 |
|
0.0 |
HA |
KYHA0553 |
10.0 |
0.85 |
0.18 |
0.0 |
HA |
incl |
2.0 |
1.35 |
|
0.0 |
HA |
KYHA0554 |
6.0 |
1.04 |
NSR |
0.0 |
HA |
incl |
3.0 |
1.36 |
|
0.0 |
HA |
KYHA0555 |
8.0 |
1.20 |
0.93 |
0.0 |
HA |
incl |
3.0 |
1.81 |
|
0.0 |
HA |
KYHA0556 |
|
NSR |
|
|
HA |
KYHA0557 |
11.0 |
0.86 |
1.93 |
0.0 |
HA |
incl |
3.0 |
1.26 |
|
0.0 |
HA |
KYHA0558 |
12.0 |
0.77 |
1.95 |
0.0 |
HA |
KYHA0559 |
2.0 |
0.61 |
0.30 |
0.0 |
HA |
KYHA0560 |
2.0 |
1.52 |
0.80 |
0.0 |
HA |
KYHA0561 |
12.0 |
1.09 |
1.23 |
0.0 |
HA |
incl |
2.0 |
1.31 |
|
0.0 |
HA |
KYHA0562 |
8.0 |
1.00 |
0.14 |
0.0 |
HA |
incl |
3.0 |
1.22 |
|
0.0 |
HA |
KYHA0563 |
|
NSR |
|
|
HA |
KYHA0564 |
|
NSR |
|
|
HA |
KYHA0565 |
3.0 |
1.64 |
0.40 |
0.0 |
HA |
KYHA0566 |
4.0 |
0.87 |
0.30 |
0.0 |
HA |
KYHA0567 |
11.0 |
0.96 |
2.54 |
0.0 |
HA |
incl |
4.0 |
1.09 |
|
2.0 |
HA |
KYHA0568 |
12.0 |
1.06 |
2.44 |
0.0 |
HA |
incl |
3.0 |
1.57 |
|
0.0 |
HA |
KYHA0569 |
6.0 |
1.29 |
0.10 |
0.0 |
HA |
incl |
3.0 |
1.72 |
|
0.0 |
HA |
KYHA0570 |
8.0 |
0.99 |
2.36 |
0.0 |
HA |
incl |
5.0 |
1.22 |
|
0.0 |
HA |
KYHA0572 |
3.0 |
0.62 |
0.20 |
0.0 |
HA |
KYHA0573 |
9.0 |
0.93 |
3.17 |
0.0 |
HA |
incl |
2.0 |
1.07 |
|
0.0 |
HA |
KYHA0576 |
3.0 |
0.94 |
0.40 |
0.0 |
HA |
KYHA0576 |
2.0 |
0.81 |
0.30 |
7.0 |
HA |
KYHA0577 |
2.0 |
1.11 |
1.10 |
0.0 |
HA |
KYHA0583 |
2.0 |
0.76 |
0.30 |
0.0 |
HA |
KYHA0584 |
10.0 |
1.18 |
0.69 |
0.0 |
HA |
incl |
4.0 |
1.83 |
|
0.0 |
HA |
KYHA0585 |
2.0 |
1.94 |
0.30 |
0.0 |
HA |
KYHA0586 |
12.0 |
1.03 |
0.67 |
0.0 |
HA |
incl |
4.0 |
1.35 |
|
0.0 |
HA |
KYHA0587 |
6.0 |
1.35 |
0.20 |
0.0 |
HA |
incl |
4.0 |
1.73 |
|
0.0 |
HA |
KYHA0588 |
4.0 |
0.86 |
0.33 |
0.0 |
HA |
KYHA0589 |
1.7 |
1.18 |
0.10 |
0.0 |
HA |
KYHA0590 |
1.5 |
1.60 |
0.10 |
0.0 |
HA |
KYHA0591 |
11.0 |
1.06 |
1.34 |
0.0 |
HA |
incl |
3.0 |
1.42 |
|
0.0 |
HA |
KYHA0592 |
7.0 |
0.85 |
0.34 |
0.0 |
HA |
incl |
4.0 |
1.09 |
|
0.0 |
HA |
KYHA0593 |
|
NSR |
|
|
HA |
KYHA0594 |
11.0 |
0.61 |
3.05 |
0.0 |
HA |
KYHA0595 |
5.0 |
0.74 |
0.40 |
0.0 |
HA |
KYHA0596 |
|
NSR |
|
|
HA |
KYHA0597 |
3.0 |
0.53 |
0.10 |
0.0 |
HA |
KYHA0598 |
|
NSR |
|
|
HA |
KYHA0599 |
|
NSR |
|
|
HA |
KYHA0600 |
8.0 |
0.80 |
1.24 |
0.0 |
HA |
KYHA0601 |
1.0 |
0.59 |
0.50 |
3.0 |
HA |
KYHA0602 |
3.0 |
0.76 |
0.40 |
0.0 |
HA |
KYHA0603 |
3.0 |
0.83 |
0.50 |
0.0 |
HA |
KYHA0604 |
3.0 |
0.69 |
NSR |
0.0 |
HA |
KYHA0605 |
|
NSR |
|
|
HA |
KYHA0606 |
6.0 |
0.65 |
1.07 |
0.0 |
HA |
KYHA0607 |
2.0 |
0.55 |
0.10 |
0.0 |
HA |
KYHA0608 |
4.0 |
1.39 |
0.20 |
0.0 |
HA |
incl |
2.0 |
1.96 |
|
0.0 |
HA |
KYHA0609 |
12.0 |
1.19 |
0.98 |
0.0 |
HA |
incl |
2.0 |
2.40 |
|
0.0 |
HA |
KYHA0610 |
4.0 |
0.56 |
0.30 |
0.0 |
HA |
KYHA0611 |
2.0 |
1.01 |
0.50 |
0.0 |
HA |
KYHA0612 |
13.0 |
0.79 |
1.68 |
0.0 |
HA |
KYHA0613 |
13.0 |
1.10 |
1.90 |
0.0 |
HA |
incl |
3.0 |
1.57 |
|
0.0 |
HA |
KYHA0614 |
9.0 |
0.92 |
0.87 |
0.0 |
HA |
incl |
3.0 |
1.33 |
|
0.0 |
HA |
KYHA0615 |
8.0 |
0.81 |
4.20 |
0.0 |
HA |
KYHA0616 |
7.0 |
1.07 |
1.34 |
0.0 |
HA |
incl |
2.0 |
1.71 |
|
0.0 |
HA |
KYHA0617 |
7.0 |
1.04 |
1.09 |
0.0 |
HA |
incl |
4.0 |
1.22 |
|
0.0 |
HA |
KYHA0618 |
5.0 |
1.13 |
0.24 |
0.0 |
HA |
incl |
2.0 |
1.91 |
|
0.0 |
HA |
KYHA0619 |
2.0 |
1.06 |
1.10 |
0.0 |
HA |
KYHA0620 |
8.0 |
1.00 |
1.56 |
0.0 |
HA |
incl |
5.0 |
1.06 |
|
0.0 |
HA |
KYHA0621 |
|
NSR |
|
|
HA |
KYHA0622 |
5.0 |
0.50 |
0.20 |
0.0 |
HA |
KYHA0623 |
12.0 |
1.19 |
5.78 |
0.0 |
HA |
incl |
2.0 |
1.52 |
|
0.0 |
HA |
KYHA0624 |
8.0 |
0.78 |
0.40 |
0.0 |
HA |
incl |
4.0 |
1.02 |
|
0.0 |
HA |
KYHA0625 |
12.0 |
1.07 |
1.87 |
0.0 |
HA |
incl |
4.0 |
1.50 |
|
0.0 |
HA |
KYHA0626 |
12.0 |
0.72 |
1.68 |
0.0 |
HA |
KYHA0627 |
13.0 |
0.85 |
1.98 |
0.0 |
HA |
incl |
2.0 |
1.03 |
|
0.0 |
HA |
KYHA0628 |
12.0 |
1.20 |
3.35 |
0.0 |
HA |
incl |
3.0 |
1.34 |
|
0.0 |
HA |
KYHA0629 |
3.0 |
0.82 |
0.30 |
0.0 |
HA |
KYHA0630 |
13.0 |
0.94 |
2.88 |
0.0 |
HA |
incl |
3.0 |
1.20 |
|
0.0 |
HA |
KYHA0631 |
4.0 |
1.15 |
0.40 |
0.0 |
HA |
KYHA0632 |
12.0 |
0.79 |
1.38 |
0.0 |
HA |
incl |
3.0 |
1.25 |
|
0.0 |
HA |
KYHA0633 |
13.0 |
1.37 |
1.20 |
0.0 |
HA |
incl |
4.0 |
1.59 |
|
0.0 |
HA |
KYHA0634 |
13.0 |
0.85 |
1.66 |
0.0 |
HA |
incl |
3.0 |
1.35 |
|
0.0 |
HA |
KYHA0635 |
6.0 |
0.81 |
0.57 |
0.0 |
HA |
incl |
2.0 |
1.28 |
|
0.0 |
HA |
KYHA0636 |
8.0 |
0.88 |
1.20 |
0.0 |
HA |
incl |
4.0 |
1.14 |
|
0.0 |
HA |
KYHA0637 |
2.0 |
1.38 |
0.50 |
0.0 |
HA |
KYHA0638 |
7.0 |
0.79 |
2.81 |
0.0 |
HA |
incl |
2.0 |
1.33 |
|
0.0 |
HA |
KYHA0639 |
4.0 |
0.79 |
2.80 |
0.0 |
HA |
KYHA0640 |
|
NSR |
|
|
HA |
KYHA0641 |
3.0 |
1.05 |
0.50 |
0.0 |
HA |
KYHA0642 |
5.0 |
1.19 |
1.24 |
0.0 |
HA |
incl |
2.0 |
1.83 |
|
0.0 |
HA |
KYHA0643 |
5.0 |
0.61 |
0.82 |
0.0 |
HA |
KYHA0644 |
3.0 |
0.95 |
0.60 |
0.0 |
HA |
KYHA0645 |
2.0 |
1.03 |
0.30 |
0.0 |
HA |
KYHA0646 |
3.0 |
0.58 |
0.50 |
0.0 |
HA |
KYHA0647 |
3.0 |
0.54 |
0.50 |
0.0 |
HA |
KYHA0648 |
5.0 |
0.78 |
0.38 |
0.0 |
HA |
KYHA0649 |
7.0 |
1.19 |
1.64 |
0.0 |
HA |
incl |
2.0 |
1.80 |
|
0.0 |
HA |
KYHA0650 |
4.0 |
1.02 |
0.50 |
0.0 |
HA |
KYHA0651 |
4.0 |
0.73 |
0.75 |
0.0 |
HA |
KYHA0652 |
2.0 |
0.62 |
0.30 |
0.0 |
HA |
KYHA0653 |
|
NSR |
|
|
HA |
KYHA0654 |
|
NSR |
|
|
HA |
KYHA0655 |
2.0 |
1.18 |
0.30 |
0.0 |
HA |
KYHA0656 |
6.0 |
1.06 |
0.63 |
0.0 |
HA |
incl |
2.0 |
1.51 |
|
0.0 |
HA |
KYHA0657 |
|
NSR |
|
|
HA |
KYHA0658 |
2.0 |
1.43 |
0.60 |
0.0 |
HA |
KYHA0659 |
3.0 |
1.17 |
0.20 |
0.0 |
HA |
KYHA0660 |
2.0 |
1.26 |
0.20 |
0.0 |
HA |
KYHA0661 |
6.0 |
1.10 |
0.53 |
0.0 |
HA |
incl |
2.0 |
2.01 |
|
0.0 |
HA |
KYHA0662 |
8.0 |
0.82 |
0.89 |
0.0 |
HA |
KYHA0663 |
4.0 |
1.39 |
0.20 |
0.0 |
HA |
KYHA0664 |
8.0 |
1.12 |
1.10 |
0.0 |
HA |
incl |
2.0 |
1.86 |
|
0.0 |
HA |
KYHA0665 |
2.0 |
0.91 |
NSR |
0.0 |
HA |
KYHA0666 |
2.0 |
1.71 |
0.30 |
0.0 |
HA |
KYHA0667 |
3.0 |
0.53 |
0.40 |
0.0 |
HA |
KYHA0668 |
2.0 |
0.78 |
0.30 |
0.0 |
HA |
KYHA0669 |
2.0 |
1.46 |
0.30 |
0.0 |
HA |
KYHA0670 |
|
NSR |
|
|
HA |
KYHA0671 |
2.0 |
0.93 |
0.60 |
0.0 |
HA |
KYHA0672 |
6.0 |
0.80 |
0.90 |
0.0 |
HA |
incl |
2.0 |
1.31 |
|
0.0 |
HA |
KYHA0673 |
|
NSR |
|
|
HA |
KYHA0674 |
|
NSR |
|
|
HA |
KYHA0675 |
|
NSR |
|
|
HA |
KYHA0676 |
5.0 |
0.76 |
0.30 |
0.0 |
HA |
KYHA0677 |
2.0 |
0.79 |
0.40 |
0.0 |
HA |
KYHA0678 |
2.0 |
0.60 |
1.70 |
3.0 |
HA |
KYHA0679 |
3.0 |
0.95 |
0.30 |
0.0 |
HA |
KYHA0680 |
|
NSR |
|
|
HA |
KYHA0681 |
3.0 |
0.90 |
0.30 |
0.0 |
HA |
KYHA0682 |
2.0 |
0.93 |
0.30 |
0.0 |
HA |
KYHA0683 |
13.0 |
0.93 |
0.86 |
0.0 |
HA |
incl |
3.0 |
1.78 |
|
0.0 |
HA |
KYHA0684 |
|
NSR |
|
|
HA |
KYHA0685 |
|
NSR |
|
|
HA |
KYHA0686 |
11.0 |
1.17 |
0.83 |
0.0 |
HA |
incl |
7.0 |
1.38 |
|
0.0 |
HA |
KYHA0687 |
8.0 |
1.23 |
2.16 |
0.0 |
HA |
incl |
2.0 |
2.18 |
|
0.0 |
HA |
KYHA0688 |
8.0 |
0.65 |
1.15 |
0.0 |
HA |
KYHA0689 |
11.0 |
0.97 |
1.25 |
0.0 |
HA |
incl |
3.0 |
1.20 |
|
0.0 |
HA |
KYHA0690 |
4.0 |
1.70 |
0.20 |
0.0 |
HA |
KYHA0691 |
2.0 |
1.53 |
0.30 |
0.0 |
HA |
KYHA0692 |
11.0 |
0.72 |
2.88 |
0.0 |
HA |
KYHA0693 |
3.0 |
0.88 |
0.30 |
0.0 |
HA |
KYHA0694 |
2.0 |
0.81 |
0.15 |
0.0 |
HA |
KYHA0695 |
|
NSR |
|
|
HA |
KYHA0696 |
|
NSR |
|
|
HA |
KYHA0697 |
|
NSR |
|
|
HA |
KYHA0698 |
|
NSR |
|
|
HA |
KYHA0699 |
3.0 |
0.77 |
0.20 |
0.0 |
HA |
KYHA0700 |
2.0 |
1.39 |
0.60 |
0.0 |
HA |
KYHA0701 |
3.0 |
1.21 |
0.30 |
0.0 |
HA |
KYHA0702 |
2.0 |
1.52 |
0.30 |
0.0 |
HA |
KYHA0703 |
6.0 |
0.99 |
0.23 |
0.0 |
HA |
incl |
2.0 |
1.56 |
|
0.0 |
HA |
KYHA0704 |
6.0 |
0.70 |
0.13 |
0.0 |
HA |
incl |
2.0 |
1.04 |
|
0.0 |
HA |
KYHA0705 |
3.0 |
1.22 |
NSR |
0.0 |
HA |
KYHA0706 |
6.0 |
0.76 |
0.80 |
0.0 |
HA |
incl |
2.0 |
1.15 |
|
0.0 |
HA |
KYHA0707 |
3.0 |
1.39 |
0.20 |
0.0 |
HA |
KYHA0708 |
2.0 |
1.46 |
0.50 |
0.0 |
HA |
KYHA0709 |
2.0 |
1.62 |
0.30 |
0.0 |
HA |
KYHA0710 |
8.0 |
0.79 |
1.29 |
0.0 |
HA |
incl |
2.0 |
1.36 |
|
0.0 |
HA |
KYHA0711 |
3.0 |
0.59 |
0.30 |
0.0 |
HA |
KYHA0712 |
12.0 |
0.64 |
0.33 |
0.0 |
HA |
KYHA0713 |
7.0 |
0.92 |
0.83 |
0.0 |
HA |
incl |
2.0 |
1.38 |
|
0.0 |
HA |
KYHA0714 |
11.0 |
0.74 |
2.34 |
0.0 |
HA |
KYHA0715 |
2.0 |
1.61 |
0.30 |
0.0 |
HA |
KYHA0716 |
2.0 |
1.58 |
0.20 |
0.0 |
HA |
KYHA0717 |
12.0 |
0.77 |
1.25 |
0.0 |
HA |
KYHA0718 |
12.0 |
0.99 |
1.67 |
0.0 |
HA |
incl |
4.0 |
1.29 |
|
0.0 |
HA |
KYHA0719 |
13.0 |
0.85 |
1.63 |
0.0 |
HA |
incl |
3.0 |
1.13 |
|
0.0 |
HA |
KYHA0720 |
3.0 |
0.66 |
NSR |
0.0 |
HA |
KYHA0721 |
8.0 |
0.91 |
0.30 |
0.0 |
HA |
incl |
4.0 |
1.26 |
|
0.0 |
HA |
KYHA0722 |
9.0 |
1.06 |
1.93 |
0.0 |
HA |
incl |
2.0 |
1.71 |
|
0.0 |
HA |
KYHA0723 |
3.0 |
1.07 |
NSR |
0.0 |
HA |
KYHA0724 |
3.0 |
0.57 |
0.30 |
0.0 |
HA |
KYHA0725 |
2.0 |
0.66 |
0.40 |
0.0 |
HA |
KYHA0726 |
3.0 |
0.74 |
0.30 |
0.0 |
HA |
KYHA0727 |
4.0 |
0.64 |
0.20 |
0.0 |
HA |
KYHA0728 |
4.0 |
0.55 |
0.20 |
0.0 |
HA |
KYHA0729 |
|
NSR |
|
|
HA |
KYHA0730 |
2.0 |
0.73 |
0.20 |
0.0 |
HA |
KYHA0731 |
11.0 |
0.76 |
2.06 |
0.0 |
HA |
incl |
3.0 |
1.04 |
|
0.0 |
HA |
KYHA0732 |
2.5 |
0.81 |
0.40 |
0.0 |
HA |
KYHA0733 |
6.0 |
0.87 |
1.25 |
0.0 |
HA |
KYHA0734 |
5.0 |
0.94 |
0.44 |
0.0 |
HA |
incl |
3.0 |
1.11 |
|
0.0 |
HA |
KYHA0735 |
2.0 |
0.95 |
0.20 |
0.0 |
HA |
KYHA0736 |
4.0 |
0.96 |
0.30 |
0.0 |
HA |
KYHA0737 |
10.0 |
0.88 |
1.29 |
0.0 |
HA |
incl |
3.0 |
1.30 |
|
0.0 |
HA |
KYHA0738 |
11.0 |
0.89 |
2.34 |
0.0 |
HA |
incl |
2.0 |
1.17 |
|
3.0 |
HA |
KYHA0739 |
|
NSR |
|
|
HA |
KYHA0740 |
10.0 |
0.94 |
1.77 |
0.0 |
HA |
incl |
3.0 |
1.02 |
|
0.0 |
HA |
KYHA0741 |
|
NSR |
|
|
HA |
KYHA0742 |
5.0 |
0.71 |
0.30 |
0.0 |
HA |
KYHA0743 |
9.0 |
0.97 |
0.43 |
0.0 |
HA |
incl |
3.0 |
1.53 |
|
0.0 |
HA |
KYHA0744 |
4.0 |
0.68 |
0.20 |
0.0 |
HA |
KYHA0745 |
9.0 |
1.28 |
1.41 |
0.0 |
HA |
incl |
3.0 |
1.63 |
|
0.0 |
HA |
KYHA0746 |
4.0 |
0.93 |
0.45 |
0.0 |
HA |
incl |
3.0 |
1.04 |
|
0.0 |
HA |
KYHA0747 |
5.0 |
0.94 |
1.24 |
0.0 |
HA |
incl |
2.0 |
1.44 |
|
0.0 |
HA |
KYHA0748 |
10.0 |
0.94 |
1.39 |
0.0 |
HA |
incl |
3.0 |
1.42 |
|
0.0 |
HA |
KYHA0749 |
5.0 |
0.63 |
0.24 |
0.0 |
HA |
KYHA0750 |
5.0 |
0.87 |
0.20 |
0.0 |
HA |
KYHA0751 |
|
NSR |
|
|
HA |
KYHA0752 |
12.0 |
0.97 |
1.43 |
0.0 |
HA |
incl |
4.0 |
1.31 |
|
0.0 |
HA |
KYHA0753 |
11.0 |
0.74 |
0.75 |
0.0 |
HA |
incl |
3.0 |
1.06 |
|
0.0 |
HA |
KYHA0754 |
7.0 |
0.61 |
0.61 |
0.0 |
HA |
KYHA0755 |
2.0 |
0.83 |
0.60 |
0.0 |
HA |
KYHA0756 |
6.0 |
1.21 |
1.15 |
0.0 |
HA |
incl |
3.0 |
1.57 |
|
0.0 |
HA |
KYHA0757 |
4.0 |
0.54 |
0.30 |
0.0 |
HA |
KYHA0758 |
11.0 |
1.06 |
2.05 |
0.0 |
HA |
incl |
5.0 |
1.43 |
|
0.0 |
HA |
KYHA0759 |
4.0 |
1.08 |
0.45 |
0.0 |
HA |
incl |
2.0 |
1.44 |
|
0.0 |
HA |
KYHA0760 |
2.0 |
1.18 |
0.50 |
0.0 |
HA |
KYHA0761 |
12.0 |
0.88 |
3.00 |
0.0 |
HA |
KYHA0762 |
6.0 |
0.70 |
0.25 |
0.0 |
HA |
KYHA0763 |
10.0 |
1.07 |
2.40 |
0.0 |
HA |
incl |
2.0 |
1.57 |
|
8.0 |
HA |
KYHA0764 |
|
NSR |
|
|
HA |
KYHA0765 |
|
NSR |
|
|
HA |
KYHA0766 |
3.0 |
1.13 |
0.50 |
0.0 |
HA |
KYHA0767 |
2.0 |
1.43 |
0.30 |
0.0 |
HA |
KYHA0768 |
3.0 |
1.02 |
0.40 |
0.0 |
HA |
KYHA0769 |
3.0 |
0.78 |
0.10 |
0.0 |
HA |
KYHA0770 |
12.0 |
1.12 |
