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#SVML Sovereign Metals Ltd – Demerger Timetable
Sovereign Metals Limited (Company) (ASX:SVM, AIM:SVML) provides an update to the indicative timetable in relation to the demerger of NGX as disclosed below.
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Event |
Indicative Date |
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Effective date of Distribution |
20 March 2023 |
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Repositioning of securities between the Australian share register and UK Depositary Interest register is suspended at the close of business |
21 March 2023 |
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Ex Date |
22 March 2023 |
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Record Date |
23 March 2023 |
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Repositioning of securities between the Australian share register and UK Depositary Interest register recommences |
24 March 2023 |
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Date for Distribution to Shareholders (Distribution Date) |
24 March 2023 |
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Despatch of holding statements for NGX Shares transferred under the Distribution |
27 March 2023 |
Note: The dates shown in the table above are indicative only and may vary subject to the Corporations Act, the Listing Rules, the AIM Rules and other applicable laws.
ENQUIRIES
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Dylan Browne Company Secretary info@sovereignmetals.com |
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Nominated Adviser on AIM |
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RFC Ambrian |
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Andrew Thomson |
+61 8 9480 2500 |
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Joint Brokers |
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Berenberg |
+44 20 3207 7800 |
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Matthew Armitt |
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Jennifer Lee |
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Optiva Securities |
+44 20 3137 1902 |
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Daniel Ingram |
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Mariela Jaho |
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Christian Dennis |
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#SVML Sovereign Metals Ltd – Company Presentation
COMPANY PRESENTATION
Sovereign Metals Limited (Company) is pleased to advise that a presentation entitled ‘Company Presentation’ is available to download from the Company’s website at: http://sovereignmetals.com.au/company-presentations/.
ENQUIRIES
|
Dr Julian Stephens (Perth) +61(8) 9322 6322 |
Sam Cordin (Perth) |
Sapan Ghai (London)
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Nominated Adviser on AIM |
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RFC Ambrian |
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Bhavesh Patel / Andrew Thomson |
+44 20 3440 6800 |
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Joint Brokers |
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Berenberg |
+44 20 3207 7800 |
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Matthew Armitt |
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Jennifer Lee |
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Optiva Securities |
+44 20 3137 1902 |
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Daniel Ingram |
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Mariela Jaho |
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Christian Dennis |
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#POW Power Metal Resources PLC – Strategic Uranium Properties Staked – Athabasca
Power Metal Resources PLC (LON:POW) the London listed exploration company seeking large-scale metal discoveries across its global project portfolio announces an update concerning its uranium property portfolio focused on the Athabasca Basin area in Saskatchewan, Canada.
Paul Johnson, Chief Executive Officer of Power Metal Resources plc, commented:
“The uranium acquisitions by staking announced today are a further leap forward for Power Metal’s strategic uranium interests in and surrounding the prolific Athabasca Basin located in northern Saskatchewan, Canada.
The two new properties now secured are adjacent to and largely surrounded by major uranium companies and they demonstrate significant uranium prospectivity with geology considered by the Company to be analogous to major producing mines and other uranium deposits within the Athabasca Basin.
Power Metal started the move to build a uranium exploration business in September 2021 and we believe we are now in a particularly strong position. Our intentions do not stop here, with plans to further expand our uranium focused interests where suitable opportunities are identified.
Uranium has a strong following in capital markets and recently the spot uranium price has moved again above USD$50/lb. With the world dynamic shifting strongly in favour of nuclear power generation we believe that Power Metal should continue this push to build its uranium exploration and development business interests in the London financial markets.“
HIGHLIGHTS:
All claims were acquired by direct mineral claim staking by the Power Metal technical team. They were acquired during the most recent Mineral Administration Registry Saskatchewan (“MARS”) electronic registry system claim reopening on 31 January 2023. The staking acquisitions represent some of the most significant additions to the Company’s uranium portfolio. Further information on the staking process can be found in the further information section below.
The newly acquired Haresign Bay uranium Property (“Haresign Bay”) covers a total area of 3,189.2-hectares (31.89km2) located 35km south of the Athabasca Basin. Haresign Bay is surrounded by claims held by uranium focussed companies F3 Uranium Corp, Baselode Energy Corp, CanAlaska Uranium Ltd and Skyharbour Resources Ltd.
The newly acquired Kernaghan uranium Property (“Kernaghan”) covers a total area of 4,566.2-hectares (45.66km2) within the northeastern edge of the Athabasca Basin. Kernaghan is bordered on three sides by claims held by uranium focussed companies including Standard Uranium Ltd., IsoEnergy Ltd., and Purepoint Uranium Group Inc.
During the most recent claim reopening, Power Metal also staked an additional 1,982-hectare (19.82km2) claim area bordering the western extension of its Thibault Lake uranium Property (the “Extension”). Significantly, the Extension covers a historical showing which returned a trenching result of 1.09% U308 over 10.7m, greatly increasing the overall prospectively of the extended Thibault Lake uranium Property. 2
With the addition of the Kernaghan and Haresign Bay uranium properties, as well as the additional staking at Thibault Lake, the Power Metal Athabasca uranium portfolio now consists of fourteen properties, including two conditional disposals1, with a combined total area of 940km2.
FURTHER INFORMATION
Mineral Claim Staking Process
The mineral claims constituting the Haresign Bay and Kernaghan Uranium Properties as well as the Thibault Lake Extension were acquired directly through the Mineral Administration Registry Saskatchewan (“MARS”) electronic registry system.
Where a previous claim owner is unable to satisfy the claim maintenance requirements, that ground is reopened to third party staking at a set time each month. Select reopening’s are often highly competitive with many parties attempting to acquire the newly available land.
The total cost of staking was CAD$5,842.34. The newly staked licences come with a two-year term with no minimum spend requirement and which can then be extended for subsequent years by spending a minimum of CAD$146,059 per annum.
The Haresign Bay Property
Haresign Bay is located 43km south of Cameco Corporation’s Key Lake Uranium Mine which is the third largest deposit within the Athabasca Basin – with an average mineable grade of just over 2% U3O8.1 Haresign Bay is located 35km south of the Athabasca Basin, along the Key Lake trend, which is defined by a cluster of northeast-southwest trending electromagnetic conductors which extend to the northeast over the Key Lake Mine. The Key Lake trend is a defining geophysical and geological trend within the Athabasca Basin, and Haresign Bay represents a significant position held within this important uranium-rich corridor.
The Upper Roberta Lake Target (“Upper Roberta Lake” or the “Target”) is located in the southwestern part of the Haresign Bay Property and is defined by a gravity low anomaly which is coincident with elevated Radon222-in-lake water results. This Target area is further intersected by multiple electromagnetic conductors of part of the Key Lake Trend. Upper Roberta Lake represents a highly compelling target for future work.
The Kernaghan Property
Kernaghan is located within the prolific Athabasca Basin approximately 13km from the Basin’s edge. Based on nearby borehole’s drilled by Denison Mines Corp., the sandstone-basement unconformity on the Property is expected to be at around 100m depth.
The Kernaghan Property covers multiple anomalous Radon222-in-lake water results which are oriented within a northeast-southwest trending belt. This trend is coincident with a magnetic low feature. Kernaghan represents the Company’s third property which is located entirely within the Athabasca Basin.
Thibault Lake West Extension
The Extension covers an additional four Saskatchewan Mineral Deposit Index (“SMDI”) points. These SMDI points cover multiple high-grade uranium showings including a north trending zone of strong uranium mineralisation from which historic trenching returned 10.7m of 1.09% U308.2 Several other high-grade uranium showings are covered by the Extension including grab and/or channel samples which returned 4.8%, 1.75%, 0.71%, and 0.66% U308.3,4
Next Steps
The Company is preparing fact sheets which will include further information and maps for newly acquired staking. These will be released to the market once ready. Furthermore, detailed data rooms are being prepared.
URANIUM PROPERTIES – HOLDING STRUCTURE
Power Metal has a 100% subsidiary Power Metal Canada Inc (“Power Canada”), which acts as the holding Company for certain Canadian project operations. Power Canada has a wholly-owned subsidiary, 102134984 Saskatchewan Ltd, which is the holder of the Company’s Athabasca uranium portfolio.
The Power Metal Canada Uranium Property Map is available to view at the following link:
https://www.powermetalresources.com/power-metal-canada-uranium-map/
Table 1: 102134984 Saskatchewan Ltd., Athabasca Basin Property Holdings
|
Project |
Licence ID |
Area (Hectare) |
Area (km2) |
|
Clearwater Uranium Property |
MC00015079 |
1,110 |
11.1 |
|
MC00015083 |
563 |
5.63 |
|
|
MC00015082 |
3,191 |
31.91 |
|
|
MC00015151 |
760 |
7.6 |
|
|
MC00015646 |
761 |
7.61 |
|
|
MC00015658 |
1,541 |
15.41 |
|
|
Tait Hill Uranium Property |
MC00015078 |
1,576 |
15.76 |
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MC00015081 |
968 |
9.68 |
|
|
MC00015153 |
1,530 |
15.3 |
|
|
MC00015152 |
1,886 |
18.86 |
|
|
MC00015647 |
725 |
7.25 |
|
|
MC00015648 |
1,129 |
11.29 |
|
|
MC00016158 |
3,242 |
32.42 |
|
|
Thibault Lake Uranium Property |
MC00015077 |
2,206 |
22.06 |
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MC00015659 |
2,195 |
21.95 |
|
|
AC00018709 |
1,982 |
19.82 |
|
|
Soaring Bay Uranium Property |
MC00015080 |
1,255 |
12.55 |
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MC00015155 |
3,375 |
33.75 |
|
|
MC00015874 |
748 |
7.48 |
|
|
MC00015875 |
2,529 |
25.29 |
|
|
Cook Lake Uranium Property |
MC00015212 |
984 |
9.84 |
|
E-12 Uranium Property5 |
MC00015213 |
1,323 |
13.23 |
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Reitenbach Uranium Property6 |
MC00015214 |
2,135 |
21.35 |
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MC00015474 |
1,235 |
12.35 |
|
|
MC00015655 |
4,570 |
45.7 |
|
|
MC00015656 |
5,322 |
53.22 |
|
|
MC00015657 |
886 |
8.86 |
|
|
MC00015824 |
528 |
5.28 |
|
|
MC00016155 |
1,333 |
13.33 |
|
|
Reindeer Lake |
MC00015522 |
3,336 |
33.36 |
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Porter Lake |
MC00015561 |
5,656 |
56.56 |
|
MC00015562 |
5,198 |
51.98 |
|
|
Old Woman Rapids |
MC00015563 |
4,851 |
48.51 |
|
MC00015564 |
5,063 |
50.63 |
|
|
MC00015565 |
3,044 |
30.44 |
|
|
Durrant Lake |
AC00018000 |
5,866 |
58.66 |
|
Badger Lake |
MC00016253 |
1,671 |
16.71 |
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Haresign Bay |
AC00018692 |
3,189 |
31.89 |
|
Kernaghan |
AC00018694 |
4,566 |
45.66 |
|
Total Licence Holding Area |
93,998 |
939.98km2 |
|
#SVML Sovereign Metals Ltd – Kasiya Resource Infill Drilling Results
Sovereign Metals Limited (ASX:SVM; AIM:SVML) (“Sovereign” or the “Company”) announced on 27 January 2023 that following movements in its share price on the Australian Securities Exchange (“ASX”) and a price query from ASX, the Company’s ordinary shares were placed in a trading halt on the ASX. The ASX has informed Sovereign that the trading halt has been lifted and trading of the Company’s ordinary shares has resumed on the ASX.
The trading halt did not affect trading in the Company’s shares on the AIM market of the London Stock Exchange plc, where normal trade continued.
Drilling results from the Company’s targeted deep infill air-core (AC) and push tube (PT) core drilling program confirms consistency of high-grade rutile and graphite mineralisation at depth
· AC results include:
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– 31m @ 1.14% rutile & 1.9% graphite – 27m @ 1.08% rutile & 2.1% graphite – 29m @ 1.14% rutile & 1.7% graphite – 24m @ 1.14% rutile & 1.8% graphite – 21m @ 1.28% rutile & 1.9% graphite |
– 25m @ 1.18% rutile & 2.0% graphite – 25m @ 1.08% rutile & 5.2% graphite – 26m @ 1.16% rutile & 1.5% graphite – 26m @ 1.07% rutile & 1.4% graphite – 24m @ 1.13% rutile & 4.0% graphite |
· Infill core PT drilling of numerous Inferred category pits and potential pit extensions is expected to add new blocks of Indicated material to the upcoming Mineral Resource Estimate (MRE) update targeted for Q1 2023
· Kasiya’s pre-feasibility study (PFS) and Environmental and Social baseline workstreams are progressing on schedule with the targeted completion of the PFS during H1 2023
Sovereign Metals Limited (ASX:SVM; AIM:SVML) (Sovereign or the Company) is pleased to report further results for 98 AC holes and 247 PT holes from the Kasiya Rutile Project (Kasiya), the world’s largest rutile deposit.
Sovereign’s Managing Director Dr Julian Stephens commented: “We are pleased with the consistency of the high-grade rutile results from the 2022 Kasiya infill resource drilling program. These results will all now feed into a revised resource estimate planned for Q1 2023 as part of the Company’s forthcoming PFS”.
ENQUIRIES
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Dr Julian Stephens (Perth) +61(8) 9322 6322 |
Sam Cordin (Perth) |
Sapan Ghai (London)
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Nominated Adviser on AIM |
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RFC Ambrian |
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Bhavesh Patel / Andrew Thomson |
+44 20 3440 6800 |
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Joint Brokers |
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Berenberg |
+44 20 3207 7800 |
|
Matthew Armitt |
|
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Jennifer Lee |
|
|
|
|
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Optiva Securities |
+44 20 3137 1902 |
|
Daniel Ingram |
|
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Mariela Jaho |
|
|
Christian Dennis |
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KASIYA AIR CORE DRILLING
A 191-hole AC drilling program was completed at the Kasiya rutile deposit. The final batch of the remaining 98 AC holes for 2,548m are reported in this announcement.
This drilling phase targeted the early-scheduled mining pit shells in the southern and central areas of the MRE footprint. As previously reported (ASX Announcement released 26 October 2022) the drilling has revealed that rutile and graphite mineralisation is commonly pervasive throughout the saprolite zone and beyond the base of the current modelled pit shells. However, it is not expected the revised MRE incorporating these results will materially impact the mine plan to be included in the PFS.
KASIYA PUSH TUBE CORE DRILLING
Results for the 247-hole PT (core) drilling program are reported in this announcement. The core program objectives were to target high grade Inferred mining pits and potential areas of pit extensions to bring into the Indicated category to facilitate conversion to Ore Reserves in the upcoming PFS. Overall, results are as expected and continue to confirm laterally extensive and consistent rutile and graphite mineralisation at Kasiya.
PT results include:
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– 11m @ 1.70% inc. 3m @ 2.13% rutile – 12m @ 1.36% inc. 7m @ 1.63% rutile – 11m @ 1.27% inc. 9m @ 1.40% rutile – 7m @ 1.67% inc. 6m @ 1.79% rutile – 11m @ 1.20% inc. 4m @ 1.72% rutile – 9m @ 1.28% inc. 4m @ 1.68% rutile |
– 13m @ 1.19% inc. 1m @ 2.29% rutile – 13m @ 1.26% inc. 9m @ 1.45% rutile – 14m @ 1.15% inc. 2m @ 2.02% rutile – 15m @ 1.03% inc. 2m @ 2.16% rutile – 11m @ 1.11% inc. 6m @ 1.43% rutile – 14m @ 1.11% inc. 2m @ 1.84% rutile |
On completion of the PFS resource drilling programs the rigs continued to execute additional PFS work programs including water bore exploration drilling, water monitoring holes, geotechnical drilling of the water dam wall, geotechnical mining pit hole drilling and community borehole drilling until November 2022.