1.16 |
0.0 |
HA |
incl |
3.0 |
1.42 |
|
0.0 |
HA |
KYHA0771 |
6.0 |
0.72 |
0.90 |
0.0 |
HA |
KYHA0772 |
11.0 |
0.90 |
2.33 |
0.0 |
HA |
incl |
4.0 |
1.00 |
|
0.0 |
HA |
KYHA0773 |
15.0 |
1.15 |
0.93 |
0.0 |
HA |
incl |
4.0 |
1.57 |
|
0.0 |
HA |
KYHA0774 |
4.0 |
0.90 |
0.30 |
0.0 |
HA |
KYHA0775 |
3.0 |
1.26 |
0.20 |
0.0 |
HA |
KYHA0776 |
4.0 |
0.92 |
0.50 |
0.0 |
HA |
KYHA0777 |
8.0 |
0.87 |
1.85 |
0.0 |
HA |
incl |
4.0 |
1.10 |
|
0.0 |
HA |
KYHA0778 |
5.0 |
1.11 |
1.40 |
0.0 |
HA |
incl |
3.0 |
1.23 |
|
0.0 |
HA |
KYHA0779 |
8.0 |
0.81 |
0.74 |
0.0 |
HA |
incl |
2.0 |
1.01 |
|
3.0 |
HA |
KYHA0780 |
5.0 |
1.06 |
0.52 |
0.0 |
HA |
incl |
3.0 |
1.31 |
|
0.0 |
HA |
KYHA0781 |
3.0 |
0.66 |
0.20 |
0.0 |
HA |
KYHA0782 |
6.0 |
0.66 |
0.33 |
0.0 |
HA |
KYHA0783 |
12.0 |
0.67 |
1.73 |
0.0 |
HA |
KYHA0784 |
12.0 |
0.89 |
0.60 |
0.0 |
HA |
incl |
4.0 |
1.23 |
|
0.0 |
HA |
KYHA0785 |
12.0 |
0.82 |
2.53 |
0.0 |
HA |
KYHA0786 |
7.0 |
0.67 |
1.01 |
0.0 |
HA |
KYHA0787 |
13.0 |
1.15 |
0.86 |
0.0 |
HA |
incl |
4.0 |
1.61 |
|
0.0 |
HA |
KYHA0788 |
12.0 |
0.81 |
1.73 |
0.0 |
HA |
KYHA0789 |
5.0 |
0.91 |
0.30 |
0.0 |
HA |
KYHA0790 |
5.0 |
0.95 |
0.30 |
0.0 |
HA |
incl |
2.0 |
1.05 |
|
0.0 |
HA |
KYHA0791 |
3.0 |
0.61 |
0.40 |
0.0 |
HA |
KYHA0792 |
8.0 |
0.86 |
0.80 |
0.0 |
HA |
incl |
2.0 |
1.26 |
|
0.0 |
HA |
KYHA0793 |
3.0 |
1.30 |
0.30 |
0.0 |
HA |
KYHA0794 |
3.0 |
0.65 |
0.50 |
0.0 |
HA |
KYHA0795 |
13.0 |
0.62 |
1.30 |
0.0 |
HA |
KYHA0796 |
7.0 |
0.78 |
1.13 |
0.0 |
HA |
KYHA0797 |
5.0 |
0.68 |
0.30 |
0.0 |
HA |
KYHA0798 |
3.0 |
1.14 |
0.30 |
0.0 |
HA |
KYHA0799 |
12.0 |
1.18 |
1.12 |
0.0 |
HA |
incl |
8.0 |
1.34 |
|
0.0 |
HA |
KYHA0800 |
6.0 |
0.90 |
0.05 |
0.0 |
HA |
incl |
3.0 |
1.10 |
|
0.0 |
HA |
KYHA0801 |
10.0 |
1.18 |
0.77 |
0.0 |
HA |
incl |
4.0 |
1.71 |
|
0.0 |
HA |
KYHA0802 |
2.0 |
0.88 |
0.40 |
0.0 |
HA |
KYHA0803 |
12.0 |
0.98 |
0.94 |
0.0 |
HA |
incl |
4.0 |
1.61 |
|
0.0 |
HA |
KYHA0804 |
11.0 |
1.34 |
1.31 |
0.0 |
HA |
incl |
2.0 |
3.00 |
|
0.0 |
HA |
KYHA0805 |
7.0 |
1.45 |
0.07 |
0.0 |
HA |
incl |
5.0 |
1.72 |
|
0.0 |
HA |
KYHA0806 |
3.0 |
0.88 |
NSR |
0.0 |
HA |
KYHA0807 |
4.0 |
0.60 |
0.10 |
0.0 |
HA |
KYHA0808 |
5.0 |
0.78 |
NSR |
0.0 |
HA |
KYHA0809 |
2.0 |
0.82 |
0.10 |
0.0 |
HA |
KYHA0810 |
4.0 |
2.15 |
0.20 |
0.0 |
HA |
KYHA0811 |
12.0 |
1.27 |
1.53 |
0.0 |
HA |
incl |
3.0 |
2.16 |
|
0.0 |
HA |
KYHA0812 |
10.0 |
1.00 |
0.90 |
0.0 |
HA |
incl |
2.0 |
1.47 |
|
0.0 |
HA |
KYHA0813 |
3.0 |
2.35 |
0.20 |
0.0 |
HA |
KYHA0814 |
6.0 |
0.94 |
1.20 |
0.0 |
HA |
incl |
4.0 |
1.05 |
|
0.0 |
HA |
KYHA0815 |
6.0 |
1.11 |
1.70 |
0.0 |
HA |
incl |
3.0 |
1.39 |
|
0.0 |
HA |
KYHA0816 |
7.0 |
1.08 |
0.23 |
0.0 |
HA |
incl |
4.0 |
1.36 |
|
0.0 |
HA |
KYHA0817 |
4.0 |
1.19 |
0.10 |
0.0 |
HA |
KYHA0818 |
12.0 |
1.26 |
1.53 |
0.0 |
HA |
incl |
5.0 |
1.67 |
|
0.0 |
HA |
KYHA0819 |
10.0 |
1.04 |
1.01 |
0.0 |
HA |
incl |
3.0 |
1.56 |
|
0.0 |
HA |
KYHA0820 |
8.0 |
0.72 |
0.85 |
0.0 |
HA |
KYHA0821 |
3.0 |
0.63 |
NSR |
0.0 |
HA |
KYHA0822 |
|
NSR |
|
|
HA |
KYHA0823 |
4.0 |
0.58 |
0.10 |
0.0 |
HA |
KYHA0824 |
8.0 |
0.79 |
0.55 |
0.0 |
HA |
KYHA0825 |
12.0 |
0.76 |
2.38 |
0.0 |
HA |
KYHA0826 |
13.0 |
0.89 |
0.35 |
0.0 |
HA |
incl |
3.0 |
1.27 |
|
0.0 |
HA |
KYHA0827 |
13.0 |
0.85 |
2.45 |
0.0 |
HA |
KYHA0828 |
4.0 |
0.61 |
NSR |
0.0 |
HA |
KYHA0829 |
|
NSR |
|
|
HA |
KYHA0830 |
|
NSR |
|
|
HA |
KYHA0831 |
4.0 |
0.66 |
NSR |
0.0 |
HA |
KYHA0832 |
3.0 |
0.59 |
0.30 |
0.0 |
HA |
KYHA0833 |
9.0 |
1.04 |
1.02 |
0.0 |
HA |
incl |
2.0 |
1.90 |
|
0.0 |
HA |
KYHA0834 |
3.0 |
0.82 |
0.30 |
0.0 |
HA |
KYHA0835 |
2.0 |
1.31 |
0.60 |
0.0 |
HA |
KYHA0836 |
8.0 |
1.36 |
1.18 |
0.0 |
HA |
incl |
2.0 |
2.66 |
|
0.0 |
HA |
KYHA0837 |
12.0 |
1.46 |
1.68 |
0.0 |
HA |
incl |
3.0 |
2.42 |
|
0.0 |
HA |
KYHA0838 |
12.0 |
1.34 |
1.00 |
0.0 |
HA |
incl |
5.0 |
1.65 |
|
0.0 |
HA |
KYHA0839 |
12.0 |
1.11 |
1.00 |
0.0 |
HA |
incl |
3.0 |
1.78 |
|
0.0 |
HA |
KYHA0840 |
4.0 |
1.07 |
0.40 |
0.0 |
HA |
KYHA0842 |
4.0 |
0.57 |
0.40 |
0.0 |
HA |
KYHA0843 |
|
NSR |
|
|
HA |
KYHA0844 |
3.0 |
0.73 |
0.20 |
0.0 |
HA |
KYHA0845 |
|
NSR |
|
|
HA |
KYHA0846 |
|
NSR |
|
|
HA |
KYHA0847 |
|
NSR |
|
|
HA |
KYHA0848 |
2.0 |
0.64 |
0.20 |
0.0 |
HA |
KYHA0849 |
3.0 |
0.67 |
0.20 |
0.0 |
HA |
KYHA0850 |
10.0 |
0.71 |
1.76 |
0.0 |
HA |
KYHA0851 |
|
NSR |
|
|
HA |
KYHA0852 |
|
NSR |
|
|
HA |
KYHA0853 |
|
NSR |
|
|
HA |
KYHA0854 |
3.0 |
0.67 |
0.20 |
0.0 |
HA |
KYHA0855 |
|
NSR |
|
|
HA |
KYHA0856 |
|
NSR |
|
|
HA |
KYHA0857 |
|
NSR |
|
|
HA |
KYHA0858 |
|
NSR |
|
|
HA |
KYHA0859 |
|
NSR |
|
|
HA |
KYHA0860 |
|
NSR |
|
|
HA |
KYHA0861 |
2.0 |
1.02 |
0.50 |
3.0 |
HA |
KYHA0862 |
2.0 |
0.70 |
0.20 |
0.0 |
HA |
KYHA0863 |
2.0 |
0.67 |
0.20 |
0.0 |
HA |
KYHA0864 |
2.0 |
0.57 |
0.30 |
0.0 |
HA |
KYHA0865 |
2.0 |
0.53 |
0.40 |
0.0 |
HA |
KYHA0866 |
|
NSR |
|
|
HA |
KYHA0867 |
11.0 |
0.93 |
2.87 |
0.0 |
HA |
incl |
4.0 |
1.12 |
|
0.0 |
HA |
KYHA0868 |
9.0 |
1.15 |
0.26 |
0.0 |
HA |
incl |
4.0 |
1.81 |
|
0.0 |
HA |
KYHA0869 |
|
NSR |
|
|
HA |
KYHA0870 |
|
NSR |
|
|
HA |
KYHA0871 |
10.0 |
0.98 |
1.58 |
0.0 |
HA |
incl |
6.0 |
1.06 |
|
0.0 |
HA |
KYHA0872 |
3.0 |
0.82 |
0.50 |
0.0 |
HA |
KYHA0873 |
|
NSR |
|
|
HA |
KYHA0874 |
11.0 |
0.91 |
1.95 |
0.0 |
HA |
incl |
3.0 |
1.22 |
|
0.0 |
HA |
KYHA0875 |
11.0 |
1.22 |
2.14 |
0.0 |
HA |
incl |
9.0 |
1.35 |
|
0.0 |
HA |
KYHA0876 |
4.0 |
1.05 |
0.40 |
0.0 |
HA |
KYHA0877 |
12.0 |
0.90 |
2.62 |
0.0 |
HA |
incl |
3.0 |
1.17 |
|
0.0 |
HA |
KYHA0878 |
4.0 |
0.74 |
0.80 |
0.0 |
HA |
KYHA0879 |
|
NSR |
|
|
HA |
KYHA0880 |
|
NSR |
|
|
HA |
KYHA0881 |
8.0 |
0.87 |
0.85 |
0.0 |
HA |
incl |
4.0 |
1.15 |
|
0.0 |
HA |
KYHA0882 |
11.0 |
1.02 |
1.71 |
0.0 |
HA |
incl |
6.0 |
1.16 |
|
0.0 |
HA |
KYHA0883 |
10.0 |
0.98 |
2.15 |
0.0 |
HA |
incl |
4.0 |
1.44 |
|
0.0 |
HA |
KYHA0884 |
11.0 |
0.94 |
1.76 |
0.0 |
HA |
incl |
4.0 |
1.14 |
|
0.0 |
HA |
KYHA0885 |
7.0 |
1.22 |
1.16 |
0.0 |
HA |
KYHA0886 |
13.0 |
0.99 |
1.11 |
0.0 |
HA |
incl |
3.0 |
1.39 |
|
0.0 |
HA |
KYHA0887 |
12.0 |
1.15 |
1.58 |
0.0 |
HA |
incl |
3.0 |
1.22 |
|
0.0 |
HA |
incl |
5.0 |
1.43 |
|
7.0 |
HA |
KYHA0888 |
4.0 |
1.02 |
0.60 |
0.0 |
HA |
KYHA0889 |
4.0 |
0.61 |
0.30 |
0.0 |
HA |
KYHA0890 |
3.0 |
1.09 |
0.40 |
0.0 |
HA |
KYHA0891 |
4.0 |
0.81 |
0.30 |
0.0 |
HA |
KYHA0892 |
12.0 |
0.74 |
2.33 |
0.0 |
HA |
incl |
4.0 |
1.01 |
|
0.0 |
HA |
KYHA0893 |
13.0 |
0.92 |
1.64 |
0.0 |
HA |
incl |
4.0 |
1.09 |
|
0.0 |
HA |
KYHA0894 |
6.0 |
0.98 |
0.55 |
0.0 |
HA |
incl |
3.0 |
1.27 |
|
0.0 |
HA |
KYHA0895 |
4.0 |
0.74 |
0.20 |
0.0 |
HA |
KYHA0896 |
4.0 |
0.51 |
0.20 |
0.0 |
HA |
KYHA0897 |
12.0 |
0.74 |
0.66 |
0.0 |
HA |
KYPT0185 |
4.0 |
1.56 |
0.50 |
0.0 |
PT |
incl |
2.0 |
2.12 |
|
0.0 |
PT |
KYPT0186 |
6.0 |
1.02 |
1.37 |
0.0 |
PT |
incl |
2.0 |
1.30 |
|
0.0 |
PT |
KYPT0187 |
13.0 |
0.92 |
2.91 |
0.0 |
PT |
incl |
2.0 |
1.40 |
|
0.0 |
PT |
KYPT0189 |
6.0 |
0.97 |
0.73 |
0.0 |
PT |
incl |
2.0 |
1.30 |
|
0.0 |
PT |
KYPT0190 |
4.0 |
1.18 |
0.55 |
0.0 |
PT |
incl |
2.0 |
1.50 |
|
0.0 |
PT |
KYPT0191 |
11.0 |
1.15 |
2.71 |
0.0 |
PT |
incl |
2.0 |
1.56 |
|
0.0 |
PT |
KYPT0192 |
6.0 |
1.02 |
0.57 |
0.0 |
PT |
incl |
2.0 |
1.48 |
|
0.0 |
PT |
KYPT0193 |
|
NSR |
|
|
PT |
KYPT0194 |
8.0 |
0.81 |
1.58 |
0.0 |
PT |
incl |
2.0 |
1.05 |
|
0.0 |
PT |
KYPT0195 |
6.0 |
0.77 |
0.73 |
0.0 |
PT |
incl |
2.0 |
1.18 |
|
0.0 |
PT |
KYPT0196 |
10.0 |
0.86 |
4.72 |
0.0 |
PT |
incl |
2.0 |
1.11 |
|
0.0 |
PT |
KYPT0197 |
8.0 |
0.89 |
0.28 |
0.0 |
PT |
incl |
2.0 |
1.00 |
|
2.0 |
PT |
KYPT0198 |
14.0 |
1.06 |
2.76 |
0.0 |
PT |
incl |
2.0 |
1.59 |
|
0.0 |
PT |
KYPT0199 |
6.0 |
0.88 |
0.30 |
0.0 |
PT |
incl |
2.0 |
1.25 |
|
0.0 |
PT |
KYPT0200 |
14.0 |
0.92 |
2.35 |
0.0 |
PT |
incl |
4.0 |
1.38 |
|
0.0 |
PT |
KYPT0201 |
12.0 |
0.87 |
3.72 |
0.0 |
PT |
incl |
2.0 |
1.25 |
|
0.0 |
PT |
KYPT0202 |
7.7 |
1.11 |
1.42 |
0.0 |
PT |
incl |
4.0 |
1.58 |
|
0.0 |
PT |
KYPT0203 |
7.6 |
0.90 |
3.24 |
0.0 |
PT |
incl |
2.0 |
1.15 |
|
2.0 |
PT |
KYPT0204 |
2.0 |
1.05 |
0.30 |
0.0 |
PT |
KYPT0205 |
13.0 |
0.92 |
3.90 |
0.0 |
PT |
incl |
2.0 |
1.35 |
|
0.0 |
PT |
KYPT0206 |
4.0 |
0.84 |
1.30 |
0.0 |
PT |
incl |
2.0 |
1.01 |
|
0.0 |
PT |
KYPT0207 |
2.0 |
0.79 |
0.30 |
0.0 |
PT |
KYPT0208 |
2.0 |
0.89 |
0.20 |
0.0 |
PT |
KYPT0209 |
13.0 |
0.93 |
1.89 |
0.0 |
PT |
incl |
2.0 |
1.44 |
|
0.0 |
PT |
KYPT0210 |
2.0 |
1.29 |
0.60 |
0.0 |
PT |
KYPT0212 |
10.8 |
1.04 |
3.02 |
0.0 |
PT |
incl |
2.0 |
1.52 |
|
0.0 |
PT |
KYPT0213 |
11.0 |
1.15 |
2.98 |
0.0 |
PT |
incl |
8.0 |
1.23 |
|
0.0 |
PT |
KYPT0214 |
4.0 |
0.84 |
0.45 |
0.0 |
PT |
incl |
2.0 |
1.13 |
|
0.0 |
PT |
KYPT0215 |
4.0 |
0.94 |
0.85 |
0.0 |
PT |
incl |
2.0 |
1.23 |
|
0.0 |
PT |
KYPT0216 |
10.0 |
0.85 |
3.08 |
0.0 |
PT |
incl |
2.0 |
1.18 |
|
0.0 |
PT |
KYPT0217 |
7.0 |
0.85 |
2.33 |
0.0 |
PT |
incl |
2.0 |
1.37 |
|
0.0 |
PT |
KYPT0218 |
2.0 |
1.31 |
0.40 |
0.0 |
PT |
KYPT0219 |
2.9 |
1.62 |
NSR |
0.0 |
PT |
KYPT0220 |
12.0 |
1.11 |
2.33 |
0.0 |
PT |
incl |
4.0 |
1.48 |
|
0.0 |
PT |
KYPT0221 |
8.0 |
0.94 |
3.40 |
0.0 |
PT |
incl |
2.0 |
1.46 |
|
0.0 |
PT |
NSHA0138 |
4.0 |
0.85 |
0.30 |
0.0 |
HA |
NSHA0139 |
11.0 |
0.67 |
1.95 |
0.0 |
HA |
NSHA0140 |
5.0 |
0.89 |
0.20 |
0.0 |
HA |
NSHA0141 |
13.0 |
0.98 |
2.00 |
0.0 |
HA |
incl |
4.0 |
1.26 |
|
0.0 |
HA |
incl |
2.0 |
1.03 |
|
11.0 |
HA |
NSHA0142 |
13.0 |
0.87 |
1.57 |
0.0 |
HA |
incl |
4.0 |
1.03 |
|
0.0 |
HA |
NSHA0143 |
5.0 |
1.00 |
0.20 |
0.0 |
HA |
NSHA0143 |
3.0 |
0.83 |
2.10 |
8.0 |
HA |
incl |
5.0 |
1.00 |
|
0.0 |
HA |
NSHA0144 |
10.0 |
0.67 |
1.25 |
0.0 |
HA |
NSHA0145 |
4.0 |
0.79 |
0.10 |
0.0 |
HA |
NSHA0146 |
5.0 |
1.13 |
0.20 |
0.0 |
HA |
NSHA0147 |
13.0 |
0.86 |
1.88 |
0.0 |
HA |
incl |
5.0 |
1.02 |
|
0.0 |
HA |
NSHA0148 |
10.0 |
0.82 |
1.66 |
0.0 |
HA |
incl |
4.0 |
1.02 |
|
0.0 |
HA |
NSHA0150 |
4.0 |
1.04 |
0.40 |
0.0 |
HA |
NSHA0151 |
5.0 |
0.97 |
0.30 |
0.0 |
HA |
NSHA0151 |
1.0 |
0.72 |
2.50 |
11.0 |
HA |
NSHA0152 |
5.0 |
0.76 |
0.20 |
0.0 |
HA |
NSHA0153 |
4.0 |
0.63 |
NSR |
0.0 |
HA |
NSHA0154 |
4.0 |
0.79 |
0.10 |
0.0 |
HA |
NSHA0155 |
8.0 |
0.77 |
0.63 |
0.0 |
HA |
incl |
2.0 |
1.00 |
|
0.0 |
HA |
NSHA0156 |
8.0 |
0.74 |
1.28 |
0.0 |
HA |
NSHA0157 |
11.0 |
1.03 |
1.61 |
0.0 |
HA |
incl |
5.0 |
1.21 |
|
0.0 |
HA |
NSHA0158 |
12.0 |
0.80 |
1.73 |
0.0 |
HA |
incl |
5.0 |
1.09 |
|
0.0 |
HA |
NSHA0159 |
12.0 |
0.95 |
NSR |
0.0 |
HA |
incl |
4.0 |
1.33 |
|
8.0 |
HA |
NSHA0160 |
12.0 |
0.95 |
1.77 |
0.0 |
HA |
incl |
4.0 |
1.13 |
|
0.0 |
HA |
NSHA0161 |
5.0 |
1.09 |
0.30 |
0.0 |
HA |
NSHA0162 |
11.0 |
0.78 |
1.02 |
0.0 |
HA |
incl |
4.0 |
1.08 |
|
0.0 |
HA |
NSHA0163 |
5.0 |
0.69 |
0.20 |
0.0 |
HA |
NSHA0164 |
4.0 |
0.65 |
0.20 |
0.0 |
HA |
NSHA0165 |
10.0 |
0.80 |
1.52 |
0.0 |
HA |
NSHA0166 |
9.0 |
0.79 |
3.42 |
0.0 |
HA |
NSHA0167 |
|
NSR |
|
|
HA |
NSHA0168 |
|
NSR |
|
|
HA |
NSHA0169 |
|
NSR |
|
|
HA |
NSHA0170 |
|
NSR |
|
|
HA |
NSHA0171 |
|
NSR |
|
|
HA |
NSHA0172 |
|
NSR |
|
|
HA |
NSHA0173 |
4.0 |
0.80 |
0.20 |
0.0 |
HA |
NSHA0174 |
11.0 |
0.73 |
1.39 |
0.0 |
HA |
NSHA0175 |
12.0 |
0.63 |
2.30 |
0.0 |
HA |
NSHA0176 |
4.0 |
0.83 |
0.20 |
0.0 |
HA |
NSHA0177 |
4.0 |
0.65 |
0.30 |
0.0 |
HA |
NSHA0178 |
|
NSR |
|
|
HA |
NSHA0179 |
7.0 |
0.78 |
0.14 |
0.0 |
HA |
NSHA0180 |
3.0 |
0.66 |
NSR |
0.0 |
HA |
NSHA0181 |
13.0 |
1.28 |
1.27 |
0.0 |
HA |
incl |
8.0 |
1.48 |
|
0.0 |
HA |
NSHA0182 |
9.0 |
1.11 |
0.71 |
0.0 |
HA |
incl |
4.0 |
1.53 |
|
0.0 |
HA |
NSHA0183 |
2.0 |
1.37 |
0.20 |
0.0 |
HA |
NSHA0184 |
12.0 |
0.86 |
1.08 |
0.0 |
HA |
incl |
4.0 |
1.24 |
|
0.0 |
HA |
NSHA0185 |
4.0 |
1.12 |
0.20 |
0.0 |
HA |
NSHA0186 |
10.0 |
0.98 |
0.58 |
0.0 |
HA |
incl |
3.0 |
1.75 |
|
0.0 |
HA |
NSHA0187 |
4.0 |
0.81 |
0.40 |
0.0 |
HA |
NSHA0188 |
7.0 |
0.71 |
0.34 |
0.0 |
HA |
NSHA0189 |
13.0 |
1.03 |
1.22 |
0.0 |
HA |
incl |
5.0 |
1.24 |
|
0.0 |
HA |
NSHA0190 |
4.0 |
0.61 |
0.20 |
0.0 |
HA |
NSHA0191 |
4.0 |
0.54 |
0.20 |
0.0 |
HA |
NSHA0192 |
5.0 |
0.90 |
0.70 |
0.0 |
HA |
NSHA0193 |
6.0 |
0.68 |
0.25 |
0.0 |
HA |
NSHA0194 |
3.0 |
1.03 |
0.20 |
0.0 |
HA |
NSHA0195 |
11.0 |
0.91 |
1.26 |
0.0 |
HA |
incl |
4.0 |
1.26 |
|
0.0 |
HA |
NSHA0196 |
11.0 |
0.74 |
1.03 |
0.0 |
HA |
NSHA0197 |
10.0 |
0.72 |
1.33 |
0.0 |
HA |
incl |
3.0 |
1.10 |
|
0.0 |
HA |
NSHA0198 |
2.0 |
0.67 |
2.00 |
4.0 |
HA |
NSHA0199 |
4.0 |
0.81 |
NSR |
0.0 |
HA |
NSHA0200 |
11.0 |
1.25 |
1.61 |
0.0 |
HA |
incl |
4.0 |
1.45 |
|
0.0 |
HA |
NSHA0201 |
2.0 |
0.87 |
0.50 |
0.0 |
HA |
NSHA0202 |
5.0 |
0.71 |
0.90 |
0.0 |
HA |
NSHA0203 |
11.0 |
0.81 |
1.53 |
0.0 |
HA |
NSHA0204 |
3.0 |
0.85 |
NSR |
0.0 |
HA |
NSHA0205 |
13.0 |
0.57 |
1.05 |
0.0 |
HA |
NSHA0206 |
4.0 |
0.54 |
NSR |
0.0 |
HA |
NSHA0207 |
|
NSR |
|
|
HA |
NSHA0208 |
2.0 |
0.81 |
0.10 |
0.0 |
HA |
NSHA0209 |
4.0 |
0.95 |
NSR |
0.0 |
HA |
NSHA0210 |
5.0 |
1.06 |
0.10 |
0.0 |
HA |
NSHA0211 |
9.0 |
0.83 |
1.29 |
0.0 |
HA |
NSHA0212 |
5.0 |
0.54 |
0.88 |
0.0 |
HA |
NSHA0213 |
4.0 |
0.71 |
0.80 |
0.0 |
HA |
NSHA0214 |
10.0 |
0.64 |
1.38 |
0.0 |
HA |
NSHA0215 |
5.0 |
0.61 |
0.60 |
0.0 |
HA |
NSHA0216 |
|
NSR |
|
|
HA |
NSHA0217 |
|
NSR |
|
|
HA |
NSHA0218 |
13.0 |
0.76 |
1.01 |
0.0 |
HA |
NSHA0219 |
5.0 |
0.52 |
NSR |
0.0 |
HA |
NSHA0220 |
5.0 |
0.82 |
NSR |
0.0 |
HA |
NSHA0221 |
8.0 |
0.99 |
0.40 |
0.0 |
HA |
incl |
4.0 |
1.40 |
|
0.0 |
HA |
NSHA0222 |
11.0 |
0.89 |
0.97 |
0.0 |
HA |
incl |
4.0 |
1.12 |
|
0.0 |
HA |
NSHA0223 |
4.0 |
0.86 |
NSR |
0.0 |
HA |
NSHA0224 |
10.0 |
1.25 |
0.98 |
0.0 |
HA |
incl |
7.0 |
1.38 |
|
0.0 |
HA |
NSHA0225 |
12.0 |
1.32 |
1.10 |
0.0 |
HA |
incl |
4.0 |
1.87 |
|
0.0 |
HA |
NSHA0226 |
4.0 |
0.74 |
NSR |
0.0 |
HA |
NSHA0227 |
4.0 |
1.11 |
NSR |
0.0 |
HA |
NSHA0228 |
11.0 |
0.62 |
1.19 |
0.0 |
HA |
NSHA0229 |
4.0 |
0.71 |
NSR |
0.0 |
HA |
NSHA0230 |
10.0 |
1.02 |
0.86 |
0.0 |
HA |
incl |
3.0 |
1.28 |
|
0.0 |
HA |
NSHA0231 |
12.0 |
0.93 |
2.84 |
0.0 |
HA |
incl |
4.0 |
1.17 |
|
0.0 |
HA |
NSHA0232 |
5.0 |
0.75 |
NSR |
0.0 |
HA |
incl |
2.0 |
1.11 |
|
0.0 |
HA |
NSHA0233 |
4.0 |
0.63 |
NSR |
0.0 |
HA |
NSHA0234 |
5.0 |
1.15 |
NSR |
0.0 |
HA |
NSHA0235 |
4.0 |
1.01 |
NSR |
0.0 |
HA |
NSHA0236 |
11.0 |
1.09 |
0.79 |
0.0 |
HA |
incl |
8.0 |
1.20 |
|
0.0 |
HA |
NSHA0237 |
|
NSR |
|
|
HA |
NSHA0238 |
2.0 |
1.09 |
NSR |
0.0 |
HA |
NSHA0239 |
6.0 |
0.61 |
1.70 |
0.0 |
HA |
NSHA0240 |
4.0 |
0.60 |
NSR |
0.0 |
HA |
NSHA0241 |
10.0 |
0.99 |
0.52 |
0.0 |
HA |
incl |
4.0 |
1.22 |
|
0.0 |
HA |
NSHA0242 |
9.0 |
0.65 |
0.29 |
0.0 |
HA |
NSHA0243 |
10.0 |
0.61 |
0.45 |
0.0 |
HA |
NSHA0244 |
7.0 |
0.80 |
1.37 |
0.0 |
HA |
NSHA0245 |
2.0 |
0.61 |
2.30 |
4.0 |
HA |
NSHA0246 |
7.0 |
0.82 |
0.67 |
0.0 |
HA |
incl |
3.0 |
1.01 |
|
4.0 |
HA |
NSHA0247 |
3.0 |
0.63 |
0.70 |
7.0 |
HA |
NSHA0248 |
|
NSR |
|
|
HA |
NSHA0249 |
5.0 |
0.74 |
0.50 |
0.0 |
HA |
NSHA0250 |
5.0 |
0.94 |
0.30 |
0.0 |
HA |
NSHA0251 |
4.0 |
0.56 |
0.90 |
0.0 |
HA |
NSHA0252 |
|
NSR |
|
|
HA |
NSHA0253 |
6.0 |
0.73 |
NSR |
0.0 |
HA |
NSHA0254 |
|
NSR |
|
|
HA |
NSHA0255 |
3.0 |
0.78 |
0.10 |
0.0 |
HA |
NSHA0256 |
4.0 |
0.51 |
NSR |
0.0 |
HA |
NSHA0257 |
7.0 |
0.76 |
0.41 |
0.0 |
HA |
NSHA0258 |
15.0 |
1.09 |
0.71 |
0.0 |
HA |
incl |
4.0 |
1.80 |
|
0.0 |
HA |
NSHA0259 |
6.0 |
1.24 |
0.73 |
0.0 |
HA |
incl |
4.0 |
1.43 |
|
0.0 |
HA |
NSHA0260 |
8.0 |
0.70 |
1.31 |
0.0 |
HA |
incl |
2.0 |
1.05 |
|
0.0 |
HA |
NSHA0261 |
12.0 |
1.23 |
1.58 |
0.0 |
HA |
incl |
3.0 |
1.94 |
|
0.0 |
HA |
NSHA0262 |
13.0 |
1.35 |
1.54 |
0.0 |
HA |
incl |
4.0 |
1.81 |
|
0.0 |
HA |
NSHA0263 |
9.0 |
1.35 |
0.90 |
0.0 |
HA |
incl |
4.0 |
1.71 |
|
0.0 |
HA |
NSHA0264 |
12.0 |
0.99 |
0.57 |
0.0 |
HA |
incl |
4.0 |
1.61 |
|
0.0 |
HA |
NSHA0265 |
12.0 |
1.11 |
0.95 |
0.0 |
HA |
incl |
4.0 |
1.81 |
|
0.0 |
HA |
NSHA0266 |
12.0 |
0.92 |
3.05 |
0.0 |
HA |
incl |
5.0 |
1.25 |
|
0.0 |
HA |
NSHA0267 |
3.0 |
0.98 |
0.40 |
0.0 |
HA |
NSHA0268 |
3.0 |
0.78 |
0.10 |
0.0 |
HA |
NSHA0269 |
11.0 |
0.81 |
0.76 |
0.0 |
HA |
NSHA0270 |
4.0 |
1.02 |
NSR |
0.0 |
HA |
NSHA0271 |
8.0 |
1.13 |
0.70 |
0.0 |
HA |
incl |
3.0 |
1.76 |
|
0.0 |
HA |
NSHA0272 |
11.0 |
0.88 |
1.41 |
0.0 |
HA |
incl |
4.0 |
1.08 |
|
0.0 |
HA |
NSHA0273 |
9.0 |
0.90 |
0.86 |
0.0 |
HA |
incl |
2.0 |
1.46 |
|
0.0 |
HA |
NSHA0274 |
8.0 |
0.99 |
0.50 |
0.0 |
HA |
incl |
3.0 |
1.47 |
|
0.0 |
HA |
NSHA0275 |
12.0 |
0.88 |
1.22 |
0.0 |
HA |
incl |
3.0 |
1.19 |
|
0.0 |
HA |
NSHA0276 |
7.0 |
1.17 |
1.03 |
0.0 |
HA |
incl |
3.0 |
1.81 |
|
0.0 |
HA |
NSHA0277 |
11.0 |
1.15 |
2.25 |
0.0 |
HA |
incl |
4.0 |
1.38 |
|
0.0 |
HA |
NSHA0278 |
7.0 |
0.98 |
2.03 |
0.0 |
HA |
incl |
4.0 |
1.16 |
|
0.0 |
HA |
NSHA0279 |
13.0 |
0.96 |
3.28 |
0.0 |
HA |
incl |
5.0 |
1.21 |
|
0.0 |
HA |
NSHA0280 |
5.0 |
0.76 |
0.40 |
0.0 |
HA |
NSHA0280 |
3.0 |
0.65 |
3.40 |
9.0 |
HA |
NSHA0281 |
5.0 |
1.17 |
0.20 |
0.0 |
HA |
NSHA0282 |
12.0 |
1.07 |
1.33 |
0.0 |
HA |
incl |
4.0 |
1.41 |
|
0.0 |
HA |
NSHA0283 |
12.0 |
0.88 |
2.12 |
0.0 |
HA |
incl |
3.0 |
1.18 |
|
0.0 |
HA |
NSHA0284 |
4.0 |
0.90 |
0.20 |
0.0 |
HA |
NSHA0285 |
12.0 |
1.09 |
1.08 |
0.0 |
HA |
incl |
4.0 |
1.61 |
|
0.0 |
HA |
NSHA0286 |
4.0 |
1.10 |
0.30 |
0.0 |
HA |
incl |
4.0 |
1.10 |
|
0.0 |
HA |
NSHA0287 |
5.0 |
0.84 |
0.10 |
0.0 |
HA |
NSHA0288 |
3.0 |
1.05 |
0.30 |
0.0 |
HA |
NSHA0289 |
10.0 |
1.19 |
2.14 |
0.0 |
HA |
incl |
2.0 |
1.43 |
|
0.0 |
HA |
NSHA0290 |
8.0 |
1.21 |
1.62 |
0.0 |
HA |
incl |
3.0 |
1.34 |
|
0.0 |
HA |
NSHA0291 |
2.0 |
1.59 |
2.00 |
0.0 |
HA |
NSHA0292 |
3.0 |
1.38 |
0.50 |
0.0 |
HA |
NSHA0293 |
12.0 |
1.44 |
1.29 |
0.0 |
HA |
incl |
3.0 |
2.47 |
|
0.0 |
HA |
NSHA0294 |
9.0 |
1.12 |
1.89 |
0.0 |
HA |
incl |
4.0 |
1.35 |
|
0.0 |
HA |
NSHA0295 |
11.0 |
1.18 |
1.91 |
0.0 |
HA |
incl |
8.0 |
1.32 |
|
0.0 |
HA |
NSHA0296 |
7.0 |
1.84 |
0.89 |
0.0 |
HA |
incl |
4.0 |
2.71 |
|
0.0 |
HA |
NSHA0297 |
12.0 |
1.10 |
3.82 |
0.0 |
HA |
incl |
7.0 |
1.18 |
|
0.0 |
HA |
NSHA0298 |
|
NSR |
|
|
HA |
NSHA0299 |
|
NSR |
|
|
HA |
NSHA0300 |
11.0 |
0.88 |
0.96 |
0.0 |
HA |
incl |
2.0 |
1.43 |
|
0.0 |
HA |
NSHA0301 |
4.0 |
0.80 |
0.30 |
0.0 |
HA |
NSHA0302 |
12.0 |
0.80 |
0.88 |
0.0 |
HA |
incl |
5.0 |
1.04 |
|
0.0 |
HA |
NSHA0303 |
4.0 |
0.90 |
0.30 |
0.0 |
HA |
NSHA0304 |
13.0 |
1.19 |
0.97 |
0.0 |
HA |
incl |
4.0 |
1.41 |
|
0.0 |
HA |
NSHA0305 |
8.0 |
0.86 |
1.16 |
0.0 |
HA |
incl |
5.0 |
1.06 |
|
0.0 |
HA |
NSHA0306 |
13.0 |
0.82 |
2.55 |
0.0 |
HA |
NSHA0307 |
4.0 |
1.11 |
0.40 |
0.0 |
HA |
NSHA0308 |
3.0 |
1.12 |
NSR |
0.0 |
HA |
NSHA0309 |
|
NSR |
|
|
HA |
NSHA0310 |
8.0 |
0.91 |
2.09 |
0.0 |
HA |
incl |
5.0 |
1.00 |
|
0.0 |
HA |
NSHA0311 |
12.0 |
1.38 |
2.14 |
0.0 |
HA |
incl |
6.0 |
1.83 |
|
0.0 |
HA |
NSHA0312 |
9.0 |
0.96 |
1.16 |
0.0 |
HA |
incl |
3.0 |
1.06 |
|
6.0 |
HA |
NSHA0313 |
11.0 |
0.91 |
0.92 |
0.0 |
HA |
incl |
4.0 |
1.07 |
|
0.0 |
HA |
NSHA0314 |
11.0 |
0.93 |
2.83 |
0.0 |
HA |
incl |
4.0 |
1.39 |
|
0.0 |
HA |
NSHA0315 |
13.0 |
1.11 |
1.74 |
0.0 |
HA |
incl |
4.0 |
1.60 |
|
0.0 |
HA |
NSHA0316 |
12.0 |
1.05 |
4.36 |
0.0 |
HA |
incl |
3.0 |
1.56 |
|
0.0 |
HA |
NSHA0317 |
5.0 |
0.94 |
0.30 |
0.0 |
HA |
NSHA0318 |
8.0 |
0.90 |
0.49 |
0.0 |
HA |
incl |
5.0 |
1.04 |
|
0.0 |
HA |
NSHA0319 |
3.0 |
1.11 |
0.20 |
0.0 |
HA |
NSHA0320 |
2.0 |
1.29 |
0.20 |
0.0 |
HA |
NSHA0321 |
8.0 |
1.02 |
NSR |
0.0 |
HA |
incl |
4.0 |
1.35 |
|
0.0 |
HA |
NSHA0322 |
13.0 |
0.79 |
NSR |
0.0 |
HA |
incl |
5.0 |
1.09 |
|
0.0 |
HA |
NSHA0323 |
2.0 |
0.89 |
0.20 |
0.0 |
HA |
NSHA0324 |
10.0 |
0.89 |
1.16 |
0.0 |
HA |
incl |
2.0 |
1.25 |
|
0.0 |
HA |
NSHA0325 |
2.0 |
1.16 |
0.10 |
0.0 |
HA |
incl |
2.0 |
1.16 |
|
0.0 |
HA |
NSHA0326 |
11.0 |
0.79 |
0.78 |
0.0 |
HA |
NSHA0327 |
11.0 |
0.70 |
1.51 |
0.0 |
HA |
NSHA0328 |
11.0 |
1.01 |
0.97 |
0.0 |
HA |
incl |
4.0 |
1.35 |
|
0.0 |
HA |
NSHA0329 |
5.0 |
0.71 |
NSR |
0.0 |
HA |
NSHA0330 |
6.0 |
0.91 |
NSR |
0.0 |
HA |
incl |
3.0 |
1.16 |
|
0.0 |
HA |
NSHA0331 |
9.0 |
0.84 |
1.38 |
0.0 |
HA |
NSHA0332 |
4.0 |
0.60 |
NSR |
0.0 |
HA |
NSHA0333 |
10.0 |
0.70 |
1.17 |
0.0 |
HA |
NSHA0334 |
3.0 |
0.91 |
0.10 |
0.0 |
HA |
NSHA0335 |
6.0 |
0.53 |
0.70 |
3.0 |
HA |
NSHA0336 |
11.0 |
0.99 |
0.12 |
0.0 |
HA |
incl |
5.0 |
1.42 |
|
0.0 |
HA |
NSHA0337 |
10.0 |
0.98 |
0.18 |
0.0 |
HA |
incl |
4.0 |
1.42 |
|
0.0 |
HA |
NSHA0338 |
12.0 |
1.30 |
1.31 |
0.0 |
HA |
incl |
4.0 |
1.72 |
|
0.0 |
HA |
NSHA0339 |
6.0 |
1.33 |
0.10 |
0.0 |
HA |
incl |
4.0 |
1.65 |
|
0.0 |
HA |
NSHA0340 |
7.0 |
0.83 |
0.87 |
0.0 |
HA |
incl |
2.0 |
1.05 |
|
5.0 |
HA |
NSHA0341 |
3.0 |
1.70 |
NSR |
0.0 |
HA |
incl |
3.0 |
1.70 |
|
0.0 |
HA |
NSHA0342 |
5.0 |
1.40 |
1.02 |
0.0 |
HA |
incl |
2.0 |
2.08 |
|
0.0 |
HA |
NSHA0343 |
7.0 |
1.06 |
0.81 |
0.0 |
HA |
incl |
3.0 |
1.48 |
|
0.0 |
HA |
NSHA0344 |
12.0 |
1.30 |
1.99 |
0.0 |
HA |
incl |
4.0 |
1.77 |
|
0.0 |
HA |
NSHA0345 |
10.0 |
1.44 |
1.47 |
0.0 |
HA |
incl |
4.0 |
2.01 |
|
0.0 |
HA |
NSHA0346 |
12.0 |
0.97 |
2.89 |
0.0 |
HA |
incl |
4.0 |
1.24 |
|
0.0 |
HA |
NSHA0347 |
13.0 |
0.89 |
2.64 |
0.0 |
HA |
incl |
4.0 |
1.24 |
|
0.0 |
HA |
NSHA0348 |
9.0 |
0.89 |
1.60 |
0.0 |
HA |
incl |
3.0 |
1.35 |
|
0.0 |
HA |
NSHA0349 |
4.0 |
0.90 |
1.50 |
0.0 |
HA |
NSHA0350 |
9.0 |
1.09 |
2.40 |
2.0 |
HA |
NSHA0351 |
3.0 |
0.70 |
0.60 |
0.0 |
HA |
NSHA0352 |
7.0 |
1.04 |
1.10 |
0.0 |
HA |
incl |
3.0 |
1.67 |
|
0.0 |
HA |
NSHA0353 |
7.0 |
0.96 |
0.87 |
0.0 |
HA |
incl |
4.0 |
1.13 |
|
0.0 |
HA |
NSHA0354 |
13.0 |
1.09 |
1.58 |
0.0 |
HA |
incl |
9.0 |
1.28 |
|
0.0 |
HA |
NSHA0355 |
13.0 |
1.03 |
3.35 |
0.0 |
HA |
incl |
3.0 |
1.34 |
|
0.0 |
HA |
NSHA0357 |
2.0 |
1.80 |
0.30 |
0.0 |
HA |
NSHA0358 |
4.0 |
1.22 |
0.30 |
0.0 |
HA |
NSHA0359 |
6.0 |
1.08 |
1.75 |
0.0 |
HA |
NSHA0360 |
9.0 |
1.09 |
1.13 |
0.0 |
HA |
incl |
3.0 |
1.48 |
|
0.0 |
HA |
NSHA0361 |
4.0 |
1.13 |
1.50 |
0.0 |
HA |
NSHA0362 |
4.0 |
1.14 |
0.30 |
0.0 |
HA |
NSHA0363 |
13.0 |
1.48 |
1.18 |
0.0 |
HA |
incl |
5.0 |
2.23 |
|
0.0 |
HA |
NSHA0364 |
12.0 |
1.22 |
1.03 |
0.0 |
HA |
incl |
4.0 |
1.73 |
|
0.0 |
HA |
NSHA0365 |
10.0 |
1.10 |
1.15 |
0.0 |
HA |
incl |
3.0 |
1.56 |
|
0.0 |
HA |
NSHA0366 |
11.0 |
1.35 |