Four “deep” stratigraphic geology holes were also completed to benefit the geological interpretation of the mineralisation at Kasiya. Drilling and logging revealed, as expected, Kasiya is underlain by a rutile and graphite rich paragneiss parent host rock.
These stratigraphic holes were suitable as pit geotechnical test work holes where standard penetration testing was completed and as observation water bores which will be monitored over the coming years. The Company was also able to drill new community water bores as well as refurbish several existing ones.
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 performance rights 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 the Mineral Resource Estimate is extracted from the announcement dated 5 April 2022. The announcement is available to view on 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 announcement; b) all material assumptions included in the 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 announcement.
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Table 1: Kasiya Mineral Resource Estimate at 0.7% Rutile Cut-off |
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Mineral Resource Category |
Material Tonnes (millions) |
Rutile |
Rutile Tonnes (millions) |
Total Contained Graphite (TGC) |
TGC Tonnes (millions) |
RutEq. Grade* |
|
Indicated |
662 |
1.05% |
6.9 |
1.43% |
9.5 |
1.76% |
|
Inferred |
1,113 |
0.99% |
11.0 |
1.26% |
14.0 |
1.61% |
|
Total |
1,775 |
1.01% |
18.0 |
1.32% |
23.4 |
1.67% |
* RutEq. Formula: Rutile Grade x Recovery (98%) x Rutile Price (US$1,308/t) + Graphite Grade x Recovery (62%) x Graphite Price (US$1,085/t) / Rutile Price (US$1,308/t). All assumptions are taken from this Study ** Any minor summation inconsistencies are due to rounding
Qualified Person
Data disclosed in this press release have been reviewed and verified by Sovereign’s Qualified Person, Dr Julian Stephens (B.Sc (Hons), PhD, MAIG), Managing Director, for the purposes of the AIM Rules for Companies.
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 the announcement in full, including all illustrations and figures, please refer to the announcement at http://sovereignmetals.com.au/announcements/
Appendix I – DRILL RESULTS – Table 2
Rutile and graphite drilling results from Kasiya are shown below in Table 2.
|
Hole ID |
Interval Thickness |
Rutile % |
TGC % |
From (m) Downhole |
Hole Type |
|
KYAC0094 |
22.0 |
0.98 |
2.1 |
0.0 |
AC |
|
incl |
15.0 |
1.07 |
2.5 |
5.0 |
|
|
KYAC0095 |
10.0 |
0.76 |
2.0 |
0.0 |
AC |
|
KYAC0096 |
NSR |
AC |
|||
|
KYAC0097 |
20.0 |
0.81 |
1.7 |
0.0 |
AC |
|
incl |
5.0 |
1.53 |
0.6 |
2.0 |
|
|
KYAC0098 |
32.0 |
0.92 |
2.0 |
0.0 |
AC |
|
incl |
2.0 |
1.83 |
0.8 |
0.0 |
|
|
KYAC0099 |
20.0 |
0.94 |
1.3 |
0.0 |
AC |
|
incl |
6.0 |
1.09 |
0.4 |
0.0 |
|
|
KYAC0100 |
27.0 |
1.02 |
1.6 |
0.0 |
AC |
|
incl |
2.0 |
2.35 |
0.5 |
0.0 |
|
|
KYAC0101 |
20.0 |
0.90 |
1.4 |
0.0 |
AC |
|
incl |
4.0 |
1.63 |
0.5 |
0.0 |
|
|
KYAC0102 |
27.0 |
0.99 |
2.0 |
0.0 |
AC |
|
incl |
16.0 |
1.09 |
2.1 |
0.0 |
|
|
KYAC0103 |
27.0 |
1.08 |
2.1 |
0.0 |
AC TWIN |
|
incl |
16.0 |
1.11 |
2.1 |
0.0 |
|
|
KYAC0104 |
25.0 |
0.80 |
1.9 |
0.0 |
AC |
|
incl |
2.0 |
1.89 |
0.3 |
0.0 |
|
|
KYAC0105 |
25.0 |
0.93 |
1.6 |
0.0 |
AC |
|
incl |
2.0 |
1.85 |
0.3 |
0.0 |
|
|
KYAC0106 |
24.0 |
1.07 |
1.9 |
0.0 |
AC |
|
incl |
20.0 |
1.15 |
1.9 |
0.0 |
|
|
KYAC0107 |
17.0 |
0.93 |
1.7 |
0.0 |
AC |
|
incl |
2.0 |
1.85 |
0.6 |
0.0 |
|
|
KYAC0108 |
4.0 |
0.86 |
0.4 |
0.0 |
AC |
|
KYAC0109 |
21.0 |
0.81 |
1.9 |
0.0 |
AC |
|
incl |
2.0 |
2.10 |
0.2 |
0.0 |
|
|
KYAC0110 |
26.0 |
0.82 |
2.1 |
0.0 |
AC |
|
incl |
4.0 |
1.28 |
0.2 |
0.0 |
|
|
KYAC0111 |
28.0 |
0.90 |
2.9 |
0.0 |
AC |
|
incl |
4.0 |
1.59 |
0.5 |
0.0 |
|
|
KYAC0112 |
24.0 |
1.01 |
1.6 |
0.0 |
AC |
|
incl |
12.0 |
1.27 |
1.6 |
0.0 |
|
|
KYAC0113 |
18.0 |
1.29 |
1.6 |
0.0 |
AC |
|
KYAC0114 |
14.0 |
1.02 |
2.5 |
0.0 |
AC |
|
incl |
2.0 |
1.84 |
0.2 |
0.0 |
|
|
KYAC0115 |
31.0 |
1.14 |
1.9 |
0.0 |
AC |
|
incl |
4.0 |
1.67 |
0.4 |
0.0 |
|
|
incl |
10.0 |
1.25 |
2.2 |
19.0 |
|
|
KYAC0116 |
24.0 |
0.92 |
1.6 |
0.0 |
AC |
|
incl |
8.0 |
1.08 |
2.2 |
8.0 |
|
|
KYAC0117 |
14.0 |
0.98 |
1.7 |
0.0 |
AC |
|
incl |
2.0 |
2.31 |
0.3 |
0.0 |
|
|
KYAC0118 |
22.0 |
1.13 |
1.8 |
0.0 |
AC |
|
incl |
9.0 |
1.17 |
2.2 |
10.0 |
|
|
KYAC0119 |
26.0 |
0.76 |
1.6 |
0.0 |
AC |
|
KYAC0120 |
21.0 |
1.00 |
1.1 |
0.0 |
AC |
|
incl |
2.0 |
2.28 |
0.4 |
0.0 |
|
|
KYAC0121 |
24.0 |
1.09 |
2.1 |
0.0 |
AC |
|
incl |
3.0 |
1.65 |
0.2 |
0.0 |
|
|
KYAC0122 |
29.0 |
1.14 |
1.7 |
0.0 |
AC |
|
incl |
21.0 |
1.25 |
1.6 |
0.0 |
|
|
KYAC0123 |
29.0 |
1.16 |
1.8 |
0.0 |
AC TWIN |
|
incl |
4.0 |
1.72 |
0.5 |
0.0 |
|
|
KYAC0124 |
23.0 |
1.03 |
1.2 |
0.0 |
AC |
|
incl |
4.0 |
1.63 |
0.1 |
0.0 |
|
|
KYAC0125 |
23.0 |
0.95 |
2.0 |
0.0 |
AC |
|
incl |
6.0 |
1.20 |
2.5 |
4.0 |
|
|
KYAC0126 |
27.0 |
0.73 |
1.1 |
0.0 |
AC |
|
incl |
4.0 |
1.14 |
1.7 |
6.0 |
|
|
KYAC0127 |
17.0 |
0.91 |
1.2 |
0.0 |
AC |
|
incl |
2.0 |
2.18 |
0.2 |
0.0 |
|
|
KYAC0128 |
21.0 |
1.00 |
1.7 |
0.0 |
AC |
|
incl |
11.0 |
1.10 |
2.2 |
6.0 |
|
|
KYAC0129 |
4.0 |
1.14 |
0.2 |
0.0 |
AC |
|
incl |
2.0 |
1.52 |
0.2 |
0.0 |
|
|
KYAC0130 |
24.0 |
0.98 |
1.5 |
0.0 |
AC |
|
incl |
2.0 |
2.12 |
0.3 |
0.0 |
|
|
KYAC0131 |
34.0 |
0.86 |
1.8 |
0.0 |
AC |
|
incl |
3.0 |
2.06 |
0.3 |
0.0 |
|
|
KYAC0132 |
32.0 |
0.73 |
1.7 |
0.0 |
AC |
|
incl |
6.0 |
1.06 |
2.4 |
6.0 |
|
|
KYAC0133 |
33.0 |
0.81 |
1.9 |
0.0 |
AC |
|
incl |
2.0 |
1.40 |
0.2 |
0.0 |
|
|
KYAC0134 |
24.0 |
0.84 |
3.1 |
0.0 |
AC |
|
incl |
2.0 |
1.48 |
0.3 |
0.0 |
|
|
KYAC0135 |
2.0 |
2.44 |
0.2 |
0.0 |
AC |
|
KYAC0136 |
19.0 |
0.90 |
2.4 |
0.0 |
AC |
|
incl |
2.0 |
1.03 |
0.2 |
0.0 |
|
|
KYAC0137 |
23.0 |
1.05 |
1.9 |
0.0 |
AC |
|
incl |
3.0 |
1.90 |
0.2 |
0.0 |
|
|
KYAC0138 |
15.0 |
1.01 |
1.5 |
0.0 |
AC |
|
incl |
3.0 |
1.32 |
0.2 |
0.0 |
|
|
KYAC0139 |
25.0 |
1.18 |
2.0 |
0.0 |
AC |
|
incl |
15.0 |
1.27 |
1.9 |
0.0 |
|
|
KYAC0140 |
25.0 |
0.93 |
1.6 |
0.0 |
AC |
|
incl |
5.0 |
1.41 |
1.2 |
0.0 |
|
|
KYAC0141 |
23.0 |
0.94 |
1.7 |
0.0 |
AC |
|
incl |
2.0 |
1.96 |
0.3 |
0.0 |
|
|
KYAC0142 |
23.0 |
1.03 |
2.2 |
0.0 |
AC |
|
incl |
6.0 |
1.51 |
1.0 |
0.0 |
|
|
KYAC0143 |
23.0 |
0.99 |
2.2 |
0.0 |
AC TWIN |
|
incl |
4.0 |
1.87 |
0.5 |
0.0 |
|
|
KYAC0144 |
24.0 |
1.14 |
1.8 |
0.0 |
AC |
|
incl |
14.0 |
1.37 |
1.5 |
0.0 |
|
|
KYAC0145 |
20.0 |
1.25 |
2.1 |
0.0 |
AC |
|
incl |
10.0 |
1.50 |
0.9 |
0.0 |
|
|
incl |
18.0 |
1.29 |
2.0 |
0.0 |
|
|
KYAC0146 |
25.0 |
0.92 |
2.5 |
0.0 |
AC |
|
incl |
2.0 |
1.38 |
0.4 |
0.0 |
|
|
KYAC0147 |
20.0 |
0.85 |
1.6 |
0.0 |
AC |
|
incl |
2.0 |
1.37 |
0.4 |
0.0 |
|
|
KYAC0148 |
20.0 |
1.08 |
1.7 |
0.0 |
AC |
|
incl |
4.0 |
1.81 |
0.3 |
0.0 |
|
|
KYAC0149 |
24.0 |
0.97 |
2.3 |
0.0 |
AC |
|
incl |
4.0 |
1.58 |
0.3 |
0.0 |
|
|
KYAC0150 |
16.0 |
0.96 |
1.7 |
0.0 |
AC |
|
incl |
2.0 |
1.05 |
0.3 |
0.0 |
|
|
KYAC0151 |
22.0 |
0.82 |
2.3 |
0.0 |
AC |
|
incl |
2.0 |
1.14 |
0.4 |
0.0 |
|
|
KYAC0152 |
27.0 |
1.01 |
2.0 |
0.0 |
AC |
|
incl |
4.0 |
1.56 |
0.4 |
0.0 |
|
|
KYAC0153 |
21.0 |
1.28 |
1.9 |
0.0 |
AC |
|
incl |
17.0 |
1.40 |
1.6 |
0.0 |
|
|
KYAC0154 |
19.0 |
1.19 |
1.6 |
0.0 |
AC |
|
incl |
5.0 |
2.00 |
0.4 |
0.0 |
|
|
KYAC0155 |
24.0 |
1.13 |
4.0 |
0.0 |
AC |
|
incl |
4.0 |
1.71 |
1.4 |
0.0 |
|
|
KYAC0156 |
22.0 |
1.09 |
1.7 |
0.0 |
AC |
|
incl |
2.0 |
2.25 |
0.2 |
0.0 |
|
|
KYAC0157 |
26.0 |
1.07 |
1.4 |
0.0 |
AC |
|
incl |
4.0 |
1.93 |
0.2 |
0.0 |
|
|
KYAC0158 |
6.0 |
0.95 |
0.3 |
0.0 |
AC |
|
incl |
2.0 |
1.54 |
0.2 |
0.0 |
|
|
KYAC0159 |
21.0 |
1.06 |
1.5 |
0.0 |
AC |
|
incl |
2.0 |
1.53 |
0.2 |
0.0 |
|
|
KYAC0160 |
33.0 |
0.80 |
1.5 |
0.0 |
AC |
|
incl |
2.0 |
1.67 |
0.3 |
0.0 |
|
|
KYAC0161 |
28.0 |
0.86 |
2.5 |
0.0 |
AC |
|
incl |
2.0 |
2.22 |
0.3 |
0.0 |
|
|
KYAC0162 |
5.0 |
1.29 |
0.1 |
0.0 |
AC |
|
incl |
2.0 |
1.97 |
0.0 |
0.0 |
|
|
KYAC0163 |
5.0 |
1.16 |
0.3 |
0.0 |
AC TWIN |
|
incl |
3.0 |
1.42 |
0.3 |
0.0 |
|
|
KYAC0164 |
20.0 |
1.07 |
2.3 |
0.0 |
AC |
|
incl |
4.0 |
1.78 |
0.4 |
0.0 |
|
|
KYAC0165 |
26.0 |
1.16 |
1.5 |
0.0 |
AC |
|
incl |
6.0 |
1.73 |
0.6 |
0.0 |
|
|
incl |
20.0 |
1.27 |
1.5 |
0.0 |
|
|
KYAC0166 |
25.0 |
1.14 |
1.6 |
0.0 |
AC |
|
incl |
5.0 |
1.73 |
0.2 |
0.0 |
|
|
KYAC0167 |
23.0 |
1.15 |
2.0 |
0.0 |
AC |
|
incl |
13.0 |
1.43 |
1.4 |
0.0 |
|
|
KYAC0168 |
21.0 |
1.04 |
1.5 |
0.0 |
AC |
|
incl |
3.0 |
1.83 |
0.2 |
0.0 |
|
|
KYAC0169 |
18.0 |
0.99 |
1.3 |
0.0 |
AC |
|
incl |
2.0 |
2.26 |
0.3 |
0.0 |
|
|
KYAC0170 |
26.0 |
0.67 |
1.1 |
0.0 |
AC |
|
incl |
2.0 |
1.01 |
2.0 |
14.0 |
|
|
KYAC0171 |
28.0 |
0.95 |
1.4 |
0.0 |
AC |
|
incl |
2.0 |
1.86 |
0.3 |
0.0 |
|
|
KYAC0172 |
17.0 |
0.81 |
1.7 |
0.0 |
AC |
|
incl |
1.0 |
1.46 |
0.3 |
0.0 |
|
|
KYAC0173 |
23.0 |
0.82 |
1.3 |
0.0 |
AC |
|
KYAC0174 |
3.0 |
0.76 |