0.89 |
0.0 |
HA |
incl |
4.0 |
1.74 |
|
0.0 |
HA |
NSHA0367 |
7.0 |
1.01 |
0.91 |
0.0 |
HA |
incl |
4.0 |
1.29 |
|
0.0 |
HA |
NSHA0368 |
13.0 |
1.29 |
1.25 |
0.0 |
HA |
incl |
11.0 |
1.40 |
|
0.0 |
HA |
incl |
4.0 |
1.94 |
|
0.0 |
HA |
NSHA0369 |
4.0 |
0.91 |
0.30 |
0.0 |
HA |
NSHA0370 |
12.0 |
1.16 |
2.17 |
0.0 |
HA |
incl |
4.0 |
1.47 |
|
0.0 |
HA |
NSHA0371 |
13.0 |
1.04 |
2.18 |
0.0 |
HA |
incl |
4.0 |
1.24 |
|
0.0 |
HA |
NSHA0372 |
5.0 |
0.51 |
0.30 |
0.0 |
HA |
NSHA0373 |
4.0 |
1.00 |
0.30 |
0.0 |
HA |
NSHA0374 |
12.0 |
0.78 |
0.87 |
0.0 |
HA |
incl |
4.0 |
1.21 |
|
0.0 |
HA |
NSHA0375 |
5.0 |
1.18 |
0.50 |
0.0 |
HA |
NSHA0376 |
6.0 |
0.91 |
0.35 |
0.0 |
HA |
NSHA0377 |
12.0 |
0.91 |
0.68 |
0.0 |
HA |
incl |
4.0 |
1.22 |
|
0.0 |
HA |
NSHA0378 |
6.0 |
1.26 |
0.10 |
0.0 |
HA |
incl |
3.0 |
1.68 |
|
0.0 |
HA |
NSHA0379 |
7.0 |
0.79 |
NSR |
0.0 |
HA |
NSHA0380 |
2.0 |
0.84 |
NSR |
0.0 |
HA |
NSHA0381 |
12.0 |
0.82 |
1.03 |
0.0 |
HA |
incl |
5.0 |
1.09 |
|
0.0 |
HA |
NSHA0382 |
2.0 |
0.61 |
0.20 |
0.0 |
HA |
NSHA0383 |
3.0 |
0.79 |
1.80 |
3.0 |
HA |
NSHA0384 |
8.0 |
0.81 |
2.08 |
0.0 |
HA |
NSHA0385 |
13.0 |
0.95 |
1.38 |
0.0 |
HA |
incl |
7.0 |
1.21 |
|
0.0 |
HA |
NSHA0386 |
12.0 |
1.16 |
0.50 |
0.0 |
HA |
incl |
8.0 |
1.38 |
|
0.0 |
HA |
incl |
5.0 |
1.63 |
|
0.0 |
HA |
NSHA0387 |
12.0 |
1.09 |
2.73 |
0.0 |
HA |
incl |
4.0 |
1.49 |
|
0.0 |
HA |
NSHA0388 |
10.0 |
1.06 |
1.88 |
0.0 |
HA |
incl |
2.0 |
1.55 |
|
4.0 |
HA |
NSHA0389 |
3.0 |
0.75 |
0.10 |
0.0 |
HA |
NSHA0390 |
10.0 |
0.74 |
0.21 |
0.0 |
HA |
NSHA0391 |
|
NSR |
|
|
HA |
NSHA0392 |
11.0 |
0.96 |
0.98 |
0.0 |
HA |
incl |
2.0 |
2.13 |
|
0.0 |
HA |
NSHA0393 |
9.0 |
1.13 |
0.50 |
0.0 |
HA |
incl |
2.0 |
2.12 |
|
0.0 |
HA |
NSHA0394 |
6.0 |
0.90 |
NSR |
0.0 |
HA |
incl |
3.0 |
1.22 |
|
0.0 |
HA |
NSHA0395 |
11.0 |
0.74 |
0.20 |
0.0 |
HA |
incl |
3.0 |
1.20 |
|
4.0 |
HA |
NSHA0396 |
7.0 |
0.80 |
0.50 |
0.0 |
HA |
NSHA0397 |
5.0 |
0.72 |
0.20 |
0.0 |
HA |
NSPT0001 |
10.0 |
1.28 |
1.22 |
0.0 |
PT |
incl |
4.0 |
1.49 |
|
0.0 |
PT |
NSPT0002 |
6.0 |
1.10 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.94 |
|
0.0 |
PT |
NSPT0003 |
10.0 |
1.11 |
1.04 |
0.0 |
PT |
incl |
4.0 |
1.36 |
|
0.0 |
PT |
NSPT0004 |
5.0 |
0.87 |
3.74 |
0.0 |
PT |
NSPT0005 |
10.0 |
1.19 |
0.84 |
0.0 |
PT |
incl |
4.0 |
1.40 |
|
0.0 |
PT |
NSPT0006 |
4.0 |
1.40 |
0.65 |
0.0 |
PT |
incl |
2.0 |
2.25 |
|
0.0 |
PT |
NSPT0007 |
9.0 |
1.02 |
1.10 |
0.0 |
PT |
incl |
2.0 |
1.14 |
|
7.0 |
PT |
NSPT0008 |
13.0 |
1.30 |
1.14 |
0.0 |
PT |
incl |
10.0 |
1.44 |
|
0.0 |
PT |
NSPT0009 |
12.0 |
1.25 |
1.08 |
0.0 |
PT |
incl |
8.0 |
1.36 |
|
0.0 |
PT |
NSPT0010 |
10.9 |
0.95 |
2.92 |
0.0 |
PT |
incl |
4.0 |
1.11 |
|
0.0 |
PT |
NSPT0011 |
6.0 |
0.89 |
0.27 |
0.0 |
PT |
incl |
2.0 |
1.38 |
|
0.0 |
PT |
NSPT0012 |
2.0 |
1.16 |
NSR |
0.0 |
PT |
NSPT0013 |
11.8 |
1.35 |
1.24 |
0.0 |
PT |
incl |
4.0 |
1.90 |
|
0.0 |
PT |
NSPT0014 |
10.0 |
1.18 |
0.70 |
0.0 |
PT |
incl |
4.0 |
1.92 |
|
0.0 |
PT |
NSPT0015 |
11.8 |
1.25 |
1.87 |
0.0 |
PT |
incl |
6.0 |
1.45 |
|
0.0 |
PT |
NSPT0016 |
2.0 |
1.15 |
0.20 |
0.0 |
PT |
NSPT0017 |
10.0 |
1.08 |
1.98 |
0.0 |
PT |
incl |
4.0 |
1.70 |
|
0.0 |
PT |
NSPT0018 |
5.0 |
1.36 |
0.66 |
0.0 |
PT |
incl |
2.0 |
2.45 |
|
0.0 |
PT |
NSPT0019 |
6.0 |
0.75 |
0.76 |
0.0 |
PT |
NSPT0020 |
10.0 |
0.88 |
1.74 |
0.0 |
PT |
incl |
2.0 |
1.55 |
|
0.0 |
PT |
NSPT0021 |
5.0 |
1.15 |
2.40 |
4.0 |
PT |
NSPT0023 |
10.0 |
1.49 |
0.97 |
0.0 |
PT |
incl |
4.0 |
2.01 |
|
0.0 |
PT |
NSPT0024 |
3.8 |
1.64 |
0.25 |
0.0 |
PT |
incl |
2.0 |
2.29 |
|
0.0 |
PT |
NSPT0025 |
8.0 |
1.16 |
0.93 |
0.0 |
PT |
incl |
2.0 |
1.87 |
|
0.0 |
PT |
NSPT0026 |
10.0 |
1.28 |
1.06 |
0.0 |
PT |
incl |
2.0 |
2.36 |
|
0.0 |
PT |
NSPT0027 |
4.0 |
1.46 |
0.24 |
0.0 |
PT |
incl |
2.2 |
2.09 |
|
0.0 |
PT |
NSPT0028 |
6.0 |
1.20 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.94 |
|
0.0 |
PT |
NSPT0029 |
12.0 |
1.00 |
0.89 |
0.0 |
PT |
incl |
1.4 |
2.10 |
|
0.0 |
PT |
NSPT0030 |
4.0 |
1.32 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.78 |
|
0.0 |
PT |
NSPT0031 |
3.0 |
1.03 |
NSR |
0.0 |
PT |
NSPT0032 |
11.5 |
1.00 |
1.59 |
0.0 |
PT |
incl |
2.0 |
1.90 |
|
0.0 |
PT |
NSPT0033 |
12.0 |
1.41 |
1.23 |
0.0 |
PT |
incl |
6.0 |
1.62 |
|
0.0 |
PT |
NSPT0034 |
6.0 |
1.12 |
NSR |
0.0 |
PT |
incl |
2.0 |
2.02 |
|
0.0 |
PT |
NSPT0035 |
6.0 |
0.82 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.22 |
|
0.0 |
PT |
NSPT0036 |
2.0 |
1.06 |
NSR |
0.0 |
PT |
NSPT0037 |
6.0 |
1.14 |
0.70 |
0.0 |
PT |
incl |
2.0 |
2.31 |
|
0.0 |
PT |
NSPT0038 |
10.0 |
0.93 |
0.84 |
0.0 |
PT |
incl |
2.0 |
1.20 |
|
0.0 |
PT |
NSPT0039 |
11.0 |
1.41 |
0.99 |
0.0 |
PT |
incl |
4.0 |
1.72 |
|
0.0 |
PT |
NSPT0040 |
10.0 |
1.00 |
0.80 |
0.0 |
PT |
incl |
4.0 |
1.41 |
|
0.0 |
PT |
NSPT0042 |
11.0 |
1.12 |
1.08 |
0.0 |
PT |
incl |
2.0 |
1.72 |
|
0.0 |
PT |
NSPT0043 |
13.0 |
1.17 |
1.69 |
0.0 |
PT |
incl |
8.0 |
1.31 |
|
0.0 |
PT |
incl |
2.0 |
2.02 |
|
0.0 |
PT |
NSPT0044 |
2.0 |
0.75 |
0.10 |
0.0 |
PT |
NSPT0045 |
11.0 |
1.20 |
0.60 |
0.0 |
PT |
incl |
4.0 |
1.50 |
|
0.0 |
PT |
NSPT0046 |
9.0 |
0.91 |
0.89 |
0.0 |
PT |
incl |
2.0 |
1.49 |
|
0.0 |
PT |
NSPT0047 |
12.0 |
1.01 |
2.53 |
0.0 |
PT |
incl |
8.0 |
1.17 |
|
0.0 |
PT |
NSPT0048 |
4.0 |
1.18 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.71 |
|
0.0 |
PT |
NSPT0049 |
4.0 |
1.09 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.42 |
|
0.0 |
PT |
NSPT0050 |
11.0 |
1.18 |
1.20 |
0.0 |
PT |
incl |
2.0 |
1.90 |
|
0.0 |
PT |
NSPT0051 |
4.0 |
0.89 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.11 |
|
0.0 |
PT |
NSPT0052 |
12.0 |
1.20 |
0.98 |
0.0 |
PT |
incl |
6.0 |
1.44 |
|
0.0 |
PT |
NSPT0053 |
10.0 |
1.28 |
0.92 |
0.0 |
PT |
incl |
6.0 |
1.56 |
|
0.0 |
PT |
NSPT0054 |
10.0 |
1.10 |
1.72 |
0.0 |
PT |
incl |
4.0 |
1.52 |
|
0.0 |
PT |
NSPT0055 |
12.0 |
0.87 |
1.10 |
0.0 |
PT |
incl |
2.0 |
1.60 |
|
0.0 |
PT |
NSPT0056 |
10.0 |
0.93 |
1.92 |
0.0 |
PT |
incl |
2.0 |
1.43 |
|
0.0 |
PT |
NSPT0057 |
2.0 |
1.64 |
0.20 |
0.0 |
PT |
NSPT0058 |
4.6 |
1.61 |
0.46 |
0.0 |
PT |
incl |
4.0 |
1.76 |
|
0.0 |
PT |
NSPT0059 |
9.0 |
0.92 |
0.43 |
0.0 |
PT |
incl |
2.0 |
1.84 |
|
0.0 |
PT |
NSPT0001 |
10.0 |
1.28 |
1.22 |
0.0 |
PT |
incl |
4.0 |
1.49 |
|
0.0 |
PT |
NSPT0002 |
6.0 |
1.10 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.94 |
|
0.0 |
PT |
NSPT0003 |
10.0 |
1.11 |
1.04 |
0.0 |
PT |
incl |
4.0 |
1.36 |
|
0.0 |
PT |
NSPT0004 |
5.0 |
0.87 |
3.74 |
0.0 |
PT |
NSPT0005 |
10.0 |
1.19 |
0.84 |
0.0 |
PT |
incl |
4.0 |
1.40 |
|
0.0 |
PT |
NSPT0006 |
4.0 |
1.40 |
0.65 |
0.0 |
PT |
incl |
2.0 |
2.25 |
|
0.0 |
PT |
NSPT0007 |
9.0 |
1.02 |
1.10 |
0.0 |
PT |
incl |
2.0 |
1.14 |
|
7.0 |
PT |
NSPT0008 |
13.0 |
1.30 |
1.14 |
0.0 |
PT |
incl |
10.0 |
1.44 |
|
0.0 |
PT |
NSPT0009 |
12.0 |
1.25 |
1.08 |
0.0 |
PT |
incl |
8.0 |
1.36 |
|
0.0 |
PT |
NSPT0010 |
10.9 |
0.95 |
2.92 |
0.0 |
PT |
incl |
4.0 |
1.11 |
|
0.0 |
PT |
NSPT0011 |
6.0 |
0.89 |
0.27 |
0.0 |
PT |
incl |
2.0 |
1.38 |
|
0.0 |
PT |
NSPT0012 |
2.0 |
1.16 |
NSR |
0.0 |
PT |
NSPT0013 |
11.8 |
1.35 |
1.24 |
0.0 |
PT |
incl |
4.0 |
1.90 |
|
0.0 |
PT |
NSPT0014 |
10.0 |
1.18 |
0.70 |
0.0 |
PT |
incl |
4.0 |
1.92 |
|
0.0 |
PT |
NSPT0015 |
11.8 |
1.25 |
1.87 |
0.0 |
PT |
incl |
6.0 |
1.45 |
|
0.0 |
PT |
NSPT0016 |
2.0 |
1.15 |
0.20 |
0.0 |
PT |
NSPT0017 |
10.0 |
1.08 |
1.98 |
0.0 |
PT |
incl |
4.0 |
1.70 |
|
0.0 |
PT |
NSPT0018 |
5.0 |
1.36 |
0.66 |
0.0 |
PT |
incl |
2.0 |
2.45 |
|
0.0 |
PT |
NSPT0019 |
6.0 |
0.75 |
0.76 |
0.0 |
PT |
NSPT0020 |
10.0 |
0.88 |
1.74 |
0.0 |
PT |
incl |
2.0 |
1.55 |
|
0.0 |
PT |
NSPT0021 |
5.0 |
1.15 |
2.40 |
4.0 |
PT |
NSPT0023 |
10.0 |
1.49 |
0.97 |
0.0 |
PT |
incl |
4.0 |
2.01 |
|
0.0 |
PT |
NSPT0024 |
3.8 |
1.64 |
0.25 |
0.0 |
PT |
incl |
2.0 |
2.29 |
|
0.0 |
PT |
NSPT0025 |
8.0 |
1.16 |
0.93 |
0.0 |
PT |
incl |
2.0 |
1.87 |
|
0.0 |
PT |
NSPT0026 |
10.0 |
1.28 |
1.06 |
0.0 |
PT |
incl |
2.0 |
2.36 |
|
0.0 |
PT |
NSPT0027 |
4.0 |
1.46 |
0.24 |
0.0 |
PT |
incl |
2.2 |
2.09 |
|
0.0 |
PT |
NSPT0028 |
6.0 |
1.20 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.94 |
|
0.0 |
PT |
NSPT0029 |
12.0 |
1.00 |
0.89 |
0.0 |
PT |
incl |
1.4 |
2.10 |
|
0.0 |
PT |
NSPT0030 |
4.0 |
1.32 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.78 |
|
0.0 |
PT |
NSPT0031 |
3.0 |
1.03 |
NSR |
0.0 |
PT |
NSPT0032 |
11.5 |
1.00 |
1.59 |
0.0 |
PT |
incl |
2.0 |
1.90 |
|
0.0 |
PT |
NSPT0033 |
12.0 |
1.41 |
1.23 |
0.0 |
PT |
incl |
6.0 |
1.62 |
|
0.0 |
PT |
NSPT0034 |
6.0 |
1.12 |
NSR |
0.0 |
PT |
incl |
2.0 |
2.02 |
|
0.0 |
PT |
NSPT0035 |
6.0 |
0.82 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.22 |
|
0.0 |
PT |
NSPT0036 |
2.0 |
1.06 |
NSR |
0.0 |
PT |
NSPT0037 |
6.0 |
1.14 |
0.70 |
0.0 |
PT |
incl |
2.0 |
2.31 |
|
0.0 |
PT |
NSPT0038 |
10.0 |
0.93 |
0.84 |
0.0 |
PT |
incl |
2.0 |
1.20 |
|
0.0 |
PT |
NSPT0039 |
11.0 |
1.41 |
0.99 |
0.0 |
PT |
incl |
4.0 |
1.72 |
|
0.0 |
PT |
NSPT0040 |
10.0 |
1.00 |
0.80 |
0.0 |
PT |
incl |
4.0 |
1.41 |
|
0.0 |
PT |
NSPT0042 |
11.0 |
1.12 |
1.08 |
0.0 |
PT |
incl |
2.0 |
1.72 |
|
0.0 |
PT |
NSPT0043 |
13.0 |
1.17 |
1.69 |
0.0 |
PT |
incl |
8.0 |
1.31 |
|
0.0 |
PT |
incl |
2.0 |
2.02 |
|
0.0 |
PT |
NSPT0044 |
2.0 |
0.75 |
0.10 |
0.0 |
PT |
NSPT0045 |
11.0 |
1.20 |
0.60 |
0.0 |
PT |
incl |
4.0 |
1.50 |
|
0.0 |
PT |
NSPT0046 |
9.0 |
0.91 |
0.89 |
0.0 |
PT |
incl |
2.0 |
1.49 |
|
0.0 |
PT |
NSPT0047 |
12.0 |
1.01 |
2.53 |
0.0 |
PT |
incl |
8.0 |
1.17 |
|
0.0 |
PT |
NSPT0048 |
4.0 |
1.18 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.71 |
|
0.0 |
PT |
NSPT0049 |
4.0 |
1.09 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.42 |
|
0.0 |
PT |
NSPT0050 |
11.0 |
1.18 |
1.20 |
0.0 |
PT |
incl |
2.0 |
1.90 |
|
0.0 |
PT |
NSPT0051 |
4.0 |
0.89 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.11 |
|
0.0 |
PT |
NSPT0052 |
12.0 |
1.20 |
0.98 |
0.0 |
PT |
incl |
6.0 |
1.44 |
|
0.0 |
PT |
NSPT0053 |
10.0 |
1.28 |
0.92 |
0.0 |
PT |
incl |
6.0 |
1.56 |
|
0.0 |
PT |
NSPT0054 |
10.0 |
1.10 |
1.72 |
0.0 |
PT |
incl |
4.0 |
1.52 |
|
0.0 |
PT |
NSPT0055 |
12.0 |
0.87 |
1.10 |
0.0 |
PT |
incl |
2.0 |
1.60 |
|
0.0 |
PT |
NSPT0056 |
10.0 |
0.93 |
1.92 |
0.0 |
PT |
incl |
2.0 |
1.43 |
|
0.0 |
PT |
NSPT0057 |
2.0 |
1.64 |
0.20 |
0.0 |
PT |
NSPT0058 |
4.6 |
1.61 |
0.46 |
0.0 |
PT |
incl |
4.0 |
1.76 |
|
0.0 |
PT |
NSPT0059 |
9.0 |
0.92 |
0.43 |
0.0 |
PT |
incl |
2.0 |
1.84 |
|
0.0 |
PT |
NSPT0001 |
10.0 |
1.28 |
1.22 |
0.0 |
PT |
incl |
4.0 |
1.49 |
|
0.0 |
PT |
NSPT0002 |
6.0 |
1.10 |
NSR |
0.0 |
PT |
incl |
2.0 |
1.94 |
|
0.0 |
PT |
NSPT0003 |
10.0 |
1.11 |
1.04 |
0.0 |
PT |
incl |
4.0 |
1.36 |
|
0.0 |
PT |
NSPT0004 |
5.0 |
0.87 |
3.74 |
0.0 |
PT |
NSPT0005 |
10.0 |
1.19 |
0.84 |
0.0 |
PT |
incl |
4.0 |
1.40 |
|
0.0 |
PT |
NSPT0006 |
4.0 |
1.40 |
0.65 |
0.0 |
PT |
incl |
2.0 |
2.25 |
|
0.0 |
PT |
NSPT0007 |
9.0 |
1.02 |
1.10 |
0.0 |
PT |
incl |
2.0 |
1.14 |
|
7.0 |
PT |
NSPT0008 |
13.0 |
1.30 |
1.14 |
0.0 |