0.8 |
0.0 |
AC |
|
KYAC0175 |
17.0 |
0.92 |
4.9 |
0.0 |
AC |
|
incl |
3.0 |
1.61 |
0.6 |
0.0 |
|
|
KYAC0176 |
23.0 |
0.99 |
6.4 |
0.0 |
AC |
|
incl |
11.0 |
1.19 |
6.1 |
0.0 |
|
|
KYAC0177 |
14.0 |
2.23 |
9.6 |
0.0 |
AC |
|
incl |
8.0 |
2.27 |
13.9 |
6.0 |
|
|
KYAC0178 |
20.0 |
1.07 |
3.4 |
0.0 |
AC |
|
incl |
6.0 |
1.43 |
1.7 |
0.0 |
|
|
KYAC0179 |
22.0 |
1.05 |
5.2 |
0.0 |
AC |
|
incl |
6.0 |
1.56 |
3.3 |
0.0 |
|
|
KYAC0180 |
13.0 |
1.06 |
5.4 |
0.0 |
AC |
|
incl |
5.0 |
1.43 |
3.2 |
0.0 |
|
|
KYAC0181 |
26.0 |
0.91 |
5.0 |
0.0 |
AC |
|
incl |
4.0 |
1.57 |
1.0 |
0.0 |
|
|
KYAC0182 |
11.0 |
0.91 |
2.2 |
0.0 |
AC |
|
incl |
2.0 |
1.56 |
0.7 |
0.0 |
|
|
KYAC0183 |
15.0 |
0.84 |
3.0 |
0.0 |
AC TWIN |
|
incl |
2.0 |
1.24 |
0.0 |
0.0 |
|
|
KYAC0184 |
4.0 |
0.83 |
0.2 |
0.0 |
AC |
|
incl |
2.0 |
1.06 |
0.0 |
0.0 |
|
|
KYAC0185 |
4.0 |
0.97 |
0.3 |
0.0 |
AC |
|
incl |
2.0 |
1.08 |
0.2 |
0.0 |
|
|
KYAC0186 |
27.0 |
1.02 |
3.5 |
0.0 |
AC |
|
incl |
12.0 |
1.20 |
4.6 |
0.0 |
|
|
KYAC0187 |
25.0 |
0.95 |
4.1 |
0.0 |
AC |
|
incl |
5.0 |
1.39 |
2.4 |
0.0 |
|
|
KYAC0188 |
9.0 |
0.90 |
0.4 |
0.0 |
AC |
|
incl |
4.0 |
1.15 |
0.3 |
0.0 |
|
|
KYAC0189 |
21.0 |
1.08 |
4.6 |
0.0 |
AC |
|
incl |
12.0 |
1.34 |
4.2 |
0.0 |
|
|
KYAC0190 |
16.0 |
1.01 |
3.9 |
0.0 |
AC |
|
incl |
5.0 |
1.47 |
2.1 |
0.0 |
|
|
KYAC0191 |
25.0 |
1.08 |
5.2 |
0.0 |
AC |
|
incl |
5.0 |
1.88 |
1.2 |
0.0 |
|
|
KYPT0222 |
6.0 |
1.33 |
0.3 |
0.0 |
PT |
|
incl |
2.0 |
2.30 |
0.3 |
0.0 |
|
|
KYPT0223 |
7.0 |
1.06 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
2.07 |
0.2 |
0.0 |
|
|
KYPT0224 |
6.0 |
1.34 |
0.7 |
0.0 |
PT |
|
incl |
3.0 |
1.75 |
0.4 |
0.0 |
|
|
KYPT0225 |
3.0 |
1.28 |
0.0 |
0.0 |
PT |
|
KYPT0226 |
2.0 |
0.82 |
0.1 |
0.0 |
PT |
|
incl |
0.5 |
1.58 |
0.0 |
0.0 |
|
|
KYPT0227 |
4.0 |
1.51 |
0.3 |
0.0 |
PT |
|
incl |
3.0 |
1.77 |
0.3 |
0.0 |
|
|
KYPT0228 |
6.0 |
1.24 |
0.4 |
0.0 |
PT |
|
incl |
2.0 |
1.98 |
0.2 |
0.0 |
|
|
KYPT0229 |
11.0 |
1.02 |
2.4 |
0.0 |
PT |
|
incl |
2.0 |
1.74 |
0.6 |
0.0 |
|
|
KYPT0230 |
7.0 |
0.93 |
0.6 |
0.0 |
PT |
|
incl |
1.0 |
2.02 |
0.3 |
0.0 |
|
|
KYPT0231 |
8.0 |
0.98 |
0.4 |
0.0 |
PT |
|
incl |
4.0 |
1.39 |
0.2 |
0.0 |
|
|
KYPT0232 |
2.0 |
1.02 |
0.2 |
0.0 |
PT |
|
KYPT0233 |
11.0 |
1.70 |
1.4 |
0.0 |
PT |
|
incl |
3.0 |
2.13 |
0.3 |
0.0 |
|
|
KYPT0234 |
9.0 |
1.16 |
0.7 |
0.0 |
PT |
|
incl |
4.0 |
1.74 |
0.2 |
0.0 |
|
|
KYPT0235 |
7.0 |
1.67 |
0.5 |
0.0 |
PT |
|
incl |
6.0 |
1.79 |
0.4 |
0.0 |
|
|
KYPT0236 |
2.0 |
2.16 |
0.2 |
0.0 |
PT |
|
KYPT0237 |
1.0 |
1.21 |
0.2 |
0.0 |
PT |
|
KYPT0238 |
3.0 |
1.49 |
0.8 |
0.0 |
PT |
|
incl |
2.0 |
1.80 |
0.6 |
0.0 |
|
|
KYPT0239 |
5.0 |
1.11 |
0.5 |
0.0 |
PT |
|
incl |
1.0 |
2.50 |
0.2 |
0.0 |
|
|
KYPT0240 |
1.0 |
1.72 |
0.4 |
0.0 |
PT |
|
KYPT0241 |
2.0 |
1.30 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
1.71 |
0.0 |
0.0 |
|
|
KYPT0242 |
10.0 |
0.92 |
1.2 |
0.0 |
PT |
|
incl |
1.0 |
2.32 |
0.0 |
0.0 |
|
|
KYPT0243 |
0.4 |
1.04 |
3.8 |
0.0 |
PT |
|
KYPT0244 |
3.0 |
0.63 |
0.0 |
0.0 |
PT |
|
KYPT0245 |
4.0 |
1.45 |
0.3 |
0.0 |
PT |
|
KYPT0246 |
7.0 |
1.19 |
0.3 |
0.0 |
PT |
|
incl |
2.0 |
2.29 |
0.2 |
0.0 |
|
|
KYPT0247 |
7.0 |
1.17 |
0.8 |
0.0 |
PT |
|
incl |
2.0 |
2.01 |
0.2 |
0.0 |
|
|
KYPT0248 |
2.0 |
1.57 |
0.2 |
0.0 |
PT |
|
KYPT0249 |
2.0 |
0.95 |
0.0 |
0.0 |
PT |
|
KYPT0250 |
3.0 |
1.19 |
0.2 |
0.0 |
PT |
|
KYPT0251 |
8.0 |
0.79 |
0.7 |
0.0 |
PT |
|
incl |
1.0 |
1.69 |
0.0 |
0.0 |
|
|
KYPT0252 |
7.0 |
0.89 |
0.6 |
0.0 |
PT |
|
incl |
1.0 |
2.11 |
0.0 |
0.0 |
|
|
KYPT0253 |
2.0 |
1.67 |
1.3 |
0.0 |
PT |
|
KYPT0254 |
7.0 |
1.11 |
1.1 |
0.0 |
PT |
|
incl |
2.0 |
1.70 |
0.3 |
0.0 |
|
|
KYPT0255 |
12.0 |
1.13 |
1.0 |
0.0 |
PT |
|
incl |
2.0 |
1.59 |
0.3 |
0.0 |
|
|
KYPT0256 |
12.0 |
1.00 |
0.8 |
0.0 |
PT TWIN |
|
incl |
2.0 |
1.68 |
0.3 |
0.0 |
|
|
KYPT0257 |
5.0 |
1.45 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
2.10 |
0.2 |
0.0 |
|
|
KYPT0258 |
10.0 |
1.02 |
1.2 |
0.0 |
PT |
|
incl |
3.0 |
1.86 |
0.4 |
0.0 |
|
|
KYPT0259 |
12.0 |
1.36 |
0.7 |
0.0 |
PT |
|
incl |
7.0 |
1.63 |
0.3 |
0.0 |
|
|
KYPT0260 |
5.0 |
0.84 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.19 |
0.1 |
0.0 |
|
|
KYPT0261 |
3.0 |
1.13 |
0.5 |
0.0 |
PT |
|
incl |
2.0 |
1.29 |
0.5 |
0.0 |
|
|
KYPT0262 |
0.2 |
1.02 |
0.0 |
0.0 |
PT |
|
KYPT0263 |
3.0 |
1.69 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
2.08 |
0.3 |
0.0 |
|
|
KYPT0264 |
3.0 |
1.77 |
0.3 |
0.0 |
PT |
|
incl |
2.0 |
2.18 |
0.4 |
0.0 |
|
|
KYPT0265 |
6.0 |
0.74 |
0.7 |
0.0 |
PT |
|
incl |
1.0 |
1.41 |
0.1 |
0.0 |
|
|
KYPT0266 |
4.0 |
0.76 |
0.0 |
0.0 |
PT |
|
incl |
1.0 |
1.43 |
0.2 |
0.0 |
|
|
KYPT0267 |
NSR |
PT |
|||
|
KYPT0268 |
3.0 |
0.95 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.69 |
0.2 |
0.0 |
|
|
KYPT0269 |
2.0 |
0.69 |
0.6 |
0.0 |
PT |
|
KYPT0270 |
9.0 |
0.84 |
2.3 |
0.0 |
PT |
|
incl |
2.0 |
1.54 |
0.5 |
0.0 |
|
|
KYPT0271 |
2.0 |
0.61 |
0.2 |
0.0 |
PT |
|
KYPT0272 |
2.0 |
1.43 |
0.3 |
0.0 |
PT |
|
KYPT0273 |
2.0 |
1.41 |
0.3 |
0.0 |
PT |
|
KYPT0274 |
3.0 |
1.30 |
0.2 |
0.0 |
PT |
|
KYPT0275 |
3.0 |
0.99 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.88 |
0.3 |
0.0 |
|
|
KYPT0276 |
3.0 |
1.03 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
1.39 |
0.2 |
0.0 |
|
|
KYPT0277 |
4.0 |
0.86 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.15 |
0.2 |
0.0 |
|
|
KYPT0278 |
10.5 |
1.03 |
1.7 |
0.0 |
PT |
|
incl |
1.0 |
2.07 |
0.5 |
0.0 |
|
|
KYPT0279 |
3.0 |
1.03 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.35 |
0.3 |
0.0 |
|
|
KYPT0280 |
3.0 |
1.04 |
0.2 |
0.0 |
PT |
|
KYPT0281 |
4.6 |
0.84 |
0.9 |
0.0 |
PT |
|
KYPT0282 |
7.9 |
0.95 |
0.6 |
0.0 |
PT |
|
incl |
1.0 |
2.04 |
0.4 |
0.0 |
|
|
KYPT0283 |
3.8 |
1.74 |
0.1 |
0.0 |
PT |
|
KYPT0284 |
1.0 |
0.91 |
0.2 |
0.0 |
PT |
|
KYPT0285 |
3.0 |
2.01 |
0.1 |
0.0 |
PT |
|
KYPT0286 |
2.0 |
1.18 |
0.2 |
0.0 |
PT |
|
KYPT0287 |
6.1 |
0.90 |
1.2 |
0.0 |
PT |
|
incl |
1.0 |
2.26 |
0.0 |
0.0 |
|
|
KYPT0288 |
6.0 |
1.16 |
0.6 |
0.0 |
PT |
|
incl |
1.0 |
3.13 |
0.4 |
0.0 |
|
|
KYPT0289 |
4.0 |
0.66 |
0.3 |
0.0 |
PT |
|
KYPT0290 |
2.0 |
0.68 |
0.0 |
0.0 |
PT |
|
KYPT0291 |
2.0 |
0.77 |
0.0 |
0.0 |
PT |
|
KYPT0292 |
4.0 |
0.73 |
0.2 |
0.0 |
PT |
|
KYPT0293 |
1.0 |
1.45 |
0.0 |
0.0 |
PT |
|
KYPT0294 |
2.0 |
0.74 |
0.2 |
0.0 |
PT |
|
KYPT0295 |
5.0 |
0.92 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.94 |
0.2 |
0.0 |
|
|
KYPT0296 |
2.0 |
1.66 |
0.1 |
0.0 |
PT |
|
KYPT0297 |
9.0 |
1.11 |
1.0 |
0.0 |
PT |
|
incl |
2.0 |
1.97 |
0.1 |
0.0 |
|
|
KYPT0298 |
4.0 |
0.75 |
0.0 |
0.0 |
PT |
|
incl |
1.0 |
1.42 |
0.0 |
0.0 |
|
|
KYPT0299 |
3.0 |
0.95 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
1.41 |
0.2 |
0.0 |
|
|
KYPT0300 |
4.0 |
0.97 |
0.0 |
0.0 |
PT |
|
incl |
2.0 |
1.21 |
0.0 |
0.0 |
|
|
KYPT0301 |
3.0 |
1.48 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.90 |
0.3 |
0.0 |
|
|
KYPT0302 |
8.0 |
1.13 |
0.4 |
0.0 |
PT |
|
incl |
3.0 |
1.67 |
0.0 |
0.0 |
|
|
KYPT0303 |
4.0 |
0.70 |
1.4 |
0.0 |
PT |
|
KYPT0304 |
4.0 |
1.04 |
0.9 |
0.0 |
PT TWIN |
|
incl |
1.0 |
2.06 |
0.6 |
0.0 |
|
|
KYPT0305 |
5.9 |
1.11 |
0.0 |
0.0 |
PT |
|
incl |
3.0 |
1.42 |
0.0 |
0.0 |
|
|
KYPT0306 |
2.6 |
1.53 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
2.87 |
0.2 |
0.0 |
|
|
KYPT0307 |
10.0 |
0.91 |
3.3 |
0.0 |
PT |
|
incl |
3.0 |
1.39 |
0.5 |
0.0 |
|
|
KYPT0308 |
1.0 |
1.10 |
0.3 |
0.0 |
PT |
|
KYPT0309 |
9.0 |
0.81 |
0.7 |
0.0 |
PT |
|
KYPT0310 |
3.0 |
0.89 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.00 |
0.2 |
0.0 |
|
|
KYPT0311 |
3.0 |
1.62 |
0.2 |
0.0 |
PT |
|
KYPT0312 |
3.0 |
1.08 |
0.4 |
0.0 |
PT |
|
KYPT0313 |
3.0 |
1.26 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.43 |
0.2 |
0.0 |
|
|
KYPT0314 |
3.8 |
1.37 |
1.1 |
0.0 |
PT |
|
incl |
2.0 |
1.78 |
0.5 |
0.0 |
|
|
KYPT0315 |
3.0 |
0.97 |
0.4 |
0.0 |
PT |
|
incl |
2.0 |
1.16 |
0.4 |
0.0 |
|
|
KYPT0316 |
5.0 |
1.05 |
1.0 |
0.0 |
PT |
|
incl |
1.7 |
1.92 |
0.6 |
0.0 |
|
|
KYPT0317 |
2.0 |
0.77 |
0.4 |
0.0 |
PT |
|
KYPT0318 |
4.2 |
1.35 |
0.2 |
0.0 |
PT |
|
KYPT0319 |
4.1 |
1.05 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.40 |
0.3 |
0.0 |
|
|
KYPT0320 |
5.0 |
0.84 |
0.3 |
0.0 |
PT |
|
incl |
1.5 |
1.36 |
0.2 |
0.0 |
|
|
KYPT0321 |
11.0 |
0.86 |
1.0 |
0.0 |
PT |
|
incl |
2.4 |
1.58 |
0.2 |
0.0 |
|
|
KYPT0322 |
1.0 |
1.42 |
0.3 |
0.0 |
PT |
|
KYPT0323 |
1.8 |
1.09 |
0.4 |
0.0 |
PT |
|
KYPT0324 |
3.0 |
1.41 |
0.5 |
0.0 |
PT |
|
incl |
1.7 |
1.95 |
0.5 |
0.0 |
|
|
KYPT0325 |
4.1 |
1.02 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.42 |
0.2 |
0.0 |
|
|
KYPT0326 |
4.2 |
1.02 |
0.1 |
0.0 |
PT TWIN |
|
incl |
2.0 |
1.46 |
0.2 |
0.0 |
|
|
KYPT0327 |
3.0 |
1.12 |
0.0 |
0.0 |
PT |
|
incl |
1.0 |
1.99 |
0.0 |
0.0 |
|
|
KYPT0328 |
8.0 |
1.00 |
1.5 |
0.0 |
PT |
|
incl |
1.0 |
1.18 |
1.9 |
0.0 |
|
|
KYPT0329 |
2.0 |
0.65 |
0.4 |
0.0 |
PT |
|
KYPT0330 |
7.0 |
1.14 |
0.4 |
0.0 |
PT TWIN |
|
incl |
3.0 |
1.82 |
0.3 |
0.0 |
|
|
KYPT0331 |
4.2 |
0.83 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.13 |
0.2 |
0.0 |
|
|
KYPT0332 |
1.0 |
0.63 |
0.2 |
0.0 |
PT |
|
KYPT0333 |
8.6 |
0.98 |
1.0 |
0.0 |
PT |
|
incl |
1.4 |
1.51 |
0.3 |
0.0 |
|
|
KYPT0334 |
2.0 |
0.60 |
0.2 |
0.0 |
PT |
|
KYPT0335 |
3.7 |
0.67 |
0.8 |
0.0 |
PT |
|
KYPT0336 |
2.0 |
1.62 |
0.1 |
0.0 |
PT |
|
KYPT0337 |
14.2 |
0.80 |
3.4 |
0.0 |
PT |
|
incl |
1.0 |
1.28 |
0.6 |
0.0 |
|
|
KYPT0338 |
5.5 |
1.25 |
0.8 |
0.0 |
PT |
|
incl |
1.0 |
2.38 |
0.4 |
0.0 |
|
|
KYPT0339 |
4.0 |
1.50 |
0.7 |
0.0 |
PT |
|
incl |
2.4 |
1.93 |
0.4 |
0.0 |
|
|
KYPT0340 |
6.0 |
0.98 |
4.0 |
0.0 |
PT |
|
KYPT0341 |
14.6 |
1.05 |
1.2 |
0.0 |
PT |
|
incl |
2.9 |
1.53 |
0.4 |
0.0 |
|
|
KYPT0342 |
6.0 |
1.30 |
2.9 |
0.0 |
PT |
|
incl |
4.7 |
1.40 |
3.6 |
1.3 |
|
|
KYPT0343 |
7.0 |
1.11 |
0.9 |
0.0 |
PT |
|
incl |
1.0 |
2.33 |
0.5 |
0.0 |
|
|
KYPT0344 |
7.0 |
1.01 |
1.4 |
0.0 |
PT |
|
incl |
1.4 |
1.29 |
0.3 |
0.0 |
|
|
KYPT0345 |
3.4 |
0.99 |
0.4 |
0.0 |
PT |
|
incl |
2.0 |
1.32 |
0.5 |
0.0 |
|
|
KYPT0346 |
2.0 |
1.70 |
0.5 |
0.0 |
PT |
|
KYPT0347 |
10.0 |
0.88 |
2.3 |
0.0 |
PT |
|
incl |
1.9 |
1.82 |
4.4 |
0.0 |
|
|
KYPT0348 |
6.0 |
1.00 |
0.7 |
0.0 |
PT |
|
incl |
2.0 |
1.55 |
0.2 |
0.0 |
|
|
KYPT0349 |
4.0 |
0.83 |
5.0 |
4.5 |
PT |
|
KYPT0350 |
10.0 |
0.82 |
3.0 |
0.0 |
PT |
|
incl |
1.0 |
1.83 |
0.5 |
0.0 |
|
|
KYPT0351 |
3.8 |
1.20 |
0.5 |
0.0 |
PT |
|
incl |
2.0 |
1.49 |
0.5 |
0.0 |
|
|
KYPT0352 |
5.0 |
1.41 |
0.3 |
0.0 |
PT |
|
KYPT0353 |
12.2 |
0.94 |
3.6 |
0.0 |
PT |
|
incl |
4.6 |
1.31 |
1.0 |
0.0 |
|
|
KYPT0354 |
13.0 |
0.90 |
1.5 |
0.0 |
PT |
|
incl |
3.7 |
1.15 |
0.2 |
0.0 |
|
|
KYPT0355 |
7.0 |
0.99 |
2.0 |
0.0 |
PT |
|
incl |
1.8 |
1.75 |
0.5 |
0.0 |
|
|
KYPT0356 |
5.0 |
0.83 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.18 |
0.2 |
0.0 |
|
|
KYPT0357 |
4.0 |
0.87 |
0.1 |
0.0 |
PT TWIN |
|
incl |
1.0 |
1.44 |
0.2 |
0.0 |
|
|
KYPT0358 |
13.0 |
1.12 |
2.0 |
0.0 |
PT |
|
incl |
2.5 |
2.06 |
0.2 |
0.0 |
|
|
KYPT0359 |
11.0 |
1.20 |
2.6 |
0.0 |
PT |
|
incl |
4.0 |
1.72 |
0.7 |
0.0 |
|
|
KYPT0360 |
11.0 |
1.27 |
1.7 |
0.0 |
PT |
|
incl |
9.0 |
1.40 |
1.6 |
0.0 |
|
|
KYPT0361 |
5.2 |
0.95 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.45 |
0.2 |
0.0 |
|
|
KYPT0362 |
5.0 |
1.27 |
0.3 |
0.0 |
PT |
|
incl |
2.0 |
2.06 |
0.2 |
0.0 |
|
|
KYPT0363 |
13.4 |
0.90 |
2.7 |
0.0 |
PT |
|
incl |
1.3 |
1.60 |
0.0 |
0.0 |
|
|
KYPT0364 |
7.0 |
1.26 |
2.5 |
0.0 |
PT |
|
incl |
3.0 |
1.80 |
1.1 |
0.0 |
|
|
KYPT0365 |
7.0 |
0.76 |
1.3 |
0.0 |
PT |
|
KYPT0366 |
4.0 |
0.77 |
0.8 |
0.0 |
PT |
|
KYPT0367 |
10.6 |
0.95 |
2.0 |
0.0 |
PT |
|
incl |
2.0 |
1.97 |
0.3 |
0.0 |
|
|
KYPT0368 |
8.3 |
0.79 |
0.6 |
0.0 |
PT |
|
incl |
3.0 |
1.19 |
0.2 |
0.0 |
|
|
KYPT0369 |
8.0 |
0.95 |
3.2 |
0.0 |
PT |
|
incl |
2.6 |
1.39 |
0.5 |
0.0 |
|
|
KYPT0370 |
1.5 |
1.84 |
0.1 |
0.0 |
PT |
|
incl |
1.5 |
1.84 |
0.1 |
0.0 |
|
|
KYPT0371 |
12.5 |
0.92 |
1.5 |
0.0 |
PT |
|
incl |
2.0 |
1.90 |
0.4 |
0.0 |
|
|
KYPT0372 |
15.0 |
0.55 |
4.4 |
0.0 |
PT |
|
incl |
0.7 |
1.18 |
1.5 |
0.0 |
|
|
KYPT0373 |
13.3 |
1.19 |
2.4 |
0.0 |
PT |
|
incl |
1.0 |
2.29 |
0.4 |
0.0 |
|
|
KYPT0374 |
5.4 |
1.17 |
1.6 |
0.0 |
PT |
|
incl |
1.2 |
2.32 |
0.3 |
0.0 |
|
|
KYPT0375 |
9.0 |
1.08 |
1.1 |
0.0 |
PT |
|
incl |
2.5 |
1.66 |
0.4 |
0.0 |
|
|
KYPT0376 |
7.0 |
1.22 |
0.7 |
0.0 |
PT |
|
incl |
2.9 |
1.79 |
0.2 |
0.0 |
|
|
KYPT0377 |
2.0 |
1.70 |
0.3 |
0.0 |
PT |
|
KYPT0378 |
4.1 |
1.31 |
0.2 |
0.0 |
PT TWIN |
|
incl |
2.0 |
1.80 |
0.1 |
0.0 |
|
|
KYPT0379 |
9.0 |
1.28 |
1.3 |
0.0 |
PT |
|
incl |
4.0 |
1.68 |
1.7 |
5.0 |
|
|
KYPT0380 |
2.0 |
1.30 |
0.5 |
0.0 |
PT |
|
KYPT0381 |
8.0 |
1.09 |
2.5 |
0.0 |
PT |
|
KYPT0382 |
3.8 |
1.80 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
2.31 |
0.2 |
0.0 |
|
|
KYPT0383 |
8.0 |
0.91 |
3.5 |
0.0 |
PT |
|
incl |
1.6 |
1.76 |
0.7 |
0.0 |
|
|
KYPT0384 |
1.8 |
1.62 |
0.4 |
0.0 |
PT |
|
incl |
1.0 |
2.35 |
0.4 |
0.0 |
|
|
KYPT0385 |
3.2 |
0.67 |
0.3 |
0.9 |
PT |
|
KYPT0386 |
8.3 |
0.85 |
1.1 |
0.0 |
PT |
|
incl |
1.6 |
1.61 |
0.0 |
0.0 |
|
|
KYPT0387 |
6.0 |
0.87 |
0.6 |
0.0 |
PT |
|
incl |
1.6 |
1.36 |
0.4 |
0.0 |
|
|
KYPT0388 |
14.0 |
1.09 |
1.3 |
0.0 |
PT |
|
incl |
4.0 |
1.57 |
0.1 |
0.0 |
|
|
KYPT0389 |
10.7 |
1.04 |
3.4 |
0.0 |
PT |
|
incl |
2.0 |
1.94 |
0.3 |
0.0 |
|
|
KYPT0390 |
11.5 |
0.97 |
4.4 |
0.0 |
PT |
|
incl |
2.0 |
2.06 |
0.5 |
0.0 |
|
|
KYPT0391 |
15.0 |
1.03 |
6.4 |
0.0 |
PT |
|
incl |
1.7 |
2.16 |
0.6 |
0.0 |
|
|
KYPT0392 |
8.0 |
1.17 |
2.9 |
0.0 |
PT |
|
incl |
2.4 |
1.70 |
0.5 |
0.0 |
|
|
KYPT0393 |
12.8 |
1.26 |
4.2 |
0.0 |
PT |
|
incl |
9.0 |
1.45 |
2.5 |
0.0 |
|
|
KYPT0394 |
4.0 |
0.98 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.20 |
0.2 |
0.0 |
|
|
KYPT0395 |
11.0 |
1.00 |
2.6 |
0.0 |
PT |
|
incl |
5.0 |
1.42 |
2.2 |
0.0 |
|
|
KYPT0396 |
5.8 |
0.91 |
0.1 |
0.0 |
PT |
|
incl |
2.7 |
1.35 |
0.0 |
0.0 |
|
|
KYPT0397 |
2.8 |
1.84 |
0.2 |
0.0 |
PT |
|
KYPT0398 |
1.0 |
0.89 |
1.7 |
5.0 |
PT |
|
KYPT0399 |
6.0 |
0.97 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.34 |
0.2 |
0.0 |
|
|
KYPT0400 |
8.0 |
0.62 |
1.9 |
2.0 |
PT |
|
KYPT0401 |
3.0 |
0.86 |
0.0 |
0.0 |
PT |
|
incl |
0.9 |
1.57 |
0.2 |
0.0 |
|
|
KYPT0402 |
2.8 |
2.26 |
0.0 |
0.0 |
PT |
|
KYPT0403 |
4.5 |
0.93 |
0.0 |
0.0 |
PT |
|
incl |
3.0 |
1.09 |
0.0 |
0.0 |
|
|
KYPT0404 |
4.3 |
0.94 |
0.0 |
0.0 |
PT TWIN |
|
incl |
3.0 |
1.09 |
0.0 |
0.0 |
|
|
KYPT0405 |
6.3 |
1.17 |
0.7 |
0.0 |
PT |
|
incl |
2.8 |
1.73 |
0.3 |
0.0 |
|
|
KYPT0406 |
10.0 |
0.78 |
1.4 |
0.0 |
PT |
|
KYPT0407 |
11.7 |
1.12 |
2.4 |
0.0 |
PT |
|
incl |
7.0 |
1.35 |
2.0 |
0.0 |
|
|
KYPT0408 |
7.0 |
0.99 |
0.1 |
0.0 |
PT |
|
incl |
4.5 |
1.17 |
0.1 |
0.0 |
|
|
KYPT0409 |
1.0 |
2.74 |
0.3 |
0.0 |
PT |
|
KYPT0410 |
6.0 |
0.93 |
0.1 |
0.0 |
PT |
|
incl |
2.0 |
1.22 |
0.1 |
0.0 |
|
|
KYPT0411 |
5.0 |
1.00 |
0.6 |
0.0 |
PT |
|
incl |
2.0 |
1.49 |
0.3 |
0.0 |
|
|
KYPT0412 |
1.0 |
0.94 |
0.4 |
0.0 |
PT |
|
incl |
1.0 |
1.06 |
2.8 |
9.0 |
|
|
KYPT0413 |
8.0 |
0.90 |
3.7 |
0.0 |
PT |
|
incl |
1.0 |
1.53 |
0.4 |
0.0 |
|
|
KYPT0414 |
3.0 |
0.68 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
1.01 |
0.2 |
0.0 |
|
|
KYPT0415 |
11.0 |
1.09 |
0.7 |
0.0 |
PT |
|
incl |
3.4 |
1.83 |
0.2 |
0.0 |
|
|
KYPT0416 |
5.0 |
1.08 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.55 |
0.2 |
0.0 |
|
|
KYPT0417 |
8.3 |
0.90 |
0.7 |
0.0 |
PT |
|
incl |
1.4 |
2.06 |
0.2 |
0.0 |
|
|
KYPT0418 |
13.6 |
1.15 |
2.3 |
0.0 |
PT |
|
incl |
2.0 |
2.02 |
0.3 |
0.0 |
|
|
KYPT0419 |
2.8 |
1.15 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.50 |
0.3 |
0.0 |
|
|
KYPT0420 |
6.0 |
0.98 |
0.0 |
0.0 |
PT |
|
incl |
3.0 |
1.39 |
0.0 |
0.0 |
|
|
KYPT0421 |
11.0 |
1.00 |
3.3 |
0.0 |
PT |
|
incl |
4.0 |
1.39 |
1.4 |
0.0 |
|
|
KYPT0422 |
6.0 |
1.10 |
0.4 |
0.0 |
PT |
|
incl |
4.7 |
1.23 |
0.3 |
0.0 |
|
|
KYPT0423 |
4.0 |
0.90 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
1.44 |
0.2 |
0.0 |
|
|
KYPT0424 |
10.8 |
1.11 |
1.5 |
0.0 |
PT |
|
incl |
6.0 |
1.43 |
0.8 |
0.0 |
|
|
KYPT0425 |
14.0 |
1.11 |
1.5 |
0.0 |
PT |
|
incl |
2.0 |
1.84 |
0.3 |
0.0 |
|
|
KYPT0426 |
2.0 |
0.70 |
0.2 |
0.0 |
PT |
|
KYPT0427 |
5.5 |
1.05 |
0.0 |
0.0 |
|
|
incl |
2.9 |
1.51 |
0.0 |
0.0 |
|
|
KYPT0428 |
3.6 |
1.21 |
0.2 |
0.0 |
PT |
|
KYPT0429 |
1.7 |
1.35 |
0.2 |
0.0 |
PT |
|
KYPT0430 |
3.8 |
1.03 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.45 |
0.2 |
0.0 |
|
|
KYPT0431 |
3.5 |
1.15 |
0.3 |
0.0 |
PT TWIN |
|
incl |
2.0 |
1.48 |
0.3 |
0.0 |
|
|
KYPT0432 |
6.0 |
0.76 |
1.1 |
0.0 |
PT |
|
incl |
0.5 |
2.77 |
0.0 |
0.0 |
|
|
KYPT0433 |
1.0 |
2.40 |
0.3 |
0.0 |
PT |
|
KYPT0434 |
4.0 |
1.92 |
0.1 |
0.0 |
PT |
|
incl |
1.0 |
2.40 |
0.3 |
0.0 |
|
|
KYPT0435 |
10.0 |
1.06 |
0.7 |
0.0 |
PT |
|
incl |
4.7 |
1.52 |
0.1 |
0.0 |
|
|
KYPT0436 |
9.0 |
1.17 |
0.9 |
0.0 |
PT |
|
incl |
3.4 |
1.85 |
0.2 |
0.0 |
|
|
KYPT0437 |
2.4 |
0.91 |
0.1 |
2.0 |
PT |
|
KYPT0438 |
6.0 |
1.26 |
0.7 |
0.0 |
PT |
|
incl |
4.0 |
1.55 |
0.3 |
0.0 |
|
|
KYPT0439 |
2.0 |
1.01 |
0.3 |
0.0 |
PT |
|
KYPT0440 |
5.4 |
0.75 |
1.0 |
0.0 |
PT |
|
KYPT0441 |
5.0 |
1.19 |
0.1 |
0.0 |
PT |
|
incl |
3.0 |
1.57 |
0.2 |
0.0 |
|
|
KYPT0442 |
10.0 |
0.93 |
2.0 |
0.0 |
PT |
|
KYPT0443 |
3.7 |
0.93 |
0.2 |
0.0 |
PT |
|
incl |
2.0 |
1.13 |
0.2 |
0.0 |
|
|
KYPT0444 |
3.8 |
1.01 |
0.7 |
0.0 |
PT |
|
incl |
1.3 |
1.18 |
0.8 |
2.0 |
|
|
KYPT0445 |
2.9 |
1.27 |
1.9 |
0.0 |
PT |
|
incl |
1.9 |
1.66 |
0.8 |
0.0 |
|
|
KYPT0446 |
3.0 |
0.65 |
0.3 |
0.0 |
PT |
|
KYPT0447 |
2.1 |
0.73 |
1.8 |
9.4 |
PT |
|
KYPT0448 |
7.0 |
1.07 |
0.7 |
0.0 |
PT |
|
incl |
3.8 |
1.28 |
0.3 |
0.0 |
|
|
KYPT0449 |
8.0 |
1.13 |
0.5 |
0.0 |
PT |
|
incl |
3.3 |
1.66 |
0.2 |
0.0 |
|
|
KYPT0450 |