PT |
incl |
10.0 |
1.44 |
|
0.0 |
PT |
NSPT0009 |
12.0 |
1.25 |
1.08 |
0.0 |
PT |
incl |
8.0 |
1.36 |
|
0.0 |
PT |
NSPT0010 |
10.9 |
0.95 |
2.92 |
0.0 |
PT |
incl |
4.0 |
1.11 |
|
0.0 |
PT |
NSPT0011 |
6.0 |
0.89 |
0.27 |
0.0 |
PT |
incl |
2.0 |
1.38 |
|
0.0 |
PT |
NSPT0012 |
2.0 |
1.16 |
NSR |
0.0 |
PT |
NSPT0013 |
11.8 |
1.35 |
1.24 |
0.0 |
PT |
incl |
4.0 |
1.90 |
|
0.0 |
PT |
NSPT0014 |
10.0 |
1.18 |
0.70 |
0.0 |
PT |
incl |
4.0 |
1.92 |
|
0.0 |
PT |
NSPT0015 |
11.8 |
1.25 |
1.87 |
0.0 |
PT |
incl |
6.0 |
1.45 |
|
0.0 |
PT |
NSPT0016 |
2.0 |
1.15 |
0.20 |
0.0 |
PT |
NSPT0017 |
10.0 |
1.08 |
1.98 |
0.0 |
PT |
incl |
4.0 |
1.70 |
|
0.0 |
PT |
NSPT0018 |
5.0 |
1.36 |
0.66 |
0.0 |
PT |
incl |
2.0 |
2.45 |
|
0.0 |
PT |
APPENDIX II: DRILL HOLE COLLAR DATA - TABLE 3
Hole ID |
Easting |
Northing |
RL |
Depth |
|
Hole ID |
Easting |
Northing |
RL |
Depth |
KYHA0537 |
538799 |
8479199 |
1090 |
12 |
|
KYHA0587 |
547601 |
8476400 |
1145 |
8 |
KYHA0538 |
539001 |
8480001 |
1090 |
11 |
|
KYHA0588 |
546402 |
8476804 |
1135 |
4 |
KYHA0541 |
542401 |
8477202 |
1099 |
8 |
|
KYHA0589 |
545999 |
8476384 |
1132 |
1.7 |
KYHA0543 |
539193 |
8477995 |
1081 |
14 |
|
KYHA0590 |
546400 |
8476397 |
1138 |
1.5 |
KYHA0544 |
540808 |
8479998 |
1101 |
11 |
|
KYHA0591 |
546800 |
8476401 |
1146 |
11 |
KYHA0547 |
542804 |
8480765 |
1122 |
7 |
|
KYHA0592 |
547199 |
8476400 |
1149 |
11 |
KYHA0548 |
543233 |
8481216 |
1125 |
6 |
|
KYHA0593 |
545599 |
8476000 |
1133 |
11 |
KYHA0549 |
542798 |
8481202 |
1116 |
10 |
|
KYHA0594 |
545197 |
8475999 |
1129 |
12 |
KYHA0550 |
542473 |
8481682 |
1117 |
11 |
|
KYHA0595 |
545606 |
8475600 |
1128 |
5 |
KYHA0552 |
543210 |
8482410 |
1123 |
9 |
|
KYHA0596 |
545188 |
8475605 |
1124 |
10 |
KYHA0553 |
541999 |
8481646 |
1114 |
10 |
|
KYHA0597 |
545199 |
8475202 |
1122 |
10 |
KYHA0554 |
541156 |
8482000 |
1111 |
11 |
|
KYHA0598 |
545603 |
8475199 |
1133 |
7 |
KYHA0555 |
541650 |
8480401 |
1104 |
8 |
|
KYHA0599 |
545599 |
8474803 |
1125 |
6 |
KYHA0556 |
541604 |
8477602 |
1096 |
8 |
|
KYHA0600 |
545190 |
8474800 |
1113 |
8 |
KYHA0557 |
542842 |
8478395 |
1119 |
11 |
|
KYHA0601 |
545598 |
8474401 |
1117 |
4 |
KYHA0558 |
543609 |
8477238 |
1118 |
12 |
|
KYHA0602 |
544798 |
8474400 |
1121 |
10 |
KYHA0559 |
543982 |
8476437 |
1113 |
6 |
|
KYHA0603 |
545200 |
8474399 |
1120 |
7 |
KYHA0560 |
541599 |
8478801 |
1116 |
2 |
|
KYHA0604 |
544398 |
8474398 |
1119 |
12 |
KYHA0561 |
543613 |
8482794 |
1123 |
12 |
|
KYHA0605 |
544001 |
8474400 |
1115 |
10 |
KYHA0562 |
544024 |
8482769 |
1126 |
8 |
|
KYHA0606 |
543599 |
8474400 |
1109 |
10 |
KYHA0563 |
542002 |
8479195 |
1116 |
11 |
|
KYHA0607 |
543598 |
8474001 |
1112 |
8 |
KYHA0564 |
541799 |
8479202 |
1117 |
9 |
|
KYHA0608 |
543594 |
8473605 |
1112 |
9 |
KYHA0565 |
542400 |
8480001 |
1125 |
3 |
|
KYHA0609 |
543597 |
8473200 |
1119 |
12 |
KYHA0566 |
539397 |
8479194 |
1094 |
13 |
|
KYHA0610 |
542384 |
8473200 |
1104 |
10 |
KYHA0567 |
539998 |
8479197 |
1093 |
11 |
|
KYHA0611 |
542825 |
8473197 |
1097 |
7 |
KYHA0568 |
540597 |
8479200 |
1105 |
12 |
|
KYHA0612 |
543199 |
8473199 |
1111 |
13 |
KYHA0569 |
540798 |
8478800 |
1108 |
16 |
|
KYHA0613 |
543198 |
8472402 |
1115 |
13 |
KYHA0570 |
537999 |
8477630 |
1076 |
8 |
|
KYHA0614 |
543600 |
8472399 |
1116 |
9 |
KYHA0572 |
540431 |
8476778 |
1079 |
8 |
|
KYHA0615 |
543600 |
8472799 |
1120 |
8 |
KYHA0573 |
542814 |
8479974 |
1128 |
9 |
|
KYHA0616 |
543200 |
8472800 |
1105 |
7 |
KYHA0576 |
543209 |
8477173 |
1110 |
12 |
|
KYHA0617 |
542800 |
8472802 |
1098 |
7 |
KYHA0577 |
542402 |
8477991 |
1108 |
10 |
|
KYHA0618 |
542401 |
8472798 |
1103 |
8 |
KYHA0583 |
544803 |
8476397 |
1115 |
10 |
|
KYHA0619 |
542390 |
8472355 |
1099 |
5 |
KYHA0584 |
547199 |
8476799 |
1150 |
10 |
|
KYHA0620 |
542799 |
8472399 |
1102 |
8 |
KYHA0585 |
546829 |
8476794 |
1145 |
2 |
|
KYHA0621 |
542799 |
8472005 |
1103 |
9 |
KYHA0586 |
547602 |
8476801 |
1149 |
12 |
|
KYHA0622 |
543200 |
8484401 |
1116 |
9 |
KYHA0623 |
542800 |
8484402 |
1115 |
12 |
|
KYHA0661 |
545572 |
8482441 |
1120 |
6 |
KYHA0624 |
542001 |
8484400 |
1105 |
12 |
|
KYHA0662 |
545196 |
8481997 |
1121 |
8 |
KYHA0625 |
542401 |
8484402 |
1112 |
12 |
|
KYHA0663 |
546017 |
8481987 |
1118 |
6 |
KYHA0626 |
543601 |
8484401 |
1118 |
12 |
|
KYHA0664 |
545191 |
8481584 |
1124 |
8 |
KYHA0627 |
544002 |
8484400 |
1122 |
13 |
|
KYHA0665 |
545598 |
8481601 |
1119 |
6 |
KYHA0628 |
544398 |
8484399 |
1122 |
12 |
|
KYHA0666 |
545186 |
8481165 |
1129 |
4 |
KYHA0629 |
544800 |
8484401 |
1124 |
12 |
|
KYHA0667 |
545212 |
8480792 |
1127 |
5 |
KYHA0630 |
543600 |
8484000 |
1120 |
13 |
|
KYHA0668 |
545198 |
8480401 |
1129 |
5 |
KYHA0631 |
543201 |
8484001 |
1117 |
11 |
|
KYHA0669 |
545599 |
8481201 |
1123 |
5 |
KYHA0632 |
542798 |
8484001 |
1115 |
12 |
|
KYHA0670 |
545634 |
8480776 |
1126 |
3 |
KYHA0633 |
542402 |
8483999 |
1111 |
13 |
|
KYHA0671 |
545198 |
8480008 |
1131 |
4 |
KYHA0634 |
542000 |
8483998 |
1105 |
13 |
|
KYHA0672 |
545616 |
8480379 |
1130 |
6 |
KYHA0635 |
542400 |
8483600 |
1103 |
7 |
|
KYHA0673 |
545600 |
8480002 |
1137 |
10 |
KYHA0636 |
542801 |
8483602 |
1107 |
8 |
|
KYHA0674 |
545198 |
8479601 |
1139 |
6 |
KYHA0637 |
543208 |
8483601 |
1111 |
9 |
|
KYHA0675 |
545601 |
8479602 |
1142 |
12 |
KYHA0638 |
543201 |
8483203 |
1108 |
7 |
|
KYHA0676 |
545989 |
8482401 |
1112 |
5 |
KYHA0639 |
542798 |
8483202 |
1103 |
4 |
|
KYHA0677 |
545599 |
8481998 |
1117 |
5 |
KYHA0640 |
542402 |
8483199 |
1101 |
6 |
|
KYHA0678 |
546395 |
8482802 |
1110 |
5 |
KYHA0641 |
542401 |
8482801 |
1111 |
12 |
|
KYHA0679 |
546800 |
8482800 |
1111 |
3 |
KYHA0642 |
542798 |
8482800 |
1109 |
5 |
|
KYHA0680 |
547197 |
8482799 |
1119 |
5 |
KYHA0643 |
538009 |
8480008 |
1071 |
11 |
|
KYHA0681 |
546003 |
8483206 |
1121 |
10 |
KYHA0644 |
537607 |
8480002 |
1061 |
7 |
|
KYHA0682 |
546798 |
8483203 |
1106 |
4 |
KYHA0645 |
537200 |
8479999 |
1058 |
6 |
|
KYHA0683 |
546399 |
8483601 |
1119 |
13 |
KYHA0646 |
538405 |
8479996 |
1082 |
6 |
|
KYHA0684 |
547604 |
8483200 |
1115 |
8 |
KYHA0647 |
536806 |
8480400 |
1064 |
12 |
|
KYHA0685 |
547600 |
8482799 |
1121 |
12 |
KYHA0648 |
537204 |
8480404 |
1071 |
12 |
|
KYHA0686 |
546003 |
8483602 |
1124 |
11 |
KYHA0649 |
537600 |
8480403 |
1073 |
7 |
|
KYHA0687 |
546799 |
8483597 |
1111 |
8 |
KYHA0650 |
537601 |
8479601 |
1069 |
12 |
|
KYHA0688 |
547199 |
8483599 |
1103 |
8 |
KYHA0651 |
537115 |
8479603 |
1055 |
7 |
|
KYHA0689 |
546795 |
8484006 |
1114 |
11 |
KYHA0652 |
538399 |
8479602 |
1085 |
11 |
|
KYHA0690 |
546002 |
8483997 |
1121 |
4 |
KYHA0653 |
536796 |
8479603 |
1055 |
8 |
|
KYHA0691 |
545994 |
8484400 |
1113 |
2 |
KYHA0654 |
538002 |
8480800 |
1084 |
12 |
|
KYHA0692 |
546401 |
8484400 |
1114 |
11 |
KYHA0655 |
537605 |
8480808 |
1081 |
7 |
|
KYHA0693 |
546800 |
8484401 |
1112 |
11 |
KYHA0656 |
536830 |
8480037 |
1053 |
8 |
|
KYHA0694 |
547584 |
8483578 |
1106 |
2 |
KYHA0657 |
538005 |
8479606 |
1079 |
9 |
|
KYHA0695 |
547987 |
8483997 |
1112 |
8 |
KYHA0658 |
537961 |
8480383 |
1070 |
7 |
|
KYHA0696 |
548402 |
8483600 |
1121 |
11 |
KYHA0659 |
545600 |
8482806 |
1121 |
5 |
|
KYHA0697 |
548032 |
8483560 |
1110 |
4 |
KYHA0660 |
545895 |
8482840 |
1115 |
5 |
|
KYHA0698 |
548400 |
8484000 |
1119 |
5 |
KYHA0699 |
548400 |
8484400 |
1116 |
11 |
|
KYHA0737 |
538401 |
8471600 |
1128 |
10 |
KYHA0700 |
547651 |
8484004 |
1104 |
5 |
|
KYHA0738 |
538795 |
8471600 |
1134 |
11 |
KYHA0701 |
547594 |
8484405 |
1099 |
5 |
|
KYHA0739 |
539202 |
8471601 |
1139 |
11 |
KYHA0702 |
546800 |
8485202 |
1105 |
8 |
|
KYHA0740 |
539598 |
8471600 |
1146 |
10 |
KYHA0703 |
546800 |
8485597 |
1109 |
9 |
|
KYHA0741 |
539998 |
8471600 |
1145 |
9 |
KYHA0704 |
546804 |
8485997 |
1109 |
10 |
|
KYHA0742 |
540403 |
8471599 |
1136 |
7 |
KYHA0705 |
547198 |
8486001 |
1099 |
3 |
|
KYHA0743 |
537600 |
8471600 |
1123 |
12 |
KYHA0706 |
547193 |
8485258 |
1096 |
6 |
|
KYHA0744 |
538001 |
8471599 |
1124 |
7 |
KYHA0707 |
547596 |
8485600 |
1092 |
6 |
|
KYHA0745 |
538399 |
8471199 |
1127 |
9 |
KYHA0708 |
546828 |
8484803 |
1104 |
6 |
|
KYHA0746 |
539197 |
8471197 |
1132 |
4 |
KYHA0709 |
547561 |
8486030 |
1089 |
2 |
|
KYHA0747 |
538801 |
8470802 |
1123 |
5 |
KYHA0710 |
547997 |
8486003 |
1093 |
8 |
|
KYHA0748 |
537599 |
8472000 |
1122 |
10 |
KYHA0711 |
548400 |
8485999 |
1101 |
11 |
|
KYHA0749 |
538405 |
8472381 |
1119 |
5 |
KYHA0712 |
548797 |
8486001 |
1104 |
12 |
|
KYHA0750 |
538799 |
8472400 |
1130 |
5 |
KYHA0713 |
549196 |
8485998 |
1103 |
11 |
|
KYHA0751 |
538001 |
8472397 |
1113 |
6 |
KYHA0714 |
548400 |
8485603 |
1108 |
11 |
|
KYHA0752 |
537594 |
8472400 |
1120 |
12 |
KYHA0715 |
547686 |
8484707 |
1099 |
2 |
|
KYHA0753 |
537210 |
8472395 |
1119 |
11 |
KYHA0716 |
547636 |
8485212 |
1095 |
2 |
|
KYHA0754 |
537201 |
8471602 |
1116 |
10 |
KYHA0717 |
548008 |
8485215 |
1107 |
12 |
|
KYHA0755 |
538000 |
8470796 |
1115 |
7 |
KYHA0718 |
548396 |
8485201 |
1113 |
12 |
|
KYHA0756 |
538402 |
8470802 |
1118 |
6 |
KYHA0719 |
548800 |
8485202 |
1115 |
13 |
|
KYHA0757 |
539600 |
8470802 |
1139 |
9 |
KYHA0720 |
549199 |
8485197 |
1112 |
11 |
|
KYHA0758 |
537599 |
8471199 |
1120 |
11 |
KYHA0721 |
548405 |
8484797 |
1115 |
11 |
|
KYHA0759 |
537600 |
8470802 |
1113 |
11 |
KYHA0722 |
547190 |
8484403 |
1104 |
9 |
|
KYHA0760 |
539199 |
8470795 |
1130 |
6 |
KYHA0723 |
548026 |
8484382 |
1111 |
3 |
|
KYHA0761 |
539993 |
8470800 |
1146 |
12 |
KYHA0724 |
536398 |
8477202 |
1085 |
3 |
|
KYHA0762 |
540399 |
8472398 |
1134 |
6 |
KYHA0725 |
536006 |
8476809 |
1083 |
5 |
|
KYHA0763 |
539999 |
8471198 |
1146 |
10 |
KYHA0726 |
535998 |
8476396 |
1088 |
8 |
|
KYHA0764 |
539209 |
8470394 |
1126 |
6 |
KYHA0727 |
537601 |
8476414 |
1094 |
9.5 |
|
KYHA0765 |
538399 |
8470400 |
1115 |
5 |
KYHA0728 |
536002 |
8475600 |
1099 |
9 |
|
KYHA0766 |
539995 |
8470400 |
1144 |
14 |
KYHA0729 |
536406 |
8475603 |
1095 |
6 |
|
KYHA0767 |
538401 |
8470001 |
1120 |
8 |
KYHA0730 |
535999 |
8475992 |
1090 |
4 |
|
KYHA0768 |
539599 |
8470005 |
1140 |
12 |
KYHA0731 |
536786 |
8475625 |
1100 |
11 |
|
KYHA0769 |
539197 |
8470002 |
1136 |
12 |
KYHA0732 |
538799 |
8473199 |
1113 |
2.5 |
|
KYHA0770 |
538798 |
8469996 |
1130 |
12 |
KYHA0733 |
539201 |
8473200 |
1118 |
6 |
|
KYHA0771 |
539203 |
8469598 |
1143 |
10 |
KYHA0734 |
537601 |
8472801 |
1116 |
10 |
|
KYHA0772 |
539203 |
8469198 |
1146 |
14 |
KYHA0735 |
538351 |
8472823 |
1114 |
2.7 |
|
KYHA0773 |
538801 |
8469198 |
1137 |
15 |
KYHA0736 |
538400 |
8471999 |
1123 |
4 |
|
KYHA0774 |
538400 |
8469202 |
1130 |
4 |
KYHA0775 |
538396 |
8469598 |
1122 |
3 |
|
KYHA0813 |
549597 |
8479214 |
1128 |
3 |
KYHA0776 |
539601 |
8474794 |
1112 |
13 |
|
KYHA0814 |
550001 |
8479198 |
1119 |
6 |
KYHA0777 |
540402 |
8474801 |
1110 |
8 |
|
KYHA0815 |
549565 |
8478793 |
1121 |
6 |
KYHA0778 |
541204 |
8474801 |
1104 |
5 |
|
KYHA0816 |
547999 |
8477602 |
1143 |
12 |
KYHA0779 |
541600 |
8474801 |
1099 |
8 |
|
KYHA0816 |
547999 |
8477602 |
1143 |
12 |
KYHA0780 |