5.0 |
1.22 |
0.3 |
0.0 |
PT |
|
incl |
1.9 |
1.81 |
0.2 |
0.0 |
|
|
KYPT0451 |
9.0 |
1.01 |
0.7 |
0.0 |
PT |
|
incl |
2.2 |
1.63 |
0.3 |
0.0 |
|
|
KYPT0452 |
10.0 |
1.00 |
2.4 |
0.0 |
PT |
|
incl |
1.7 |
1.55 |
0.3 |
0.0 |
|
|
KYPT0453 |
3.0 |
1.02 |
0.3 |
0.0 |
PT |
|
incl |
1.7 |
1.34 |
0.3 |
0.0 |
|
|
KYPT0454 |
9.0 |
0.95 |
0.8 |
0.0 |
PT |
|
incl |
2.0 |
1.74 |
0.5 |
0.0 |
|
|
KYPT0455 |
4.0 |
1.43 |
0.3 |
0.0 |
PT |
|
incl |
2.0 |
1.88 |
0.3 |
0.0 |
|
|
KYPT0456 |
5.0 |
1.10 |
0.3 |
0.0 |
PT |
|
incl |
2.9 |
1.47 |
0.2 |
0.0 |
|
|
KYPT0457 |
2.4 |
1.11 |
0.2 |
0.0 |
PT |
|
incl |
1.0 |
1.84 |
0.3 |
0.0 |
|
|
KYPT0458 |
1.0 |
1.02 |
0.4 |
0.0 |
PT |
|
KYPT0459 |
8.0 |
0.80 |
2.0 |
0.0 |
PT |
|
incl |
1.0 |
1.51 |
0.4 |
0.0 |
|
|
KYPT0460 |
1.5 |
1.59 |
0.2 |
0.0 |
PT |
|
KYPT0461 |
1.0 |
1.38 |
0.4 |
0.0 |
PT |
|
KYPT0462 |
2.0 |
1.17 |
0.4 |
0.0 |
PT |
|
KYPT0463 |
2.0 |
1.58 |
0.3 |
0.0 |
PT |
|
KYPT0464 |
5.0 |
0.78 |
1.1 |
0.0 |
PT |
|
KYPT0465 |
1.1 |
1.17 |
0.4 |
0.0 |
PT |
|
KYPT0466 |
2.0 |
1.75 |
0.3 |
0.0 |
PT |
|
KYPT0467 |
NSR |
PT |
|||
|
KYPT0468 |
NSR |
PT |
APPENDIX II: DRILL HOLE COLLAR DATA – TABLE 3
|
Hole ID |
Easting |
Northing |
RL |
Depth |
|
Hole ID |
Easting |
Northing |
RL |
Depth |
|
KYAC0094 |
549202 |
8479802 |
1129 |
23.0 |
KYAC0137 |
544001 |
8468400 |
1137 |
24.0 |
|
|
KYAC0095 |
549400 |
8479802 |
1128 |
30.0 |
KYAC0138 |
543800 |
8468400 |
1132 |
16.0 |
|
|
KYAC0096 |
549600 |
8479776 |
1126 |
34.0 |
KYAC0139 |
543597 |
8468400 |
1127 |
28.0 |
|
|
KYAC0097 |
549778 |
8479810 |
1123 |
27.0 |
KYAC0140 |
543599 |
8468001 |
1132 |
27.0 |
|
|
KYAC0098 |
548998 |
8479395 |
1135 |
33.0 |
KYAC0141 |
543800 |
8468000 |
1138 |
24.0 |
|
|
KYAC0099 |
549198 |
8479401 |
1133 |
26.0 |
KYAC0142 |
544000 |
8467999 |
1141 |
25.5 |
|
|
KYAC0100 |
549400 |
8479401 |
1131 |
29.0 |
KYAC0143 |
544000 |
8468000 |
1141 |
25.5 |
|
|
KYAC0101 |
549600 |
8479402 |
1128 |
25.0 |
KYAC0144 |
543799 |
8467801 |
1140 |
25.0 |
|
|
KYAC0102 |
549800 |
8479402 |
1126 |
28.0 |
KYAC0145 |
544001 |
8467801 |
1143 |
24.0 |
|
|
KYAC0103 |
549800 |
8479402 |
1126 |
28.0 |
KYAC0146 |
543599 |
8467803 |
1135 |
26.5 |
|
|
KYAC0104 |
549600 |
8479603 |
1129 |
27.0 |
KYAC0147 |
543600 |
8467601 |
1136 |
21.0 |
|
|
KYAC0105 |
549401 |
8479600 |
1131 |
25.8 |
KYAC0148 |
543800 |
8467605 |
1141 |
21.0 |
|
|
KYAC0106 |
549799 |
8479600 |
1126 |
25.0 |
KYAC0149 |
544000 |
8467600 |
1144 |
33.0 |
|
|
KYAC0107 |
549200 |
8479600 |
1132 |
20.0 |
KYAC0150 |
543800 |
8467401 |
1143 |
30.0 |
|
|
KYAC0108 |
549000 |
8479802 |
1128 |
22.7 |
KYAC0151 |
544001 |
8467401 |
1145 |
24.0 |
|
|
KYAC0109 |
548798 |
8479195 |
1138 |
25.0 |
KYAC0152 |
544402 |
8467801 |
1144 |
28.6 |
|
|
KYAC0110 |
548799 |
8479000 |
1138 |
27.0 |
KYAC0153 |
545000 |
8465600 |
1162 |
22.0 |
|
|
KYAC0111 |
548600 |
8478999 |
1141 |
29.0 |
KYAC0154 |
545200 |
8465601 |
1163 |
21.0 |
|
|
KYAC0112 |
548399 |
8478999 |
1143 |
25.0 |
KYAC0155 |
545201 |
8465799 |
1161 |
28.0 |
|
|
KYAC0113 |
548801 |
8478799 |
1138 |
19.8 |
KYAC0156 |
545399 |
8465201 |
1167 |
24.0 |
|
|
KYAC0114 |
548600 |
8478799 |
1141 |
14.0 |
KYAC0157 |
545200 |
8465202 |
1164 |
28.0 |
|
|
KYAC0115 |
548401 |
8478800 |
1143 |
32.0 |
KYAC0158 |
544996 |
8465204 |
1161 |
28.0 |
|
|
KYAC0116 |
548201 |
8478801 |
1145 |
24.8 |
KYAC0159 |
545201 |
8465000 |
1164 |
34.0 |
|
|
KYAC0117 |
549399 |
8478799 |
1124 |
15.0 |
KYAC0160 |
545398 |
8465001 |
1167 |
35.0 |
|
|
KYAC0118 |
549204 |
8478815 |
1128 |
22.0 |
KYAC0161 |
545400 |
8464801 |
1167 |
30.0 |
|
|
KYAC0119 |
549002 |
8478801 |
1134 |
27.0 |
KYAC0162 |
545600 |
8465000 |
1169 |
35.0 |
|
|
KYAC0120 |
549001 |
8478403 |
1133 |
22.7 |
KYAC0163 |
545600 |
8464999 |
1169 |
35.0 |
|
|
KYAC0121 |
548800 |
8478399 |
1136 |
25.8 |
KYAC0164 |
545600 |
8465200 |
1169 |
27.0 |
|
|
KYAC0122 |
548600 |
8478399 |
1138 |
30.0 |
KYAC0165 |
545400 |
8465600 |
1164 |
27.0 |
|
|
KYAC0123 |
548599 |
8478399 |
1138 |
30.0 |
KYAC0166 |
545601 |
8465602 |
1164 |
29.0 |
|
|
KYAC0124 |
548400 |
8478398 |
1140 |
24.0 |
KYAC0167 |
545400 |
8465800 |
1160 |
24.0 |
|
|
KYAC0125 |
549000 |
8478200 |
1131 |
24.0 |
KYAC0168 |
545600 |
8465784 |
1160 |
22.6 |
|
|
KYAC0126 |
548799 |
8478200 |
1134 |
28.0 |
KYAC0169 |
545800 |
8465601 |
1164 |
20.0 |
|
|
KYAC0127 |
548599 |
8478198 |
1136 |
18.0 |
KYAC0170 |
545800 |
8465800 |
1159 |
27.0 |
|
|
KYAC0128 |
548397 |
8478197 |
1137 |
22.0 |
KYAC0171 |
546000 |
8465800 |
1157 |
29.0 |
|
|
KYAC0129 |
548201 |
8478201 |
1139 |
14.0 |
KYAC0172 |
546000 |
8466201 |
1149 |
18.0 |
|
|
KYAC0130 |
548200 |
8478401 |
1142 |
25.0 |
KYAC0173 |
546002 |
8466001 |
1152 |
25.0 |
|
|
KYAC0131 |
544600 |
8468801 |
1136 |
36.0 |
KYAC0174 |
545999 |
8466401 |
1147 |
13.0 |
|
|
KYAC0132 |
544601 |
8468598 |
1137 |
35.0 |
KYAC0175 |
545998 |
8467403 |
1162 |
19.0 |
|
|
KYAC0133 |
544798 |
8468597 |
1132 |
35.0 |
KYAC0176 |
546200 |
8467400 |
1165 |
26.6 |
|
|
KYAC0134 |
544598 |
8468398 |
1139 |
29.0 |
KYAC0177 |
546400 |
8467399 |
1168 |
23.0 |
|
|
KYAC0135 |
544792 |
8468405 |
1135 |
30.0 |
KYAC0178 |
546400 |
8467600 |
1169 |
21.4 |
|
|
KYAC0136 |
544600 |
8468000 |
1142 |
32.0 |
KYAC0179 |
546200 |
8467601 |
1166 |
26.0 |
|
|
KYAC0180 |
545998 |
8467601 |
1162 |
15.5 |
KYPT0255 |
547793 |
8477399 |
1148 |
12.0 |
|
|
KYAC0181 |
546198 |
8467797 |
1164 |
27.0 |
KYPT0256 |
547793 |
8477400 |
1148 |
12.0 |
|
|
KYAC0182 |
546197 |
8467999 |
1162 |
32.0 |
KYPT0257 |
547401 |
8477398 |
1150 |
11.0 |
|
|
KYAC0183 |
546198 |
8467999 |
1162 |
32.0 |
KYPT0258 |
547000 |
8477000 |
1149 |
10.0 |
|
|
KYAC0184 |
546400 |
8468199 |
1161 |
22.8 |
KYPT0259 |
547395 |
8477000 |
1152 |
12.0 |
|
|
KYAC0185 |
546601 |
8468201 |
1163 |
32.7 |
KYPT0260 |
547800 |
8476999 |
1148 |
11.0 |
|
|
KYAC0186 |
546398 |
8468002 |
1165 |
32.0 |
KYPT0261 |
548201 |
8477000 |
1140 |
6.0 |
|
|
KYAC0187 |
546600 |
8468001 |
1166 |
27.4 |
KYPT0262 |
546604 |
8477001 |
1143 |
8.0 |
|
|
KYAC0188 |
546200 |
8468201 |
1159 |
25.8 |
KYPT0263 |
546999 |
8476604 |
1148 |
8.0 |
|
|
KYAC0189 |
546400 |
8467801 |
1167 |
22.0 |
KYPT0264 |
547399 |
8476604 |
1149 |
9.0 |
|
|
KYAC0190 |
546599 |
8467803 |
1169 |
17.4 |
KYPT0265 |
547801 |
8476601 |
1144 |
6.0 |
|
|
KYAC0191 |
546598 |
8467599 |
1171 |
26.0 |
KYPT0266 |
547387 |
8476200 |
1146 |
4.0 |
|
|
KYPT0222 |
549000 |
8479394 |
1135 |
9.0 |
KYPT0267 |
545001 |
8471800 |
1133 |
8.6 |
|
|
KYPT0223 |
549400 |
8479400 |
1131 |
7.0 |
KYPT0268 |
547000 |
8476199 |
1149 |
9.0 |
|
|
KYPT0224 |
549800 |
8479400 |
1126 |
7.0 |
KYPT0269 |
544998 |
8472202 |
1134 |
10.0 |
|
|
KYPT0225 |
548999 |
8479802 |
1128 |
3.0 |
KYPT0270 |
546605 |
8476211 |
1146 |
9.0 |
|
|
KYPT0226 |
549401 |
8479803 |
1128 |
4.0 |
KYPT0271 |
544598 |
8472601 |
1129 |
3.9 |
|
|
KYPT0227 |
549777 |
8479810 |
1124 |
6.0 |
KYPT0272 |
546197 |
8476198 |
1138 |
7.0 |
|
|
KYPT0228 |
548200 |
8479000 |
1145 |
12.0 |
KYPT0273 |
544200 |
8472600 |
1128 |
3.2 |
|
|
KYPT0229 |
548601 |
8478999 |
1141 |
11.0 |
KYPT0274 |
546199 |
8475798 |
1142 |
9.0 |
|
|
KYPT0230 |
549000 |
8479001 |
1135 |
7.0 |
KYPT0275 |
543800 |
8472600 |
1123 |
8.0 |
|
|
KYPT0231 |
547799 |
8478599 |
1148 |
11.0 |
KYPT0276 |
546196 |
8475402 |
1143 |
11.0 |
|
|
KYPT0232 |
547800 |
8479001 |
1149 |
12.9 |
KYPT0277 |
546196 |
8475403 |
1143 |
11.0 |
|
|
KYPT0233 |
548198 |
8478600 |
1144 |
11.0 |
KYPT0278 |
543803 |
8472997 |
1124 |
10.5 |
|
|
KYPT0234 |
548598 |
8478601 |
1140 |
9.0 |
KYPT0279 |
546201 |
8474634 |
1130 |
3.0 |
|
|
KYPT0235 |
548998 |
8478600 |
1134 |
7.0 |
KYPT0280 |
544200 |
8473002 |
1130 |
10.7 |
|
|
KYPT0236 |
549401 |
8478602 |
1125 |
8.0 |
KYPT0281 |
546594 |
8474612 |
1133 |
4.6 |
|
|
KYPT0237 |
549400 |
8478183 |
1123 |
3.0 |
KYPT0282 |
543400 |
8473001 |
1114 |
7.9 |
|
|
KYPT0238 |
549764 |
8479050 |
1121 |
3.0 |
KYPT0283 |
546598 |
8476548 |
1138 |
3.8 |
|
|
KYPT0239 |
549400 |
8478999 |
1126 |
5.0 |
KYPT0284 |
546201 |
8476465 |
1132 |
4.0 |
|
|
KYPT0240 |
550202 |
8479799 |
1118 |
4.0 |
KYPT0285 |
547799 |
8476129 |
1143 |
3.0 |
|
|
KYPT0241 |
550197 |
8479406 |
1117 |
7.0 |
KYPT0286 |
543051 |
8472996 |
1104 |
2.0 |
|
|
KYPT0242 |
548599 |
8479402 |
1138 |
10.0 |
KYPT0287 |
542998 |
8472623 |
1105 |
6.1 |
|
|
KYPT0243 |
548205 |
8479442 |
1139 |
6.6 |
KYPT0288 |
548202 |
8476199 |
1144 |
6.0 |
|
|
KYPT0244 |
547400 |
8478200 |
1144 |
3.6 |
KYPT0289 |
543347 |
8472600 |
1110 |
4.0 |
|
|
KYPT0245 |
548200 |
8478200 |
1139 |
4.0 |
KYPT0290 |
543000 |
8473400 |
1105 |
10.3 |
|
|
KYPT0246 |
548600 |
8478199 |
1136 |
7.0 |
KYPT0291 |
548598 |
8476199 |
1143 |
9.0 |
|
|
KYPT0247 |
549000 |
8478200 |
1131 |
7.0 |
KYPT0292 |
543000 |
8473800 |
1103 |
9.0 |
|
|
KYPT0248 |
547788 |
8478206 |
1139 |
2.0 |
KYPT0293 |
548201 |
8476599 |
1138 |
4.0 |
|
|
KYPT0249 |
546999 |
8477800 |
1150 |
9.0 |
KYPT0294 |
543407 |
8473756 |
1107 |
3.0 |
|
|
KYPT0250 |
547000 |
8477400 |
1150 |
9.0 |
KYPT0295 |
548600 |
8476600 |
1139 |
5.0 |
|
|
KYPT0251 |
547400 |
8477800 |
1145 |
8.0 |
KYPT0296 |
543800 |
8473800 |
1115 |
4.0 |
|
|
KYPT0252 |
547800 |
8477761 |
1143 |
7.0 |
KYPT0297 |
548202 |
8474999 |
1151 |
9.0 |
|
|
KYPT0253 |
548200 |
8477800 |
1135 |
3.0 |
KYPT0298 |
543799 |
8473402 |
1118 |
5.0 |
|
|
KYPT0254 |
548201 |
8477401 |
1141 |
8.0 |
KYPT0299 |
548485 |
8474600 |
1146 |
4.0 |
|
|
KYPT0300 |
543400 |
8473377 |
1113 |
4.5 |
KYPT0345 |
544200 |
8469800 |
1130 |
14.5 |
|
|
KYPT0301 |
548598 |
8475458 |
1144 |
4.0 |
KYPT0346 |
545111 |
8468600 |
1132 |
12.3 |
|
|
KYPT0302 |
548179 |
8474595 |
1154 |
8.9 |
KYPT0347 |
545400 |
8468600 |
1138 |
14.4 |
|
|
KYPT0303 |
547800 |
8473801 |
1158 |
8.9 |
KYPT0348 |
547004 |
8473401 |
1148 |
8.0 |
|
|
KYPT0304 |
547800 |
8473800 |
1158 |
9.0 |
KYPT0349 |
545802 |
8468598 |
1148 |
10.0 |
|
|
KYPT0305 |
542600 |
8471400 |
1107 |
5.9 |
KYPT0350 |
547796 |
8472997 |
1167 |
13.4 |
|
|
KYPT0306 |
548205 |
8473797 |
1151 |
3.0 |
KYPT0351 |
547714 |
8472654 |
1170 |
15.0 |
|
|
KYPT0307 |
547806 |
8474197 |
1157 |
11.0 |
KYPT0352 |
546200 |
8468601 |
1154 |
15.0 |
|
|
KYPT0308 |
542600 |
8471000 |
1110 |
5.9 |
KYPT0353 |
547401 |
8472600 |
1169 |
12.2 |
|
|
KYPT0309 |
548200 |
8474200 |
1152 |
9.0 |
KYPT0354 |
546600 |
8468600 |
1156 |
13.0 |
|
|
KYPT0310 |
542999 |
8471401 |
1110 |
8.3 |
KYPT0355 |
547400 |
8472202 |
1167 |
7.0 |
|
|
KYPT0311 |
547403 |
8473802 |
1152 |
5.0 |
KYPT0356 |
546600 |
8468200 |
1163 |
13.9 |
|
|
KYPT0312 |
542997 |
8471027 |
1104 |
5.0 |
KYPT0357 |
546602 |
8468200 |
1163 |
14.0 |
|
|
KYPT0313 |
547350 |
8473399 |
1158 |
11.0 |
KYPT0358 |
547774 |
8472220 |
1170 |
14.0 |
|
|
KYPT0314 |
543393 |
8471084 |
1105 |
3.8 |
KYPT0359 |
547800 |
8471801 |
1169 |
11.0 |
|
|
KYPT0315 |
543000 |
8470600 |
1111 |
6.3 |
KYPT0360 |
546999 |
8468601 |
1156 |
12.0 |
|
|
KYPT0316 |
543347 |
8470600 |
1106 |
5.0 |
KYPT0361 |
547401 |
8471803 |
1164 |
12.9 |
|
|
KYPT0317 |
548602 |
8475002 |
1142 |
6.3 |
KYPT0362 |
547000 |
8468200 |
1162 |
12.0 |
|
|
KYPT0318 |
543000 |
8470200 |
1122 |
11.0 |
KYPT0363 |
548210 |
8472992 |
1161 |
10.4 |
|
|
KYPT0319 |
547797 |
8473428 |
1162 |
12.0 |
KYPT0364 |
547403 |
8468612 |
1151 |
7.0 |
|
|
KYPT0320 |
542600 |
8470200 |
1122 |
8.0 |
KYPT0365 |
548199 |
8473400 |
1158 |
7.0 |
|
|
KYPT0321 |
547403 |
8474199 |
1154 |
11.0 |
KYPT0366 |
547400 |
8471399 |
1160 |
12.0 |
|
|
KYPT0322 |
542600 |
8470520 |
1110 |
2.3 |
KYPT0367 |
547400 |
8471002 |
1160 |
10.6 |
|
|
KYPT0323 |
547006 |
8474128 |
1141 |
4.4 |
KYPT0368 |
546200 |
8468200 |
1159 |
8.3 |
|
|
KYPT0324 |
543398 |
8470206 |
1114 |
3.5 |
KYPT0369 |
547400 |
8470601 |
1158 |
8.4 |
|
|
KYPT0325 |
543000 |
8469802 |
1128 |
9.1 |
KYPT0370 |
545800 |
8468200 |
1152 |
14.4 |
|
|
KYPT0326 |
543001 |
8469803 |
1128 |
9.2 |
KYPT0371 |
547801 |
8471000 |
1164 |
12.5 |
|
|
KYPT0327 |
547082 |
8473799 |
1142 |
3.0 |
KYPT0372 |
545400 |
8468200 |
1143 |
15.0 |
|
|
KYPT0328 |
543394 |
8469800 |
1120 |
8.0 |
KYPT0373 |
547804 |
8471403 |
1167 |
13.3 |
|
|
KYPT0329 |
548599 |
8479800 |
1131 |
6.6 |
KYPT0374 |
545400 |
8467800 |
1146 |
11.4 |
|
|
KYPT0330 |
549000 |
8479394 |
1135 |
8.0 |
KYPT0375 |
547800 |
8470599 |
1158 |
9.0 |
|
|
KYPT0331 |
543000 |
8469400 |
1130 |
11.1 |
KYPT0376 |
547798 |
8470200 |
1148 |
7.0 |
|
|
KYPT0332 |
549002 |
8480143 |
1127 |
5.3 |
KYPT0377 |
545799 |
8467800 |
1146 |
14.0 |
|
|
KYPT0333 |
543400 |
8469400 |
1122 |
8.6 |
KYPT0378 |
545799 |
8467801 |
1156 |
14.0 |
|
|
KYPT0334 |
549400 |
8480159 |
1123 |
5.0 |
KYPT0379 |
547414 |
8470212 |
1152 |
9.0 |
|
|
KYPT0335 |
549801 |
8480163 |
1120 |
4.7 |
KYPT0380 |
547396 |
8469807 |
1141 |
2.0 |
|
|
KYPT0336 |
543800 |
8469000 |
1123 |
2.0 |
KYPT0381 |
546980 |
8468992 |
1149 |
8.0 |
|
|
KYPT0337 |
547401 |
8472999 |
1167 |
14.2 |
KYPT0382 |
547360 |
8469019 |
1144 |
4.0 |
|
|
KYPT0338 |
543800 |
8469400 |
1119 |
14.5 |
KYPT0383 |
545800 |
8467400 |
1158 |
8.0 |
|
|
KYPT0339 |
543799 |
8469802 |
1118 |
14.5 |
KYPT0384 |
545410 |
8467400 |
1146 |
15.0 |
|
|
KYPT0340 |
543797 |
8470198 |
1118 |
20.4 |
KYPT0385 |
546599 |
8469002 |
1147 |
4.0 |
|
|
KYPT0341 |
543800 |
8470600 |
1119 |
14.6 |
KYPT0386 |
547799 |
8468999 |
1149 |
7.0 |
|
|
KYPT0342 |
544201 |
8471000 |
1121 |
17.5 |
KYPT0387 |
547794 |
8469400 |
1144 |
6.0 |
|
|
KYPT0343 |
543851 |
8471000 |
1116 |
20.5 |
KYPT0388 |
546999 |
8467401 |
1169 |
14.0 |
|
|
KYPT0344 |
544200 |
8470200 |
1128 |
14.5 |
KYPT0389 |
546197 |
8467796 |
1164 |
10.7 |
|
|
KYPT0390 |
547000 |
8467800 |
1167 |
11.5 |
KYPT0430 |
544999 |
8465800 |
1160 |
10.6 |
|
|
KYPT0391 |
546201 |
8467400 |
1165 |
15.0 |
KYPT0431 |
544999 |
8465799 |
1160 |
10.6 |
|
|
KYPT0392 |
546600 |
8467805 |
1169 |
8.0 |
KYPT0432 |
545000 |
8466200 |
1154 |
9.0 |
|
|
KYPT0393 |
546599 |
8467399 |
1171 |
12.8 |
KYPT0433 |
544998 |
8466601 |
1147 |
15.0 |
|
|
KYPT0394 |
547407 |
8467404 |
1169 |
9.6 |
KYPT0434 |
545400 |
8464200 |
1165 |
4.0 |
|
|
KYPT0395 |
546602 |
8467001 |
1165 |
12.0 |
KYPT0435 |
545800 |
8464199 |
1174 |
10.0 |
|
|
KYPT0396 |
546999 |
8466999 |
1167 |
6.5 |
KYPT0436 |
545403 |
8464598 |
1167 |
9.0 |
|
|
KYPT0397 |
546200 |
8467000 |
1159 |
15.0 |
KYPT0437 |
546199 |
8464601 |
1173 |
11.6 |
|
|
KYPT0398 |
544199 |
8484999 |
1112 |
6.0 |
KYPT0438 |
545801 |
8464599 |
1173 |
13.0 |
|
|
KYPT0399 |
544602 |
8484598 |
1119 |
6.0 |
KYPT0439 |
546199 |
8464201 |
1176 |
14.0 |
|
|
KYPT0400 |
544199 |
8484603 |
1119 |
10.0 |
KYPT0440 |
545000 |
8468200 |
1133 |
15.0 |
|
|
KYPT0401 |
543802 |
8484999 |
1112 |
9.0 |
KYPT0441 |
544199 |
8465800 |
1157 |
11.0 |
|
|
KYPT0402 |
546291 |
8466603 |
1151 |
11.6 |
KYPT0442 |
543800 |
8465799 |
1150 |
10.0 |
|
|
KYPT0403 |
543798 |
8484602 |
1117 |
10.0 |
KYPT0443 |
544552 |
8466601 |
1155 |
11.0 |
|
|
KYPT0404 |
543799 |
8484602 |
1117 |
10.0 |
KYPT0444 |
545001 |
8467800 |
1136 |
11.6 |
|
|
KYPT0405 |
545799 |
8466996 |
1150 |
15.0 |
KYPT0445 |
545000 |
8466991 |
1142 |
15.0 |
|
|
KYPT0406 |
543800 |
8484201 |
1122 |
10.9 |
KYPT0446 |
545400 |
8466600 |
1144 |
13.0 |
|
|
KYPT0407 |
544201 |
8484201 |
1125 |
11.7 |
KYPT0447 |
545800 |
8466600 |
1146 |
15.0 |
|
|
KYPT0408 |
543399 |
8484200 |
1119 |
12.0 |
KYPT0448 |
545401 |
8483801 |
1129 |
10.7 |
|
|
KYPT0409 |
545503 |
8467035 |
1145 |
15.0 |
KYPT0449 |
546202 |
8483795 |
1122 |
8.0 |
|
|
KYPT0410 |
543400 |
8484602 |
1114 |
6.0 |
KYPT0450 |
545805 |
8483799 |
1126 |
9.0 |
|
|
KYPT0411 |
543001 |
8484601 |
1114 |
10.0 |
KYPT0451 |
545805 |
8483800 |
1125 |
9.0 |
|
|
KYPT0412 |
544986 |
8467390 |
1139 |
13.7 |
KYPT0452 |
545401 |
8483400 |
1129 |
10.0 |
|
|
KYPT0413 |
542600 |
8484602 |
1112 |
10.0 |
KYPT0453 |
545801 |
8483400 |
1125 |
11.0 |
|
|
KYPT0414 |
542201 |
8484600 |
1107 |
10.0 |
KYPT0454 |
546199 |
8483399 |
1121 |
9.0 |
|
|
KYPT0415 |
544600 |
8467001 |
1150 |
11.0 |
KYPT0455 |
546600 |
8483400 |
1114 |
9.0 |
|
|
KYPT0416 |
542201 |
8484202 |
1110 |
9.5 |
KYPT0456 |
546601 |
8483792 |
1117 |
9.5 |
|
|
KYPT0417 |
542200 |
8483802 |
1106 |
8.3 |
KYPT0457 |
546601 |
8484201 |
1115 |
10.0 |
|
|
KYPT0418 |
544200 |
8467000 |
1151 |
13.6 |
KYPT0458 |
546207 |
8484200 |
1117 |
9.0 |
|
|
KYPT0419 |
542604 |
8483802 |
1110 |
8.0 |
KYPT0459 |
545800 |
8484200 |
1121 |
8.0 |
|
|
KYPT0420 |
543800 |
8467000 |
1146 |
11.0 |
KYPT0460 |
544953 |
8481801 |
1125 |
2.5 |
|
|
KYPT0421 |
542600 |
8484204 |
1114 |
11.0 |
KYPT0461 |
545400 |
8481800 |
1120 |
7.0 |
|
|
KYPT0422 |
543800 |
8466600 |
1149 |
12.0 |
KYPT0462 |
545401 |
8481400 |
1123 |
8.2 |
|
|
KYPT0423 |
543005 |
8484200 |
1117 |
11.0 |
KYPT0463 |
545400 |
8482201 |
1121 |
4.0 |
|
|
KYPT0424 |
544200 |
8466600 |
1155 |
10.8 |
KYPT0464 |
548961 |
8477740 |
1128 |
5.0 |
|
|
KYPT0425 |
544200 |
8466200 |
1156 |
14.0 |
KYPT0465 |
549307 |
8477767 |
1127 |
4.0 |
|
|
KYPT0426 |
544600 |
8466201 |
1158 |
9.0 |
KYPT0466 |
548450 |
8477772 |
1132 |
4.0 |
|
|
KYPT0427 |
543800 |
8466200 |
1150 |
5.5 |
KYPT0467 |
544650 |
8470996 |
1113 |
1.7 |
|
|
KYPT0428 |
544600 |
8465800 |
1161 |
8.7 |
KYPT0468 |
544913 |
8471407 |
1125 |
8.0 |
|
|
KYPT0429 |
544642 |
8484599 |
1119 |
1.7 |
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.
|
Air-Core 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 2m 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 bounded by weathering contacts 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 98 Air-Core holes for 2,548m are reported here from drilling at the Kasiya Rutile Deposit to obtain samples for quantitative determination of recoverable rutile and Total Graphitic Carbon (TGC).