540799 |
8474795 |
1106 |
5 |
|
KYHA0817 |
548003 |
8477202 |
1145 |
12 |
KYHA0781 |
539200 |
8474400 |
1113 |
11 |
|
KYHA0818 |
548399 |
8478798 |
1144 |
12 |
KYHA0782 |
541599 |
8474401 |
1105 |
6 |
|
KYHA0819 |
548026 |
8476793 |
1142 |
10 |
KYHA0783 |
541599 |
8474001 |
1110 |
12 |
|
KYHA0820 |
547999 |
8476402 |
1139 |
8 |
KYHA0784 |
540797 |
8474399 |
1115 |
12 |
|
KYHA0821 |
546399 |
8479201 |
1140 |
5 |
KYHA0785 |
540799 |
8473601 |
1118 |
12 |
|
KYHA0822 |
545998 |
8479199 |
1145 |
11 |
KYHA0786 |
540802 |
8473200 |
1117 |
7 |
|
KYHA0823 |
545598 |
8479198 |
1147 |
13 |
KYHA0787 |
540798 |
8474001 |
1119 |
13 |
|
KYHA0824 |
545198 |
8479199 |
1145 |
11 |
KYHA0788 |
541200 |
8473998 |
1114 |
12 |
|
KYHA0825 |
546827 |
8479182 |
1145 |
11 |
KYHA0789 |
540399 |
8473200 |
1122 |
8 |
|
KYHA0826 |
547199 |
8477600 |
1149 |
13 |
KYHA0790 |
540799 |
8472802 |
1122 |
5 |
|
KYHA0827 |
545203 |
8478802 |
1147 |
13 |
KYHA0791 |
539998 |
8473200 |
1129 |
11 |
|
KYHA0828 |
545598 |
8478803 |
1148 |
11 |
KYHA0792 |
541199 |
8473202 |
1116 |
8 |
|
KYHA0829 |
545999 |
8478801 |
1147 |
12 |
KYHA0793 |
541554 |
8473602 |
1114 |
3 |
|
KYHA0830 |
546401 |
8478801 |
1148 |
13 |
KYHA0794 |
541588 |
8472783 |
1121 |
10 |
|
KYHA0831 |
546799 |
8478801 |
1150 |
10 |
KYHA0795 |
541599 |
8473200 |
1119 |
13 |
|
KYHA0832 |
546800 |
8478400 |
1153 |
13 |
KYHA0796 |
541997 |
8472799 |
1115 |
11 |
|
KYHA0833 |
547600 |
8478000 |
1139 |
9 |
KYHA0797 |
542848 |
8474005 |
1095 |
7 |
|
KYHA0834 |
547996 |
8478001 |
1136 |
9 |
KYHA0798 |
546803 |
8477198 |
1148 |
11 |
|
KYHA0835 |
549585 |
8478449 |
1121 |
2 |
KYHA0799 |
547202 |
8477200 |
1151 |
12 |
|
KYHA0836 |
549198 |
8478387 |
1129 |
8 |
KYHA0800 |
547600 |
8477200 |
1151 |
12 |
|
KYHA0837 |
548799 |
8478402 |
1136 |
12 |
KYHA0801 |
547600 |
8477602 |
1147 |
12 |
|
KYHA0838 |
548400 |
8478399 |
1140 |
12 |
KYHA0802 |
547603 |
8479612 |
1145 |
11 |
|
KYHA0839 |
548000 |
8478400 |
1143 |
12 |
KYHA0803 |
548401 |
8479201 |
1142 |
12 |
|
KYHA0840 |
547639 |
8478437 |
1147 |
13 |
KYHA0804 |
549199 |
8479602 |
1132 |
11 |
|
KYHA0842 |
547603 |
8478800 |
1152 |
13 |
KYHA0805 |
549201 |
8479202 |
1133 |
11 |
|
KYHA0843 |
546000 |
8478398 |
1147 |
13 |
KYHA0806 |
548400 |
8479601 |
1134 |
4 |
|
KYHA0844 |
546400 |
8478400 |
1150 |
13 |
KYHA0807 |
548003 |
8479197 |
1145 |
10 |
|
KYHA0845 |
545599 |
8478401 |
1146 |
10 |
KYHA0808 |
547596 |
8479197 |
1149 |
9 |
|
KYHA0846 |
545199 |
8478397 |
1144 |
12 |
KYHA0809 |
547203 |
8479202 |
1150 |
12 |
|
KYHA0847 |
546001 |
8477999 |
1141 |
8 |
KYHA0810 |
549202 |
8478796 |
1129 |
4 |
|
KYHA0848 |
545603 |
8477999 |
1137 |
8 |
KYHA0811 |
548799 |
8479198 |
1138 |
12 |
|
KYHA0849 |
545202 |
8478002 |
1137 |
13 |
KYHA0812 |
550000 |
8479598 |
1123 |
10 |
|
KYHA0850 |
545201 |
8477602 |
1126 |
10 |
KYHA0851 |
545602 |
8477601 |
1129 |
9 |
|
KYHA0889 |
554393 |
8488399 |
1117 |
7 |
KYHA0852 |
544001 |
8475595 |
1111 |
8 |
|
KYHA0890 |
554000 |
8488399 |
1119 |
10 |
KYHA0853 |
544398 |
8475603 |
1116 |
9 |
|
KYHA0891 |
553602 |
8488399 |
1117 |
8 |
KYHA0854 |
544802 |
8475601 |
1120 |
11 |
|
KYHA0892 |
554002 |
8488003 |
1125 |
12 |
KYHA0855 |
543979 |
8475206 |
1105 |
8 |
|
KYHA0893 |
553599 |
8488001 |
1124 |
13 |
KYHA0856 |
544399 |
8475200 |
1110 |
8 |
|
KYHA0894 |
553200 |
8488003 |
1123 |
12 |
KYHA0857 |
544819 |
8475194 |
1114 |
6 |
|
KYHA0895 |
553198 |
8488400 |
1118 |
10 |
KYHA0858 |
544000 |
8475999 |
1104 |
6 |
|
KYHA0896 |
552799 |
8488402 |
1120 |
13 |
KYHA0859 |
544399 |
8476002 |
1112 |
8 |
|
KYHA0897 |
552399 |
8488001 |
1121 |
12 |
KYHA0860 |
544800 |
8476004 |
1122 |
11 |
|
KYHA0889 |
554393 |
8488399 |
1117 |
7 |
KYHA0861 |
544799 |
8474803 |
1107 |
5 |
|
KYHA0890 |
554000 |
8488399 |
1119 |
10 |
KYHA0862 |
544402 |
8474799 |
1106 |
7 |
|
KYHA0891 |
553602 |
8488399 |
1117 |
8 |
KYHA0863 |
544000 |
8474803 |
1103 |
5 |
|
KYHA0892 |
554002 |
8488003 |
1125 |
12 |
KYHA0864 |
543598 |
8474802 |
1098 |
7 |
|
KYHA0893 |
553599 |
8488001 |
1124 |
13 |
KYHA0865 |
543200 |
8474801 |
1091 |
5 |
|
KYHA0894 |
553200 |
8488003 |
1123 |
12 |
KYHA0866 |
542826 |
8474786 |
1086 |
6 |
|
KYHA0895 |
553198 |
8488400 |
1118 |
10 |
KYHA0867 |
542799 |
8473598 |
1098 |
11 |
|
KYHA0896 |
552799 |
8488402 |
1120 |
13 |
KYHA0868 |
543190 |
8473603 |
1109 |
13 |
|
KYHA0897 |
552399 |
8488001 |
1121 |
12 |
KYHA0869 |
543188 |
8473995 |
1108 |
8 |
|
KYPT0185 |
542230 |
8481487 |
1111 |
6.0 |
KYHA0870 |
543200 |
8474403 |
1103 |
8 |
|
KYPT0186 |
542543 |
8481323 |
1113 |
7.0 |
KYHA0871 |
551604 |
8486804 |
1094 |
10 |
|
KYPT0187 |
539800 |
8474400 |
1121 |
13.0 |
KYHA0872 |
552000 |
8486804 |
1089 |
7 |
|
KYPT0189 |
544957 |
8480648 |
1133 |
6.0 |
KYHA0873 |
551199 |
8486799 |
1102 |
13 |
|
KYPT0190 |
539801 |
8474000 |
1126 |
14.0 |
KYHA0874 |
551199 |
8487198 |
1107 |
11 |
|
KYPT0191 |
540203 |
8474400 |
1121 |
12.0 |
KYHA0875 |
551600 |
8487199 |
1108 |
11 |
|
KYPT0192 |
539401 |
8474000 |
1120 |
14.0 |
KYHA0876 |
552002 |
8487200 |
1108 |
12 |
|
KYPT0193 |
540201 |
8474002 |
1125 |
13.0 |
KYHA0877 |
552397 |
8487201 |
1110 |
12 |
|
KYPT0194 |
539802 |
8473602 |
1127 |
12.0 |
KYHA0878 |
552799 |
8487202 |
1109 |
13 |
|
KYPT0195 |
539799 |
8473200 |
1130 |
13.0 |
KYHA0879 |
553211 |
8487215 |
1110 |
7 |
|
KYPT0196 |
539399 |
8473598 |
1122 |
10.0 |
KYHA0880 |
554000 |
8487602 |
1127 |
12 |
|
KYPT0197 |
539400 |
8473200 |
1124 |
10.0 |
KYHA0881 |
553600 |
8487598 |
1125 |
12 |
|
KYPT0198 |
539798 |
8472799 |
1138 |
14.0 |
KYHA0882 |
553197 |
8487601 |
1122 |
11 |
|
KYPT0199 |
538998 |
8472802 |
1126 |
12.0 |
KYHA0883 |
552797 |
8487600 |
1120 |
12 |
|
KYPT0200 |
538999 |
8472399 |
1135 |
14.0 |
KYHA0884 |
552399 |
8487603 |
1119 |
11 |
|
KYPT0201 |
539800 |
8472398 |
1146 |
14.0 |
KYHA0885 |
552801 |
8488002 |
1123 |
12 |
|
KYPT0202 |
539391 |
8472807 |
1133 |
7.7 |
KYHA0886 |
551995 |
8487600 |
1115 |
13 |
|
KYPT0203 |
539537 |
8472406 |
1153 |
7.6 |
KYHA0887 |
551600 |
8487598 |
1111 |
12 |
|
KYPT0204 |
540198 |
8472003 |
1141 |
11.0 |
KYHA0888 |
551199 |
8487598 |
1108 |
12 |
|
KYPT0205 |
539798 |
8471997 |
1149 |
13.0 |
KYPT0206 |
539400 |
8471971 |
1152 |
4.9 |
|
NSHA0161 |
545999 |
8461101 |
1196 |
12 |
KYPT0207 |
540198 |
8472800 |
1133 |
12.0 |
|
NSHA0162 |
547601 |
8461100 |
1189 |
11 |
KYPT0208 |
540202 |
8472397 |
1138 |
9.7 |
|
NSHA0163 |
548002 |
8461103 |
1177 |
5 |
KYPT0209 |
539001 |
8472001 |
1138 |
13.0 |
|
NSHA0164 |
548400 |
8454003 |
1205 |
8 |
KYPT0210 |
537000 |
8477800 |
1085 |
11.0 |
|
NSHA0165 |
548799 |
8454004 |
1215 |
10 |
KYPT0212 |
537000 |
8477400 |
1089 |
10.8 |
|
NSHA0166 |
549201 |
8454000 |
1221 |
9 |
KYPT0213 |
537400 |
8477400 |
1089 |
11.0 |
|
NSHA0167 |
549604 |
8454000 |
1212 |
12 |
KYPT0214 |
537400 |
8477000 |
1093 |
10.8 |
|
NSHA0168 |
550001 |
8453999 |
1200 |
13 |
KYPT0215 |
537000 |
8477000 |
1092 |
11.0 |
|
NSHA0169 |
550397 |
8454004 |
1188 |
5 |
KYPT0216 |
537400 |
8477800 |
1083 |
10.3 |
|
NSHA0170 |
551608 |
8454005 |
1181 |
7 |
KYPT0217 |
537800 |
8477800 |
1075 |
7.4 |
|
NSHA0171 |
552001 |
8453999 |
1177 |
7 |
KYPT0218 |
537000 |
8476600 |
1097 |
10.0 |
|
NSHA0172 |
552810 |
8453996 |
1185 |
10 |
KYPT0219 |
543802 |
8472199 |
1121 |
3.2 |
|
NSHA0173 |
553199 |
8454000 |
1188 |
12 |
KYPT0220 |
543401 |
8472201 |
1120 |
12.0 |
|
NSHA0174 |
553597 |
8454010 |
1189 |
11 |
KYPT0221 |
543000 |
8472199 |
1113 |
9.0 |
|
NSHA0175 |
553999 |
8454000 |
1186 |
12 |
NSHA0138 |
546000 |
8462202 |
1182 |
4 |
|
NSHA0176 |
554398 |
8454001 |
1181 |
10 |
NSHA0139 |
546400 |
8462201 |
1186 |
11 |
|
NSHA0177 |
549200 |
8449598 |
1233 |
13 |
NSHA0140 |
546801 |
8462200 |
1183 |
6 |
|
NSHA0178 |
549599 |
8449599 |
1241 |
7 |
NSHA0141 |
547202 |
8462207 |
1188 |
13 |
|
NSHA0179 |
550000 |
8449601 |
1231 |
12 |
NSHA0142 |
547600 |
8462202 |
1191 |
13 |
|
NSHA0180 |
550399 |
8449568 |
1224 |
9 |
NSHA0143 |
548000 |
8462202 |
1191 |
11 |
|
NSHA0181 |
550801 |
8449598 |
1222 |
13 |
NSHA0144 |
548401 |
8462203 |
1186 |
10 |
|
NSHA0182 |
551200 |
8449600 |
1216 |
9 |
NSHA0145 |
548799 |
8462199 |
1182 |
11 |
|
NSHA0183 |
551606 |
8449623 |
1212 |
11 |
NSHA0146 |
549193 |
8462180 |
1179 |
12 |
|
NSHA0184 |
546799 |
8475600 |
1152 |
12 |
NSHA0147 |
549600 |
8462200 |
1175 |
13 |
|
NSHA0185 |
546399 |
8475000 |
1142 |
11 |
NSHA0148 |
549999 |
8462205 |
1175 |
10 |
|
NSHA0186 |
546800 |
8475000 |
1146 |
10 |
NSHA0149 |
547400 |
8457800 |
1186 |
12 |
|
NSHA0187 |
546399 |
8474398 |
1127 |
6 |
NSHA0150 |
547800 |
8457802 |
1190 |
10 |
|
NSHA0188 |
546801 |
8474401 |
1135 |
7 |
NSHA0151 |
548199 |
8457800 |
1199 |
12 |
|
NSHA0189 |
546399 |
8475601 |
1146 |
13 |
NSHA0152 |
548596 |
8457796 |
1202 |
13 |
|
NSHA0190 |
548799 |
8475603 |
1139 |
5 |
NSHA0153 |
549001 |
8457798 |
1198 |
8 |
|
NSHA0191 |
549202 |
8475597 |
1137 |
7 |
NSHA0154 |
549400 |
8457798 |
1193 |
8 |
|
NSHA0192 |
549602 |
8475598 |
1141 |
10 |
NSHA0155 |
549800 |
8457801 |
1189 |
8 |
|
NSHA0193 |
548800 |
8475000 |
1141 |
6 |
NSHA0156 |
546799 |
8461100 |
1199 |
11 |
|
NSHA0194 |
549195 |
8474997 |
1146 |
11 |
NSHA0157 |
547200 |
8461097 |
1197 |
11 |
|
NSHA0195 |
549600 |
8474998 |
1151 |
11 |
NSHA0158 |
545199 |
8461099 |
1184 |
12 |
|
NSHA0196 |
549601 |
8474400 |
1157 |
11 |
NSHA0159 |
546399 |
8461098 |
1198 |
12 |
|
NSHA0197 |
549199 |
8474399 |
1152 |
10 |
NSHA0160 |
545601 |
8461099 |
1191 |
12 |
|
NSHA0198 |
548800 |
8474400 |
1144 |
6 |
NSHA0199 |
549201 |
8473595 |
1158 |
12 |
|
NSHA0237 |
546400 |
8463400 |
1181 |
14 |
NSHA0200 |
544405 |
8472007 |
1129 |
11 |
|
NSHA0238 |
546801 |
8463399 |
1173 |
2 |
NSHA0201 |
548001 |
8470000 |
1146 |
4 |
|
NSHA0239 |
547199 |
8463400 |
1170 |
12 |
NSHA0202 |
548398 |
8470000 |
1153 |
9 |
|
NSHA0240 |
547568 |
8463402 |
1180 |
10 |
NSHA0203 |
549199 |
8470001 |
1172 |
11 |
|
NSHA0241 |
548000 |
8463398 |
1185 |
13 |
NSHA0204 |
550000 |
8470000 |
1181 |
3 |
|
NSHA0242 |
548400 |
8463399 |
1181 |
9 |
NSHA0205 |
550800 |
8469997 |
1183 |
13 |
|
NSHA0243 |
548800 |
8463400 |
1174 |
12 |
NSHA0206 |
551599 |
8470003 |
1183 |
10 |
|
NSHA0244 |
549200 |
8463400 |
1166 |
7 |
NSHA0207 |
552399 |
8470001 |
1180 |
11 |
|
NSHA0245 |
549600 |
8463400 |
1162 |
6 |
NSHA0208 |
549200 |
8466799 |
1173 |
5 |
|
NSHA0246 |
550000 |
8463400 |
1162 |
7 |
NSHA0209 |
548800 |
8466797 |
1179 |
13 |
|
NSHA0247 |
549198 |
8464401 |
1170 |
12 |
NSHA0210 |
548398 |
8466797 |
1182 |
16 |
|
NSHA0248 |
548800 |
8464401 |
1175 |
11 |
NSHA0211 |
548001 |
8466805 |
1182 |
9 |
|
NSHA0249 |
548400 |
8464399 |
1180 |
12 |
NSHA0212 |
548000 |
8468400 |
1151 |
5 |
|
NSHA0250 |
548000 |
8464403 |
1181 |
14 |
NSHA0213 |
548401 |
8468401 |
1155 |
7 |
|
NSHA0251 |
549999 |
8464400 |
1157 |
8 |
NSHA0214 |
547998 |
8469199 |
1150 |
10 |
|
NSHA0252 |
549600 |
8464401 |
1165 |
10 |
NSHA0215 |
548396 |
8469200 |
1153 |
8 |
|
NSHA0253 |
547601 |
8464400 |
1174 |
9 |
NSHA0216 |