A total of 247 push-tube core holes, for 2,205m, were drilled at the Kasiya Rutile Deposit to obtain samples for quantitative determination of recoverable rutile and Total Graphitic Carbon (TGC).
Placer has reviewed SOPs for Air-Core and Core drilling and found them to be fit for purpose and support the resource classifications as applied to the MRE.
|
|
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. Air-Core drilling recovery in the top few metres are moderate to good. Extra care is taken to ensure sample is recovered best as possible in these metres. Recoveries are recorded on the rig at the time of drilling by the geologist. Drilling is ceased when recoveries become poor once Sap rock has been encountered. 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.
Air-core drilling samples are recovered in large plastic bags. The bags are clearly labelled and delivered back to the laydown at the end of shift for processing.
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 intervals are geologically logged, recording relevant data to a set log-chief 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.
|
|
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 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.
|
N/A
|
|
If non-core, whether riffled, tube sampled, rotary split, etc. and whether sampled wet or dry. |
Air-Core 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.
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For all sample types, the nature, quality and appropriateness of the sample preparation technique.
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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.
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Quality control procedures adopted for all sub-sampling stages to maximise representivity of samples.
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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.
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Measures taken to ensure that the sampling is representative of the in situ material collected, including for instance results for field duplicate/second-half sampling.
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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.
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Whether sample sizes are appropriate to the grain size of the material being sampled.
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The sample size is considered appropriate for the material sampled. |
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Quality of assay data and laboratory tests |
The nature, quality and appropriateness of the assaying and laboratory procedures used and whether the technique is considered partial or total. |
Rutile The Malawi onsite laboratory sample preparation methods are considered quantitative to the point where a non-magnetic mineral concentrate (NM) 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) · Pan HMC to remove retained light minerals · Dry HMC in oven for 30 minutes at 105℃ · Magnetic separation of the HMC by Carpco magnet @ 16,800G (2.9Amps) into a magnetic (M) and non-magnetic (NM) fraction.
Bag NM fraction and send to Perth, Australia for quantitative chemical and mineralogical determination. · The NM fractions were sent to ALS Metallurgy Perth for quantitative XRF analysis. Samples received XRF_MS.
Graphite All samples are initially checked in and processed to pulp at Intertek-Genalysis Johannesburg. The pulp samples are then dispatched to Intertek-Genalysis Perth where they undergo TGC assay 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.
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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.
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Acceptable levels of accuracy and precision have been established. No handheld XRF methods are used for quantitative determination. |
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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.
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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.
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.
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.
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Verification of sampling & assaying |
The verification of significant intersections by either independent or alternative company personnel.
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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.
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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.
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Documentation of primary data, data entry procedures, data verification, data storage (physical and electronic) protocols. |
All geological logging data is collected in LogChief logging software. This data is then imported to Datashed5 and validated automatically and then manually.
Sovereigns’ laboratory data is captured onto paper templates or excel and transferred manually to the database. A transition to electronic laboratory data capture is under investigation.
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Discuss any adjustment to assay data.
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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.
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Location of data points |
Accuracy and quality of surveys used to locate drill holes (collar and down-hole surveys), trenches, mine workings and other locations used in Mineral Resource estimation.
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A Trimble R2 Differential GPS is used to pick up the collars. Daily capture at a registered reference marker ensures equipment remains in calibration. No downhole surveying is completed. Given the vertical nature and shallow depths of the holes, drill hole deviation is not considered to significantly affect the downhole location of samples.
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Specification of the grid system used. |
WGS84 UTM Zone 36 South.
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Quality and adequacy of topographic control. |
DGPS pickups are considered to be high quality topographic control measures.
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Data spacing & distribution |
Data spacing for reporting of Exploration Results. |
The Air-Core holes are spaced on a 200m x 200m grid which is deemed to adequately define the mineralisation.
The Core holes are spaced on a 400m x 400m grid which is deemed to adequately define the mineralisation.
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Whether the data spacing and distribution is sufficient to establish the degree of geological and grade continuity appropriate for the Mineral Resource and Ore Reserve estimation procedure(s) and classifications applied. |
The drill spacing and distribution is considered to be sufficient to establish a degree of geological and grade continuity appropriate for further future Mineral Resource estimation.
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Whether sample compositing has been applied. |
Individual 1m intervals have been composited, based on lithology, at a max 2m sample interval for the 98 Air-Core holes and 247 Core holes.
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Orientation of data in relation to geological structure |
Whether the orientation of sampling achieves unbiased sampling of possible structures and the extent to which this is known considering the deposit type
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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.
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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.
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There is no apparent bias arising from the orientation of the drill holes with respect to the orientation of the deposit. |
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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 or Malawi to Johannesburg. 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.
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Audits or reviews |
The results of any audits or reviews of sampling techniques and data
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Richard Stockwell (resource 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.
Malawi Field and Laboratory visits have been completed by Richard Stockwell in May 2022. A high standard of operation, procedure and personnel was observed and reported.
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SECTION 2 – REPORTING OF EXPLORATION RESULTS
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Criteria |
Explanation |
Commentary |
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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 (No 8. of 2019), held in the Company’s wholly-owned, Malawi-registered subsidiaries: EL0609, 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. |
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The security of the tenure held at the time of reporting along with any known impediments to obtaining a licence to operate in the area. |
The tenements are in good standing and no known impediments to exploration or mining exist. |
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Exploration done by other parties
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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. |
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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 eluvial 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 areas specifically, the preserved weathering profile hosts significant vertical thicknesses from near surface of graphite mineralisation. |
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Drill hole information |
A summary of all information material to the understanding of the exploration results including a tabulation of the following information for all Material drill holes: 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.
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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. |
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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 and exclude bottom of hole samples where saprock has been geologically logged.
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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. |
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The assumptions used for any reporting of metal equivalent values should be clearly stated. |
No metal equivalent values are used in this report. |
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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°. |
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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. |
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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. Graphite results are approximate true width as defined by the sample interval and typically increase with depth. |
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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 announcement at http://sovereignmetals.com.au/announcements/. |
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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. |
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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. |
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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). |
No further exploration is planned at this stage. |
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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. |
#POW Power Metal Resources PLC – Tati Project, Botswana – 2023 Exploration Underway
Power Metal Resources PLC (LON:POW) the London listed exploration company seeking large-scale metal discoveries across its global project portfolio announces next stage exploration on its 100% owned and operated Tati Gold Project (“Tati” or the “Project”) located within the Tati Greenstone Belt near Francistown, Botswana, is underway.
EXPLORATION PROGRAMME KEY OBJECTIVES
– To confirm the presence of a large gold-bearing system and delineate a deposit, through follow-on work over a larger portion of the approximately 8km long gold-in-soil anomaly.
– Through Power Metal’s largest and most comprehensive exploration campaign across the Tati Project, to date.
o Programme will include mechanised trenching, geophysics surveys, high-resolution geochemical surveys, reverse circulation (“RC”) drilling and diamond core drilling.
o Both geophysical survey work and mechanised trenching are currently underway, with further soil sampling scheduled and RC and diamond drilling to follow on in order to test the emerging high priority gold targets.
Paul Johnson, Chief Executive Officer of Power Metal Resources plc commented:
“The exploration campaign now underway is a key step forward for Power Metal with the various planned works tailored towards a single objective, namely the discovery of a large gold deposit.
Our exploration programmes in 2021 and 2022 have built a robust picture of the Project’s potential and we are particularly excited as we proceed with the next stage of exploration – the largest ever completed on the Project by Power Metal.
So far, we have confirmed near surface high-grade gold from reverse circulation drilling, conducted last year, which intersected the quartz reef structure near the Cherished Hope mine and delivered high-grade and bonanza-grade gold results. Figure 1 below provides an overview of those results.
Within the table immediately below is an overview of the work we are planning to undertake, with explanatory notes on the various steps to be implemented.”
EXPLORATION PROGRAMME OVERVIEW
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Exploration Work |
Rationale and Targeted Outcome |
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TRENCHING A circa 500 metre mechanised trenching programme (underway). Trenching will be focused along various strike-length extensions of the known outcropping gold mineralised quartz reef structure. Quartz reef as well as mineralised wall rock will be sampled when intersected within the exposed trenches.
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This work will look to extend the already known strike length extension of the main quartz reef structure at the Cherished Hope gold mine (the “Cherished Hope”) within the Project licence area. The quartz reef currently remains open towards the northwest and southeast as well as down dip. If the main quartz reef is successfully intercepted, the trenching would highlight quartz reef continuity between known historical workings at Cherished Hope, as well as to the northwest and southeast of current (~175m) strike length extents as defined by the recently completed RC drilling campaign. By extending the surficial expression of the mineralised quartz reef structure beyond the currently defined 175m strike length, Power Metal will be able to follow up drill test these areas to prove the downdip continuity, therefore increasing the size of the mineralised system in multiple dimensions. |
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SOIL GEOCHEMISTRY High-resolution soil geochemistry programme focussed on approximately 3km of strike-length (see red area highlighted on figure 1 below). Approximately 500-600 individual soil samples are planned with follow up assay testing of samples. Soil samples will be collected along a grid which will be focussed northwest of the 2022 RC drilling area. The goal is to improve the resolution and definition over several kilometres of the currently defined ~8km long gold-in-soil anomaly. |
Historical soil sampling completed over the majority of the Tati Project was undertaken by previous operators along 400m spaced lines at 40m sample spacing. This programme looks to infill the line spacing so that the definition and location of already proven Au-in-soil anomalies is vastly improved. This work will then allow Power Metal to follow up with more focussed next exploration steps which could include trenching and RC drilling of these new areas during subsequent work programmes. By completing this work, a much larger percentage of the 8km long Au-in-soil anomaly can move to next exploration steps therefore increasing the overall attractiveness of the Project as well as the size of the mineralised footprint. |
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GEOPHYSICS A ground magnetometer geophysics survey focussed on the northwestern strike length extension of the Cherished Hope Mine (underway).
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The goal of the magnetometer survey is to provide high-resolution imaging of any structures or geology which may have had an influence on the emplacement of mineralised quartz reef structures. Prospective structures and geology identified by the magnetometer survey can then be upgraded to further work streams which may include geochemical sampling, trenching and RC & diamond drilling. |
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REVERSE CIRCULATION (“RC”) DRILLING(1) ~15 RC drillholes are planned to an average planned depth of ~100m for ~1,500m in total.
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This RC programme is designed to test for the along strike and down dip extension of the main mineralised quartz reef structure. The mechanised trenching programme will be completed prior to the RC drilling and will look to extend the known surficial expression of the mineralised quartz reef structure. Once the surface expression is well defined by trenching, RC drilling will be employed in order to test for the down dip or depth extension of the quartz reefs within the subsurface. The goal is to prove continuity in the widths as well as grades of the quartz reef structure from surface down to depths targeted by the RC drilling. |
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DIAMOND CORE DRILLING(2)
~5 diamond drill holes are planned to an average expected depth of 100m for ~500m in total.
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The diamond drilling programme is designed to drill test select portions of the quartz reef structures which were previously successfully delineated by the RC drilling conducted during fall 2022. Diamond drilling provides full core rock samples, and therefore valuable information about structure, geology, and the nature of gold mineralisation. The information extracted from diamond drilling will allow the company to gain a better understanding of the mineralised quartz reefs and surrounding wall rocks. This data will be important as exploration continues to develop across the broader Tati Project. |
KEY:
(1) RC drilling involves a “hammer” piston which repeatedly strikes the target rock. Simultaneously, a powerful drill-bit at the end made of tungsten rotates at high speed. This creates small chips of rock known as drill cuttings that are sucked up with a vacuum and transported to a cyclone at the surface through dedicated tubes. The chips are then sorted into a variety of sampling bags, each of which represents a certain depth section of the drill hole. These bags are then sent off directly to the assay lab where their mineral content can be analysed. In turn, a picture of the rock types the hole encountered throughout its length can be established.
(2) Diamond core drilling involves rotating a hollow drill bit embedded with diamonds into the ground to a certain depth before extracting the solid, intact core recovered for analysis.
FURTHER INFORMATION
Figure 1 – Tati Project Overview Plan Map:
Figure 2 – Tati Project Q3 Drilling Area Zoomed Plan Map:
QUALIFIED PERSON STATEMENT
The technical information contained in this disclosure has been read and approved by Mr Nick O’Reilly (MSc, DIC, MIMMM, MAusIMM, FGS), who is a qualified geologist and acts as the Qualified Person under the AIM Rules – Note for Mining and Oil & Gas Companies. Mr O’Reilly is a Principal consultant working for Mining Analyst Consulting Ltd which has been retained by Power Metal Resources PLC to provide technical support.
This announcement contains inside information for the purposes of Article 7 of the Market Abuse Regulation (EU) 596/2014 as it forms part of UK domestic law by virtue of the European Union (Withdrawal) Act 2018 (“MAR”), and is disclosed in accordance with the Company’s obligations under Article 17 of MAR.
For further information please visit https://www.powermetalresources.com/ or contact:
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Power Metal Resources plc |
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Paul Johnson (Chief Executive Officer) |
+44 (0) 7766 465 617 |
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SP Angel Corporate Finance (Nomad and Joint Broker) |
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Ewan Leggat/Charlie Bouverat |
+44 (0) 20 3470 0470 |
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SI Capital Limited (Joint Broker) |
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Nick Emerson |
+44 (0) 1483 413 500 |
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First Equity Limited (Joint Broker) |
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David Cockbill/Jason Robertson |
+44 (0) 20 7330 1883 |
#FCM First Class Metals PLC – Gold & Molybdenum Trend Identified on North Hemlo
First Class Metals PLC (“First Class Metals” “FCM” or the “Company”) the UK metals exploration company seeking large scale metal discoveries across its extensive Canadian Schreiber-Hemlo & Sunbeam Project land holding is pleased to provide an update on activities in respect to the North Hemlo property.
Marc J Sale, Chief Executive Officer of First Class Metals commented:
“I am delighted to report on what has been a highly successful first field season for FCM across the North Hemlo property. The newly defined extension of the Dead Otter Lake occurrence into a trend of over 3km is a significant event. This trend with several gold assays over 1g/t and the incredible +19 g/t. Furthermore the associated molybdenum as a key pathfinder is very positive, given the Mo associated at Hemlo, only 20km to the south on a similar structural trend.
Alongside our own work on the property which has been majority focussed on the south, Palladium One have achieved some outstanding successes with high grade nickel sulphides from several drill intercepts on the West Pickle Lake JV. We are preparing for the 2023 season with the encouragement to develop an exploration programme to further this highly prospective project”.