540399 |
8469200 |
1151 |
12 |
|
NSHA0254 |
547201 |
8464398 |
1164 |
5 |
NSHA0217 |
541201 |
8469198 |
1139 |
12 |
|
NSHA0255 |
546779 |
8464397 |
1165 |
9 |
NSHA0218 |
540401 |
8466798 |
1153 |
13 |
|
NSHA0256 |
546400 |
8464401 |
1173 |
10 |
NSHA0219 |
540801 |
8467600 |
1152 |
12 |
|
NSHA0257 |
546000 |
8464400 |
1174 |
11 |
NSHA0220 |
548001 |
8467597 |
1163 |
9 |
|
NSHA0258 |
545601 |
8464404 |
1171 |
15 |
NSHA0221 |
544402 |
8465999 |
1159 |
8 |
|
NSHA0259 |
545201 |
8464403 |
1161 |
6 |
NSHA0222 |
545199 |
8465992 |
1157 |
11 |
|
NSHA0260 |
544800 |
8464400 |
1155 |
8 |
NSHA0223 |
546000 |
8465200 |
1168 |
11 |
|
NSHA0261 |
544000 |
8471998 |
1125 |
12 |
NSHA0224 |
545600 |
8465201 |
1169 |
10 |
|
NSHA0262 |
543600 |
8471998 |
1122 |
13 |
NSHA0225 |
545200 |
8465200 |
1165 |
12 |
|
NSHA0263 |
543199 |
8471997 |
1119 |
9 |
NSHA0226 |
544801 |
8465185 |
1159 |
14 |
|
NSHA0264 |
547200 |
8476000 |
1150 |
12 |
NSHA0227 |
544400 |
8465200 |
1155 |
10 |
|
NSHA0265 |
546800 |
8476000 |
1150 |
12 |
NSHA0228 |
541999 |
8464799 |
1157 |
12 |
|
NSHA0266 |
546400 |
8476000 |
1145 |
12 |
NSHA0229 |
542401 |
8464802 |
1155 |
13 |
|
NSHA0267 |
546000 |
8476000 |
1136 |
10 |
NSHA0230 |
542800 |
8464800 |
1150 |
10 |
|
NSHA0268 |
546000 |
8475600 |
1137 |
3 |
NSHA0231 |
542800 |
8464001 |
1159 |
12 |
|
NSHA0269 |
544400 |
8473997 |
1127 |
11 |
NSHA0232 |
543199 |
8464003 |
1151 |
8 |
|
NSHA0270 |
544000 |
8474000 |
1120 |
4 |
NSHA0233 |
544782 |
8463403 |
1164 |
10 |
|
NSHA0271 |
548400 |
8476000 |
1146 |
12 |
NSHA0234 |
545200 |
8463401 |
1172 |
13 |
|
NSHA0272 |
548000 |
8476000 |
1147 |
11 |
NSHA0235 |
545600 |
8463400 |
1178 |
13 |
|
NSHA0273 |
547600 |
8476000 |
1145 |
9 |
NSHA0236 |
546000 |
8463397 |
1182 |
11 |
|
NSHA0274 |
547203 |
8473987 |
1147 |
8 |
NSHA0275 |
547600 |
8474000 |
1156 |
12 |
|
NSHA0313 |
546800 |
8468830 |
1151 |
11 |
NSHA0276 |
548000 |
8473999 |
1153 |
10 |
|
NSHA0314 |
547200 |
8468000 |
1162 |
11 |
NSHA0277 |
548000 |
8473200 |
1163 |
11 |
|
NSHA0315 |
546801 |
8467998 |
1166 |
13 |
NSHA0278 |
547600 |
8473200 |
1165 |
13 |
|
NSHA0316 |
546400 |
8468000 |
1165 |
12 |
NSHA0279 |
547600 |
8472401 |
1170 |
13 |
|
NSHA0317 |
546000 |
8467999 |
1158 |
12 |
NSHA0280 |
547201 |
8472401 |
1164 |
12 |
|
NSHA0318 |
545601 |
8468000 |
1150 |
12 |
NSHA0281 |
547187 |
8471608 |
1157 |
5 |
|
NSHA0319 |
547187 |
8468800 |
1151 |
3 |
NSHA0282 |
547599 |
8471603 |
1166 |
12 |
|
NSHA0320 |
542000 |
8468800 |
1136 |
6 |
NSHA0283 |
548000 |
8471599 |
1169 |
12 |
|
NSHA0321 |
542400 |
8468798 |
1139 |
13 |
NSHA0284 |
547202 |
8470398 |
1154 |
11 |
|
NSHA0322 |
542802 |
8468801 |
1134 |
13 |
NSHA0285 |
547600 |
8470400 |
1155 |
12 |
|
NSHA0323 |
543241 |
8468800 |
1123 |
8 |
NSHA0286 |
548000 |
8470800 |
1160 |
12 |
|
NSHA0324 |
543602 |
8468799 |
1120 |
10 |
NSHA0287 |
544400 |
8473200 |
1133 |
12 |
|
NSHA0325 |
547600 |
8468000 |
1155 |
8 |
NSHA0288 |
544400 |
8472400 |
1127 |
11 |
|
NSHA0326 |
542802 |
8467999 |
1135 |
11 |
NSHA0289 |
544400 |
8471600 |
1124 |
10 |
|
NSHA0327 |
542400 |
8468002 |
1142 |
11 |
NSHA0290 |
544001 |
8471199 |
1112 |
8 |
|
NSHA0328 |
542000 |
8468003 |
1147 |
11 |
NSHA0291 |
544401 |
8471131 |
1111 |
9 |
|
NSHA0329 |
541599 |
8468005 |
1147 |
15 |
NSHA0292 |
542847 |
8471200 |
1100 |
6 |
|
NSHA0330 |
541200 |
8467200 |
1157 |
12 |
NSHA0293 |
543200 |
8471200 |
1113 |
12 |
|
NSHA0331 |
541602 |
8467201 |
1154 |
9 |
NSHA0294 |
543609 |
8471250 |
1108 |
9 |
|
NSHA0332 |
542000 |
8467203 |
1145 |
8 |
NSHA0295 |
543198 |
8470399 |
1116 |
11 |
|
NSHA0333 |
542001 |
8466402 |
1142 |
10 |
NSHA0296 |
543599 |
8470398 |
1110 |
7 |
|
NSHA0334 |
541596 |
8466401 |
1146 |
7 |
NSHA0297 |
544000 |
8470400 |
1124 |
12 |
|
NSHA0335 |
541204 |
8466401 |
1156 |
11 |
NSHA0298 |
544400 |
8470400 |
1125 |
9 |
|
NSHA0336 |
546400 |
8467200 |
1166 |
13 |
NSHA0299 |
544399 |
8470797 |
1120 |
8 |
|
NSHA0337 |
546800 |
8467200 |
1169 |
13 |
NSHA0300 |
542800 |
8470398 |
1118 |
11 |
|
NSHA0338 |
545994 |
8467209 |
1159 |
12 |
NSHA0301 |
544400 |
8470001 |
1130 |
11 |
|
NSHA0339 |
545627 |
8467229 |
1152 |
9 |
NSHA0302 |
542402 |
8469600 |
1131 |
12 |
|
NSHA0340 |
545201 |
8467201 |
1140 |
7 |
NSHA0303 |
542800 |
8469600 |
1131 |
12 |
|
NSHA0341 |
544784 |
8467160 |
1145 |
3 |
NSHA0304 |
543200 |
8469600 |
1127 |
13 |
|
NSHA0342 |
545199 |
8468001 |
1138 |
7 |
NSHA0305 |
543587 |
8469601 |
1113 |
8 |
|
NSHA0343 |
544800 |
8467996 |
1137 |
7 |
NSHA0306 |
544000 |
8469600 |
1127 |
13 |
|
NSHA0344 |
544399 |
8467998 |
1143 |
12 |
NSHA0307 |
544400 |
8469600 |
1132 |
14 |
|
NSHA0345 |
544002 |
8468004 |
1141 |
10 |
NSHA0308 |
544797 |
8469189 |
1129 |
11 |
|
NSHA0346 |
544400 |
8467201 |
1149 |
12 |
NSHA0309 |
544771 |
8469609 |
1128 |
6 |
|
NSHA0347 |
544001 |
8467201 |
1147 |
13 |
NSHA0310 |
544800 |
8468834 |
1130 |
8 |
|
NSHA0348 |
543600 |
8467202 |
1141 |
9 |
NSHA0311 |
544400 |
8468800 |
1138 |
12 |
|
NSHA0349 |
543201 |
8467200 |
1130 |
6 |
NSHA0312 |
543999 |
8468804 |
1133 |
9 |
|
NSHA0350 |
543601 |
8468001 |
1132 |
11 |
NSHA0351 |
543200 |
8467999 |
1123 |
6 |
|
NSHA0389 |
549126 |
8474770 |
1145 |
10 |
NSHA0352 |
543203 |
8466395 |
1137 |
11 |
|
NSHA0390 |
548800 |
8474800 |
1142 |
10 |
NSHA0353 |
543609 |
8466406 |
1146 |
13 |
|
NSHA0391 |
545999 |
8474800 |
1135 |
11 |
NSHA0354 |
543999 |
8466401 |
1153 |
13 |
|
NSHA0392 |
546400 |
8474800 |
1136 |
11 |
NSHA0355 |
544399 |
8466400 |
1156 |
13 |
|
NSHA0393 |
546773 |
8474772 |
1139 |
9 |
NSHA0356 |
544802 |
8466400 |
1154 |
13 |
|
NSHA0394 |
547202 |
8474801 |
1150 |
10 |
NSHA0357 |
545201 |
8466399 |
1147 |
8 |
|
NSHA0395 |
543998 |
8473200 |
1126 |
11 |
NSHA0358 |
545600 |
8466400 |
1147 |
6 |
|
NSHA0396 |
545982 |
8474427 |
1123 |
7 |
NSHA0359 |
545997 |
8466401 |
1147 |
6 |
|
NSHA0397 |
544023 |
8472412 |
1123 |
7 |
NSHA0360 |
546001 |
8465998 |
1152 |
9 |
|
NSHA0389 |
549126 |
8474770 |
1145 |
10 |
NSHA0361 |
544398 |
8465601 |
1159 |
12 |
|
NSHA0390 |
548800 |
8474800 |
1142 |
10 |
NSHA0362 |
544802 |
8465600 |
1162 |
10 |
|
NSHA0391 |
545999 |
8474800 |
1135 |
11 |
NSHA0363 |
545200 |
8465600 |
1163 |
13 |
|
NSHA0392 |
546400 |
8474800 |
1136 |
11 |
NSHA0364 |
545600 |
8465601 |
1164 |
12 |
|
NSHA0393 |
546773 |
8474772 |
1139 |
9 |
NSHA0365 |
546003 |
8465600 |
1162 |
10 |
|
NSHA0394 |
547202 |
8474801 |
1150 |
10 |
NSHA0366 |
545198 |
8464801 |
1162 |
11 |
|
NSHA0395 |
543998 |
8473200 |
1126 |
11 |
NSHA0367 |
545600 |
8464799 |
1170 |
13 |
|
NSHA0396 |
545982 |
8474427 |
1123 |
7 |
NSHA0368 |
545997 |
8464800 |
1172 |
13 |
|
NSHA0397 |
544023 |
8472412 |
1123 |
7 |
NSHA0369 |
542001 |
8464399 |
1164 |
12 |
|
NSPT0001 |
543800 |
8471801 |
1124 |
11.0 |
NSHA0370 |
542398 |
8464404 |
1161 |
12 |
|
NSPT0002 |
544599 |
8472201 |
1131 |
11.4 |
NSHA0371 |
542799 |
8464405 |
1155 |
13 |
|
NSPT0003 |
544598 |
8471799 |
1130 |
10.0 |
NSHA0372 |
545999 |
8475202 |
1141 |
12 |
|
NSPT0004 |
544600 |
8471399 |
1121 |
6.0 |
NSHA0373 |
546401 |
8475199 |
1145 |
13 |
|
NSPT0005 |
544200 |
8471801 |
1126 |
10.0 |
NSHA0374 |
546802 |
8475201 |
1149 |
12 |
|
NSPT0006 |
544208 |
8471458 |
1116 |
5.0 |
NSHA0375 |
547198 |
8475200 |
1154 |
12 |
|
NSPT0007 |
544200 |
8472202 |
1126 |
9.0 |
NSHA0376 |
547610 |
8475181 |
1157 |
9 |
|
NSPT0008 |
543399 |
8471803 |
1121 |
13.0 |
NSHA0377 |
547999 |
8475199 |
1154 |
12 |
|
NSPT0009 |
543399 |
8471399 |
1117 |
12.9 |
NSHA0378 |
548398 |
8475199 |
1144 |
6 |
|
NSPT0010 |
544198 |
8470599 |
1125 |
10.9 |
NSHA0379 |
548801 |
8475201 |
1140 |
7 |
|
NSPT0011 |
544200 |
8469400 |
1132 |
12.6 |
NSHA0380 |
549201 |
8475199 |
1143 |
7 |
|
NSPT0012 |
544600 |
8469400 |
1132 |
10.0 |
NSHA0381 |
549599 |
8475200 |
1148 |
12 |
|
NSPT0013 |
544202 |
8469000 |
1135 |
12.0 |
NSHA0382 |
546790 |
8469552 |
1134 |
4 |
|
NSPT0014 |
544201 |
8468600 |
1138 |
11.0 |
NSHA0383 |
547195 |
8469582 |
1137 |
6 |
|
NSPT0015 |
544200 |
8468201 |
1141 |
11.8 |
NSHA0384 |
547601 |
8469602 |
1140 |
8 |
|
NSPT0016 |
542999 |
8471800 |
1112 |
11.0 |
NSHA0385 |
549599 |
8474800 |
1153 |
13 |
|
NSPT0017 |
544200 |
8467800 |
1144 |
11.0 |
NSHA0386 |
547601 |
8474798 |
1157 |
10 |
|
NSPT0018 |
543799 |
8471402 |
1113 |
5.0 |
NSHA0387 |
548000 |
8474800 |
1155 |
12 |
|
NSPT0019 |
544204 |
8467403 |
1147 |
13.0 |
NSHA0388 |
548400 |
8474800 |
1147 |
10 |
|
NSPT0020 |
544594 |
8469000 |
1135 |
11.0 |
NSPT0021 |
543800 |
8467398 |
1142 |
10.0 |
|
NSPT0042 |
547002 |
8474993 |
1149 |
11.0 |
NSPT0023 |
543801 |
8467800 |
1140 |
10.0 |
|
NSPT0043 |
547403 |
8474998 |
1155 |
13.0 |
NSPT0024 |
544595 |
8468604 |
1137 |
9.0 |
|
NSPT0044 |
546223 |
8475008 |
1141 |
13.7 |
NSPT0025 |
543800 |
8468201 |
1136 |
9.0 |
|
NSPT0045 |
547005 |
8475798 |
1152 |
11.0 |
NSPT0026 |
544589 |
8468199 |
1141 |
10.0 |
|
NSPT0046 |
546597 |
8475000 |
1143 |
9.0 |
NSPT0027 |
543794 |
8468605 |
1129 |
4.0 |
|
NSPT0047 |
546601 |
8475399 |
1149 |
13.0 |
NSPT0028 |
545801 |
8465000 |
1170 |
12.0 |
|
NSPT0048 |
547399 |
8474600 |
1154 |
12.0 |
NSPT0029 |
545400 |
8465000 |
1167 |
12.5 |
|
NSPT0049 |
547001 |
8475400 |
1152 |
12.0 |
NSPT0030 |
545000 |
8465400 |
1162 |
11.0 |
|
NSPT0050 |
547403 |
8475401 |
1155 |
12.0 |
NSPT0031 |
545001 |
8465001 |
1160 |
7.0 |
|
NSPT0051 |
546989 |
8474606 |
1141 |
8.0 |
NSPT0032 |
545800 |
8465401 |
1167 |
10.5 |
|
NSPT0052 |
547802 |
8475398 |
1155 |
12.0 |
NSPT0033 |
545400 |
8465400 |
1166 |
13.0 |
|
NSPT0053 |
547799 |
8474602 |
1158 |
13.0 |
NSPT0034 |
544601 |
8467801 |
1143 |
11.0 |
|
NSPT0054 |
548194 |
8475395 |
1150 |
10.0 |
NSPT0035 |
544600 |
8467400 |
1146 |
10.0 |
|
NSPT0055 |
547799 |
8474999 |
1157 |
13.0 |
NSPT0036 |
545402 |
8466200 |
1149 |
4.2 |
|
NSPT0056 |
548600 |
8475798 |
1144 |
10.0 |
NSPT0037 |
545799 |
8466200 |
1149 |
6.0 |
|
NSPT0057 |
547401 |
8475800 |
1151 |
4.0 |
NSPT0038 |
545800 |
8465800 |
1159 |
10.0 |
|
NSPT0058 |
548200 |
8475800 |
1149 |
4.6 |
NSPT0039 |
545400 |
8465800 |
1161 |
10.0 |
|
NSPT0059 |
547802 |
8475799 |
1150 |
10.0 |
NSPT0040 |
546598 |
8475799 |
1149 |
13.0 |
|
|
|
|
|
|
Appendix III: JORC Code, 2012 Edition - Table 1
SECTION 1 - SAMPLING TECHNIQUES AND DATA
Criteria |
JORC Code explanation |
Commentary |
Sampling Techniques |
Nature and quality of sampling (e.g. cut channels, random chips, or specific specialised industry standard measurement tools appropriate to the minerals under investigation, such as down hole gamma sondes, or handheld XRF instruments, etc). These examples should not be taken as limiting the broad meaning of sampling.
|
Hand auger samples are composited based on regolith boundaries and sample chemistry, generated by hand-held XRF analysis. Each 1m of sample is dried and riffle-split to generate a total sample weight of 3kg for analysis, generally at 2 - 5m intervals. This primary sample is then split again to provide a 1.5kg sample for both rutile and graphite analyses.
Push tube/core drilling is sampled routinely at 2m intervals by compositing dried and riffle-split half core. A consistent, 1.5kg sample is generated for both the rutile and graphite determination.
|
Include reference to measures taken to ensure sample representivity and the appropriate calibration of any measurement tools or systems used.
|
Drilling and sampling activities are supervised by a suitably qualified Company geologist who is present at all times. All drill samples are geologically logged by the geologist at the drill site/core yard.
Each sample is sun dried and homogenised. Sub-samples are carefully riffle split to ensure representivity. The 1.5kg composite samples are then processed.
An equivalent mass is taken from each sample to make up the composite. A calibration schedule is in place for laboratory scales, sieves and field XRF equipment.
Placer Consulting Pty Ltd (Placer) Resource Geologists have reviewed Standard Operating Procedures (SOPs) for the collection and processing of drill samples and found them to be fit for purpose. The primary composite sample is considered representative for this style of rutile mineralisation.
|
|
Aspects of the determination of mineralisation that are Material to the Public Report. In cases where 'industry standard' work has been done this would be relatively simple (e.g. 'reverse circulation drilling was used to obtain 1 m samples from which 3 kg was pulverised to produce a 30 g charge for fire assay'). In other cases more explanation may be required, such as where there is coarse gold that has inherent sampling problems. Unusual commodities or mineralisation types (e.g. submarine nodules) may warrant disclosure of detailed information.
|
Logged mineralogy percentages, lithology information and TiO2% obtained from handheld XRF are used to determine compositing intervals. Care is taken to ensure that only samples with similar geological characteristics are composited together |
|
Drilling Techniques |
Drill type (e.g. core, reverse circulation, open ‐ hole hammer, rotary air blast, auger, Bangka, sonic, etc) and details (e.g. core diameter, triple or standard tube, depth of diamond tails, face ‐ sampling bit or other type, whether core is oriented and if so, by what method, etc).
|
A total of 607 hand auger holes for 5,724m were drilled at the Kasiya-Nsaru Rutile Deposit to obtain samples for quantitative determination of recoverable rutile and Total Graphitic Carbon (TGC).
A total of 92 push-tube core holes, for 950.4m, were drilled at the Kasiya-Nsaru Rutile Deposit to obtain samples for quantitative determination of recoverable rutile and Total Graphitic Carbon (TGC).
Placer has reviewed SOPs for hand-auger and push-tube drilling and found them to be fit for purpose and support the resource classifications as applied to the MRE. Sample handling and preparation techniques is consistent for push-tube and coring samples.
Hand-auger drilling is completed with 75mm diameter enclosed spiral bits (SOS) with 1-metre-long steel rods. Drilling is oriented vertically by eye. Each 1m of drill sample is collected into separate sample bags and set aside. The auger bits and flights are cleaned between each metre of sampling to avoid contamination. Core-drilling is undertaken using a drop hammer, Dando Terrier MK1. The drilling generated 1-metre runs of 83mm PQ core in the first 2m and then transitioned to 72mm core for the remainder of the hole. Core drilling is oriented vertically by spirit level.
|
Drill Sample Recovery |
Method of recording and assessing core and chip sample recoveries and results assessed.
|
Samples are assessed visually for recoveries. The configuration of drilling and nature of materials encountered results in negligible sample loss or contamination. Hand-auger drilling is ceased when recoveries become poor once the water table has been reached. Water table and recovery information is included in lithological logs. Core drilling samples are actively assessed by the driller and geologist onsite for recoveries and contamination.
|
Measures taken to maximise sample recovery and ensure representative nature of the samples.
|
The Company's trained geologists supervise drilling on a 1 team 1 geologist basis and are responsible for monitoring all aspects of the drilling and sampling process.
For push-tube drilling, core is extruded into core trays; slough is actively removed by the driller at the drilling rig and core recovery and quality is recorded by the geologist.
|
|
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.
|
No relationship is believed to exist between grade and sample recovery. The high percentage of silt and absence of hydraulic inflow from groundwater at this deposit results in a sample size that is well within the expected size range.
No bias related to preferential loss or gain of different materials is observed. |
|
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.
|
Geologically, data is collected in detail, sufficient to aid in Mineral Resource estimation.
All individual 1-metre auger intervals are geologically logged, recording relevant data to a set template using company codes. A small representative sample is collected for each 1-metre interval and placed in appropriately labelled chip trays for future reference.
All individual 1-metre core intervals are geologically logged, recording relevant data to a set template using company codes.
Half core remains in the trays and is securely stored in the company warehouse.
|
Whether logging is qualitative or quantitative in nature. Core (or costean, channel, etc.) photography.
|
All logging includes lithological features and estimates of basic mineralogy. Logging is generally qualitative.
The core is photographed dry, after logging and sampling is completed.
|
|
The total length and percentage of the relevant intersection logged
|
100% of samples are geologically logged. |
|
Sub-sampling techniques and sample preparation |
If core, whether cut or sawn and whether quarter, half or all core taken.
|
Due to the soft nature of the material, core samples are carefully cut in half by hand tools.
|
If non-core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry. |
Auger and core hole samples are dried, riffle split and composited. Samples are collected and homogenised prior to splitting to ensure sample representivity. ~1.5kg composite samples are processed.
An equivalent mass is taken from each primary sample to make up the composite.
The primary composite sample is considered representative for this style of mineralisation and is consistent with industry standard practice.
|
|
For all sample types, the nature, quality and appropriateness of the sample preparation technique.
|
Techniques for sample preparation are detailed on SOP documents verified by Placer Resource Geologists.
Sample preparation is recorded on a standard flow sheet and detailed QA/QC is undertaken on all samples. Sample preparation techniques and QA/QC protocols are appropriate for mineral determination.
|
|
Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.
|
The sampling equipment is cleaned after each sub-sample is taken.
Field duplicate, laboratory replicate and standard sample geostatistical analysis is employed to manage sample precision and analysis accuracy.
|
|
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.
|
Sample size analysis is completed to verify sampling accuracy. Field duplicates are collected for precision analysis of riffle splitting. SOPs consider sample representivity. Results indicate a sufficient level of precision for the resource classification.
|
|
Whether sample sizes are appropriate to the grain size of the material being sampled.
|
The sample size is considered appropriate for the material sampled. |
|
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. |
Rutile The Malawi onsite laboratory sample preparation methods are considered quantitative to the point where a heavy mineral concentrate (HMC) is generated.
Final results generated are for recovered rutile i.e, the % mass of the sample that is rutile that can be recovered to the non-magnetic component of a HMC.
The HMC is prepared via wet-table, gravity separation at the Lilongwe Laboratory which provides an ideal sample for subsequent magnetic separation and XRF.
All samples (incl. QA) included in this announcement received the following workflow undertaken on-site in Malawi; · Dry sample in oven for 1 hour at 105 ℃ · Soak in water and lightly agitate · Wet screen at 5mm, 600µm and 45µm to remove oversize and slimes material · Dry +45µm -600mm (sand fraction) in oven for 1 hour at 105 ℃ · Pass +45µm -600mm (sand fraction) across wet table to generate a heavy mineral concentrate (HMC) · Dry HMC in oven for 30 minutes at 105 ℃ Bag HMC fraction and send to Perth, Australia for quantitative chemical and mineralogical determination.
All of the sample received the final workflow undertaken at Perth based Laboratories. · Magnetic separation of the HMC by Carpco magnet @ 16,800G (2.9Amps) into a magnetic (M) and non-magnetic (NM) fraction. Work undertaken at Allied Mineral Laboratories (AML) in Perth. · The NM fractions were sent to ALS Perth for quantitative XRF analysis. Samples received XRF_MS. Graphite All samples were processed at Intertek-Genalysis Perth via method C72/CSA.
A portion of each test sample is dissolved in dilute hydrochloric acid to liberate carbonate carbon. The solution is filtered using a filter paper and the collected residue is the dried to 425°C in a muffle oven to drive off organic carbon. The dried sample is then combusted in a Carbon/ Sulphur analyser to yield total graphitic or elemental carbon (TGC). The graphitic carbon content is determined by eliminating other carbon forms from the total carbon content. The addition of acid to the sample liberates carbon dioxide thus removing carbonate carbon. Soluble organic carbon will also be removed. Insoluble organic carbon is removed by heating the samples at 425°C in an oxidising environment. The "dried" carbon-bearing sample that is analysed in the resistance furnace is considered to contain only graphitic carbon. An Eltra CS-800 induction furnace infra-red CS analyser is then used to determine the remaining carbon which is reported as Total Graphitic Carbon (TGC) as a percentage.
|
For geophysical tools, spectrometers, handheld XRF instruments, etc., the parameters used in determining the analysis including instrument make and model, reading times, calibrations factors applied and their derivation, etc.
|
Acceptable levels of accuracy and precision have been established. No handheld XRF methods are used for quantitative determination. |
|
Nature of quality control procedures adopted (e.g. standards, blanks, duplicate, external laboratory checks) and whether acceptable levels of accuracy (i.e. lack of bias) and precision have been established.
|
Sovereign uses internal and externally sourced wet screening reference material inserted into samples batches at a rate of 1 in 20. The externally sourced, certified standard reference material for HM and Slimes assessment is provided by Placer Consulting.
An external laboratory raw sample duplicate is sent to laboratories in Perth, Australia as an external check of the full workflow. These duplicates are produced at a rate of 1 in 20.
Accuracy monitoring is achieved through submission of certified reference materials (CRM's).
ALS and Intertek both use internal CRMs and duplicates on XRF analyses.
Sovereign also inserts CRMs into the sample batches at a rate of 1 in 20.
Three CRMs used by Sovereign. AMIS0602 (Rutile A) containing TiO2 XRF 90.62%. The CRM is supplied by African Mineral Standards (AMIS), South Africa. Rutile B containing TiO2 XRF 70.71%. The CRM is supplied by OREAS and has been designed and matrix matched specifically for Sovereign. Rutile C containing TiO2 XRF 40.76%. The CRM is supplied by OREAS and has been designed and matrix matched specifically for Sovereign.
Analysis of sample duplicates is undertaken by standard geostatistical methodologies (Scatter, Pair Difference and QQ Plots) to test for bias and to ensure that sample splitting is representative. Standards determine assay accuracy performance, monitored on control charts, where failure (beyond 3SD from the mean) may trigger re-assay of the affected batch.
Examination of the QA/QC sample data indicates satisfactory performance of field sampling protocols and assay laboratories providing acceptable levels of precision and accuracy.
Acceptable levels of accuracy and precision are displayed in geostatistical analyses.
|
|
Verification of sampling & assaying |
The verification of significant intersections by either independent or alternative company personnel.
|
Results are reviewed in cross-section using Micromine software and any spurious results are investigated. The deposit type and consistency of mineralisation leaves little room for unexplained variance. Extreme high grades are not encountered. Significant mineralisation intersections.
|
The use of twinned holes. |
Twinned holes are drilled across a geographically-dispersed area to determine short-range geological and assay field variability. Twin drilling is applied at a rate of 1 in 20 routine holes.
Acceptable levels of precision are displayed in the geostatistical analysis of twin drilling data.
No twin holes are reported here. |
|
Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. |
All data are collected initially on paper logging sheets and codified to the Company's templates. This data is hand entered to spreadsheets and validated by Company geologists. This data is then imported to a Datashed5 and validated automatically and then manually.
A transition to electronic field and laboratory data capture is underway.
|
|
Discuss any adjustment to assay data.
|
QEMSCAN of the NM fraction shows dominantly clean and liberated rutile grains and confirms rutile is the only titanium species in the NM fraction.
Recovered rutile is therefore defined and reported here as: TiO2 recovered in the +45 to -600um range to the NM concentrate fraction as a % of the total primary, dry, raw sample mass divided by 95% (to represent an approximation of final product specifications). i.e recoverable rutile within the whole sample.
|
|
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.
|
A Trimble R2 Differential GPS is used to pick up the hand auger collars. Daily capture at a registered reference marker ensures equipment remains in calibration. No downhole surveying of hand-auger holes is completed. Given the vertical nature and shallow depths of the hand-auger holes, drill hole deviation is not considered to significantly affect the downhole location of samples.
|
Specification of the grid system used. |
WGS84 UTM Zone 36 South.
|
|
Quality and adequacy of topographic control. |
DGPS pickups are considered to be high quality topographic control measures.
|
|
Data spacing & distribution |
Data spacing for reporting of Exploration Results. |
The hand auger collars are spaced at nominally 400m along the 400m spaced drill-lines with the push-tube holes similarly spaced at an offset, infill grid. The resultant 200m by 200m drill spacing (to the strike orientation of the deposit) is deemed to adequately define the mineralisation.
|
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. |
The drill spacing and distribution is considered to be sufficient to establish a degree of geological and grade continuity appropriate for a future Mineral Resource estimation.
|
|
Whether sample compositing has been applied. |
Individual 1m auger intervals have been composited, based on lithology, at 2 - 5m sample intervals for the 607 auger holes. Core holes have been sampled at a regular 2m interval to provide greater control on mineralisation.
|
|
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
|
Sample orientation is vertical and approximately perpendicular to the orientation of the mineralisation, which results in true thickness estimates, limited by the sampling interval as applied. Drilling and sampling are carried out on a regular square grid. There is no apparent bias arising from the orientation of the drill holes with respect to the orientation of the deposit.
|
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.
|
There is no apparent bias arising from the orientation of the drill holes with respect to the orientation of the deposit. |
|
Sample security |
The measures taken to ensure sample security |
Samples are stored in secure storage from the time of drilling, through gathering, compositing and analysis. The samples are sealed as soon as site preparation is complete.
A reputable international transport company with shipment tracking enables a chain of custody to be maintained while the samples move from Malawi to Australia. Samples are again securely stored once they arrive and are processed at Australian laboratories. A reputable domestic courier company manages the movement of samples within Perth, Australia.
At each point of the sample workflow the samples are inspected by a company representative to monitor sample condition. Each laboratory confirms the integrity of the samples upon receipt.
|
Audits or reviews |
The results of any audits or reviews of sampling techniques and data
|
Richard Stockwell (CP) has reviewed and advised on all stages of data collection, sample processing, QA protocol and mineral resource estimation. Methods employed are considered industry best-practice.
Perth Laboratory visits have been completed by Richard. Field and in-country lab visits are precluded, for the time being, by Covid 19 travel restrictions. In these cases, audit is completed by SOP review, site visits by an experienced senior geologist from South Africa and collection of photographs and video during operations.
Sovereign Metals Managing Director and CP for all exploration results Julian Stephens has been onsite in Malawi numerous times since the discovery of the Kasiya-Nsaru Deposit.
|
Criteria |
Explanation |
Commentary |
Mineral tenement & 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 environment settings. |
The Company owns 100% of the following Exploration Licences (ELs) and Retention Licence (RL) under the Mines and Minerals Act 2019, held in the Company's wholly-owned, Malawi-registered subsidiaries: EL0372, EL0413, EL0492, EL0528, EL0545, EL0561, EL0582 and RL0012 A 5% royalty is payable to the government upon mining and a 2% of net profit royalty is payable to the original project vendor. No significant native vegetation or reserves exist in the area. The region is intensively cultivated for agricultural crops. |
The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
The tenements are in good standing and no known impediments to exploration or mining exist. |
|
Exploration done by other parties
|
Acknowledgement and appraisal of exploration by other parties. |
Sovereign Metals Ltd is a first-mover in the discovery and definition of residual rutile and graphite resources in Malawi. No other parties are involved in exploration. |
Geology |
Deposit type, geological setting and style of mineralisation |
The rutile deposit type is considered a residual placer formed by the intense weathering of rutile-rich basement paragneisses and variable enrichment by elluvial processes. Rutile occurs in a mostly topographically flat area west of Malawi's capital, known as the Lilongwe Plain, where a deep tropical weathering profile is preserved. A typical profile from top to base is generally soil ("SOIL" 0-1m) ferruginous pedolith ("FERP", 1-4m), mottled zone ("MOTT", 4-7m), pallid saprolite ("PSAP", 7-9m), saprolite ("SAPL", 9-25m), saprock ("SAPR", 25-35m) and fresh rock ("FRESH" >35m). The low-grade graphite mineralisation occurs as multiple bands of graphite gneisses, hosted within a broader Proterozoic paragneiss package. In the Kasiya-Nsaru areas specifically, the preserved weathering profile hosts significant vertical thicknesses from near surface of graphite mineralisation. |
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: easting and northings of the drill hole collar; elevation or RL (Reduced Level-elevation above sea level in metres of the drill hole collar); dip and azimuth of the hole; down hole length and interception depth; and hole length |
All collar and composite data are provided in the body and appendices of this report.
|
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 |
No information has been excluded. |
|
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. |
All results reported are of a length-weighted average of in-situ grades. The results reported in the body of the report are on a nominal lower cut-off of 0.5% Rutile.
|
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. |
No data aggregation was required. |
|
The assumptions used for any reporting of metal equivalent values should be clearly stated. |
No metal equivalent values are used in this report. |
|
Relationship between mineralisation widths & intercept lengths |
These relationships are particularly important in the reporting of Exploration Results. |
The mineralisation has been released by weathering of the underlying, layered gneissic bedrock that broadly trends NE-SW. It lies in a laterally extensive superficial blanket with high-grade zones reflecting the broad bedrock strike orientation of ~045°. |
If the geometry of the mineralisation with respect to the drill hole angle is known, its nature should be reported. |
The mineralisation is laterally extensive where the entire weathering profile is preserved and not significantly eroded. Minor removal of the mineralised profile has occurred in alluvial channels. These areas are adequately defined by the drilling pattern and topographical control. |
|
If it is not known and only the down hole lengths are reported, there should be a clear statement to this effect (e.g. 'down hole length, true width not known'. |
Downhole widths approximate true widths limited to the sample intervals applied. Mineralisation remains open at depth and in areas coincident with high-rutile grade lithologies in basement rocks, is increasing with depth. Graphite results are approximate true width as defined by the sample interval and typically increase with depth. |
|
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 the drill collar locations and appropriate sectional views. |
Refer to figures in the body of the full report. |
Balanced reporting |
Where comprehensive reporting of all Exploration Results is not practicable, representative reporting of both low and high-grades and/or widths should be practiced to avoid misleading reporting of exploration results. |
All results are included in this report. |
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. |
Rutile has been determined, by QEMSCAN, to be the major TiO2-bearing mineral at and around several rutile prospects within Sovereign's ground package. The company continues to examine areas within the large tenement package for rutile and graphite by-product mineralisation. |
Further work |
The nature and scale of planned further work (e.g. test for lateral extensions or depth extensions or large-scale step-out drilling). |
Air-Core drilling is planned for 2022 to further expand the area of known mineralisation, specifically at depth. |
Diagrams clearly highlighting the areas of possible extensions, including the main geological interpretations and future drilling areas, provided this information is not commercially sensitive. |
Refer to diagrams in the body of this report. |