HIGHLIGHTS:
Identification of the Dead Otter Lake gold & molybdenum trend
· Identification of a +3km long gold (Au) and molybdenum (Mo) anomalous trend to the southeast of the historic Dead Otter Lake occurrence. Grab samples recorded up to 19.6g/t Au along the trend.
Sampling of the Dead Otter Lake trend (“DOLT”) has extended anomalous Au/Mo mineralisation for +3km to the SE from the historic showing (3.7 g/t Au, 0.59% Mo). The mineralised structure closely mimics the granite contact. The 19.6 g/t Au sample, (see Photo 1), in the extreme SE of the trend could be where one of potentially two subparallel arcuate trends intersects the DOLT, see Figure 1
The Dead Otter Lake area is situated 20.5km North of the iconic Barrick Hemlo 23m Oz Au producing mine.
Photo 1 Sample from the DOLT trend which has reported a double-digit g/t gold assay.
Figure 1 the ‘DOLT’ with potential for subparallel / intersecting trends
Drilling at the West Pickle Lake JV
· Drilling at West Pickle Lake by Palladium One has demonstrated that the high-grade nickel-copper sulphide occurrence hold’s potential to be extended both east towards their RJ showing as well as west onto or close to the 100% owned FCM North Hemlo property. This area will also be a focus for reconnaissance in the upcoming field season and is currently being explored via collection of lake sediment samples and grab samples. See Table 1.
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Drill Hole ID |
Intersection (% Ni Eq.) |
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TK22-059 |
5.27% over 2.4m from 185.3m |
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TK22-060 |
3.94% over 2.4m from 186.6m |
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TK22-070 |
12.76% over 2.3m from 165.4m |
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TK22-073 |
7.2% Ni & 2.0% Cu over 2.6m of massive sulphides from 137.5m |
Table 1 Highlights of the to date significant drilling intercept results, from West Pickle Lake
Photo 2 Massive nickel-copper sulphides in drill core from West Pickle Lake, drill hole TK22-059
Figure 2 West Pickle Lake area showing the potential for extension to the east and west on to the FCM property.
High-Definition Magnetic Survey
· High-definition magnetic survey (HDMS) has shown that there are additional linear anomalies which require further exploration throughout the property, especially where intersected by north-south and north west structures. The survey highlighted the structure hosting the DOLT, as well as other potentially interesting features such as the extension of the Dotted Lake mineralised zone. The intersections of the N-S and NW-SE structures in the central north area are veritable exploration targets as are the structures paralleling the DOLT in the south.
Figure 3 hi resolution magnetic survey across the entire block, highlighting potential exploration targets.
Winter Exploration Activities
· In January 52 Lake sediment samples and 8 rock samples have been collected to date as part of the Winter exploration programme on North Hemlo currently focussed in the north central sector but which will continue to the south as well as on other properties thereafter. During the exploration season of 2022 there were significant anomalous samples reported from Olga Lake on the Dotted Lake / Fairservice trend, proving the viability of this exploration method in the Hemlo area.
First Class Metals is extremely excited about the DOLT ‘discovery’ an enthusiasm shared by Bruce MacLachlan, head of Emerald Geological Services1 (FCM geological lead) who commented that to the best of his understanding “this is one of the highest grab sample results ever recorded on the Hemlo north limb.”
Further work including reconnaissance and detailed sampling is required in order to define the trend as well as the potential and role that the ‘subparallel’ trends play in the mineralisation.
Exploration on the remainder of the claim area is ongoing and this field season will see a focus not only on the DOLT but also the area around the anomalous lake sediment samples reported and anticipated. This area is exciting as it is on strike from not only interesting magnetic features evidenced by the (HDMS) but also the interpreted extension of the Fairservice showing to the SW.
Future work in 2023 will focus on
• Dead Otter Lake trend and potential subparallel structures highlighted in soil samples.
• West Pickle Lake extension on to 100% owned FCM area of North Hemlo.
• Extension of the Dotted Lake / Fairservice structure.
• Other areas with potentially mineralised structures identified by the high-definition magnetic survey.
• Completion of the exploration Permit process
Background:
Historic exploration and to an extent contemporary data was limited and sporadic across the property, however, the pre field season deep review of the historic data did reveal that some encouraging ‘showings’, exist on the property or on structures interpreted to continue to the property, including Dotted Lake, Dead Otter Lake as well as the West Pickle Lake on Pezim II. The historic ‘showings’ identified on North Hemlo as well as the vectors from successful of exploration on neighbouring properties highlighted the potential for discovery of both gold and base metals and were what drove the exploration effort in the 2022 field season. The most important historical showing is the gold / molybdenum showing at Dead Otter Lake.
The Flagship North Hemlo property historically comprised of three claim areas:
Pezim I & II, and Wabikoba, which weren’t contiguous, but the additional of the Hemlo north block, acquired from Power Metals Plc. brought North Hemlo together as one cohesive block. The property now extends across 427 claims covering ~90km². The North Hemlo block is located in the north limb of the Hemlo greenstone belt, the comprising volcano-sedimentary rocks occur in an antiformal pattern, mimicking the ‘southern limb’ hosting the Barrick Hemlo gold mine.
Three parallel mineralised trends, potentially occupying shears, have been identified north of the Barrick Hemlo gold trend, interpreted as lying within proximity to magnetic anomalies. This is a similar signature to the Hemlo mine which is defined as ‘shear hosted’.
The North Hemlo (and Esa) properties are situated in an extremely prospective geological setting, as three of these inferred shears pass through the claim blocks, See figure 4.
Figure 4 the simplified regional structure of the Hemlo areas highlighting the subparallel trends in the north Hemlo Limb
For further information, please contact:
First Class Metals PLC
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James Knowles, Executive Chairman |
07488 362641 |
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Marc J Sale, CEO |
07711 093532 |
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Ayub Bodi, Executive Director |
07860 598086 |
First Equity Limited
(Financial Adviser & Broker)
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Jonathan Brown |
0207 3742212 |
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Jason Robertson |
0207 3742212 |
#TM1 Technology Minerals PLC – Exploration Update on the Leinster Project
Technology Minerals Plc (LSE: TM1), the first listed UK company focused on creating a sustainable circular economy for battery metals, is pleased to announce results from detailed lithogeochemical sampling has yielded high-grade spodumene pegmatite samples in float ranging up to 3.75% lithium oxide (“Li2O”) at Prospecting Licence Area (“PLA 1597”) in County Carlow, Republic of Ireland.
Highlights:
· Assay results are reported for the first stage of detailed lithogeochemical sampling at the Knockeen and Carriglead target areas on the Company’s Leinster Lithium Project.
· A total of 56 rock samples are reported, all of which were analysed at ALS Laboratories in Ireland.
· Two prospects are reported at:
o Knockeen: Out of a total of 56 samples, 41 samples graded above 1% Li2O, of which 20 graded above 2% Li2O and of which two graded above 3% Li2O (Sample AES 63003 – 3.63% Li2O and Sample AES 63033 – 3.75% Li2O)
o Carriglead: Out of a total of 10 samples, six samples graded above 1% Li2O of which one sample analysed above 2% Li2O (sample AES63504 – 2.09% Li2O).
· The programme of intensive prospecting has consolidated the extent of the spodumene pegmatite boulder train at surface as well as significantly enhancing the resolution of the dispersion zone
· The known extent of the boulder train is now over 1km in length from NE to SW and 0.5km from NW to SE and is still open in all directions at Knockeen and Carriglead
· The ongoing work is helping to refine specific areas for targeted drilling.
The licence, which was awarded to Technology Minerals’ wholly owned subsidiary LRH Resources Limited (“LRH”) on 22 March 2022, forms part of the Company’s Leinster Property exploration block, which is operated under an exclusive Option and Earn-in agreement with Global Battery Metals Ltd (“GBML”), (TSXV: GBML; OTCQB: REZZF; Frankfurt: REZ) with no project expenditure required by the Company.
Field Exploration Programme Update
The current phase of detailed exploration work is centred on an area where a forty-year-old historical company report described a trench excavated at Knockeen Townlands on PLA 1597 (Figure 1) which uncovered in bedrock, a 1.8m wide spodumene-bearing pegmatite vein. However no detailed laboratory assays or geological maps of the trench were reported at that time. Historical prospecting around the trench also reported the occurrence of up to 10 large boulders of spodumene-bearing pegmatite at surface.
The current exploration programme carried out under LRH Resources management by Aurum Exploration Services Limited included an initial reconnaissance in July 2022 totalling six samples followed by a more detailed prospecting and lithogeochemical survey on two areas at Knockeen and Carriglead Townlands in December 2022 and totalling 56 samples (Figure 1 & Table 1).
|
Prospect |
Programme |
No |
|
Carriglead |
Recon Sampling July 2022 |
2 |
|
Knockeen |
Recon Sampling July 2022 |
4 |
|
Prospect |
Programme |
No |
|
Carriglead |
Follow Up Sampling Dec 2022 |
10 |
|
Knockeen |
Follow Up Sampling Dec 2022 |
56 |
|
Prospect |
Programme |
No |
|
Carriglead |
Total |
12 |
|
Knockeen |
Total |
60 |
Table 1: Showing number of samples collected (July 2022 & December 2022)
Preliminary Reconnaissance July 2022
Two areas at Knockeen and Carriglead Townlands were targeted with an initial reconnaissance visit in July 2022. Six samples were collected during a site visit and included four at Knockeen and two at Carriglead. Analytical results confirmed the presence of the historically reported spodumene pegmatite boulder train and returned very significant grades of Li2O in all samples. These results have been reported previously but are reproduced here for continuity (Table 2).
|
Sample_ID |
Programme |
Li_ppm |
Li2O_% |
Prospect |
|
210724CL05 |
Recon Sampling July 2022 |
13,700 |
2.95 |
Knockeen |
|
210724CL03 |
Recon Sampling July 2022 |
11,200 |
2.41 |
Knockeen |
|
210724CL04 |
Recon Sampling July 2022 |
11,000 |
2.37 |
Knockeen |
|
210724CL02 |
Recon Sampling July 2022 |
3,240 |
0.70 |
Knockeen |
|
AES61138 |
Recon Sampling July 2022 |
7,470 |
1.61 |
Carriglead |
|
AES61137 |
Recon Sampling July 2022 |
3,550 |
0.76 |
Carriglead |
Table 2: Results from reconnaissance prospecting (July 2022)
* Li2O % = Li ppm % (x 2.153)
Follow Up Detailed Prospecting and Lithogeochemistry
In December 2022, an extensive prospecting and lithogeochemistry survey was completed covering the two areas identified during the reconnaissance programme. A total of 56 samples were collected at Knockeen and 10 at Carriglead. The results were highly encouraging with coherent boulder trains of spodumene-bearing lithium pegmatites mapped out across the prospects. The highlight sample results are shown in Table 3 and the full results are appended in Appendix 1 to this release in Tables 4 and 5 with associated maps showing the locations in Figure 2 (Knockeen) and Figure 3 (Carriglead) below.
Figure 1: Location of the Knockeen and Carriglead target areas PL 1597 showing sample locations
|
Sample_ID |
Programme |
Li_ppm |
Li2O% |
|
AES63003 |
Follow Up Sampling Dec 2022 |
17,410 |
3.75 |
|
AES63033 |
Follow Up Sampling Dec 2022 |
16,860 |
3.63 |
|
AES63519 |
Follow Up Sampling Dec 2022 |
13,160 |
2.83 |
|
AES63015 |
Follow Up Sampling Dec 2022 |
13,050 |
2.81 |
|
AES63029 |
Follow Up Sampling Dec 2022 |
12,920 |
2.78 |
|
AES63042 |
Follow Up Sampling Dec 2022 |
12,580 |
2.71 |
|
AES63014 |
Follow Up Sampling Dec 2022 |
12,200 |
2.63 |
|
AES63021 |
Follow Up Sampling Dec 2022 |
12,040 |
2.59 |
|
AES63018 |
Follow Up Sampling Dec 2022 |
11,980 |
2.58 |
|
AES63011 |
Follow Up Sampling Dec 2022 |
11,820 |
2.54 |
Table 3: Highlight results from the prospecting programme (December 2022)
* Li2O % = Li ppm % (x 2.153)
The current results focussed on the two areas and considerably enhanced the area of boulder trains and significantly shows the high-grade nature and size of the boulders in the material being sampled.
Figure 2: Location of samples and assay results from the Knockeen target area
Figure 3: Location of samples and assay results from the Carriglead target area
Photo 1: Spodumene pegmatite samples from Knockeen and Carriglead
Alex Stanbury, CEO of Technology Minerals, said: “These latest assay results from the Leinster Project in Ireland are highly encouraging and build on previous reconnaissance work which displayed significant grades of Li2O in all samples. The results announced today continue to demonstrate the high-grade nature and size of the boulders in the material being sampled as well as expanding the known extent of the spodumene pegmatite boulder train at Knockeen and Carriglead. Today’s results and ongoing work will help us to determine specific areas for targeted drilling as we progress with the exploration campaign.”
Competent Person
All scientific and technical information in this announcement has been prepared under the supervision of EuroGeol Vaughan Williams M.Sc. P.Geo (a Principal of Aurum Exploration Services who currently provides exploration services to TM and to LRH), and a “qualified person” within the meaning of National Instrument 43-101. Vaughan Williams is also company secretary of LRH and a Director of the LRH Spanish subsidiary Asturmet Recursos S.L.
Enquiries
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Technology Minerals Plc |
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Robin Brundle, Executive Chairman Alexander Stanbury, Chief Executive Officer |
+44 20 4582 3500 |
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Global Battery Metals Ltd. |
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Michael Murphy BA, MBA, MSc., ICD, President & CEO |
+1 604-649-2350 |
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Oberon Investments Limited |
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Nick Lovering, Adam Pollock |
+44 (0)20 3179 0535 |
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Arden Partners Plc |
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Louisa Waddell, Tim Dainton |
+44 207 614 5900 |
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Gracechurch Group |
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Harry Chathli, Alexis Gore, William Dobinson |
+44 20 4582 3500 |
Technology Minerals Plc
Technology Minerals is developing the UK’s first listed, sustainable circular economy for battery metals, using cutting-edge technology to recycle, recover, and re-use battery technologies for a renewable energy future. Technology Minerals is focused on extracting raw materials required for Li-ion batteries, whilst solving the ecological issue of spent Li-ion batteries, by recycling them for re-use by battery manufacturers. With the increasing global demand for battery metals to supply electrification, the group will explore, mine, and recycle metals from spent batteries. Further information on Technology Minerals is available at www.technologyminerals.co.uk
Appendix 1: Analytical Results
|
Sample_ID |
Programme |
Li _ppm |
Li2O% |
Prospect |
|
AES63003 |
Follow Up Sampling Dec 2022 |
17,410 |
3.75 |
Knockeen |
|
AES63033 |
Follow Up Sampling Dec 2022 |
16,860 |
3.63 |
Knockeen |
|
AES63519 |
Follow Up Sampling Dec 2022 |
13,160 |
2.83 |
Knockeen |
|
AES63015 |
Follow Up Sampling Dec 2022 |
13,050 |
2.81 |
Knockeen |
|
AES63029 |
Follow Up Sampling Dec 2022 |
12,920 |
2.78 |
Knockeen |
|
AES63042 |
Follow Up Sampling Dec 2022 |
12,580 |
2.71 |
Knockeen |
|
AES63014 |
Follow Up Sampling Dec 2022 |
12,200 |
2.63 |
Knockeen |
|
AES63021 |
Follow Up Sampling Dec 2022 |
12,040 |
2.59 |
Knockeen |
|
AES63018 |
Follow Up Sampling Dec 2022 |
11,980 |
2.58 |
Knockeen |
|
AES63011 |
Follow Up Sampling Dec 2022 |
11,820 |
2.54 |
Knockeen |
|
AES63023 |
Follow Up Sampling Dec 2022 |
11,620 |
2.50 |
Knockeen |
|
AES63028 |
Follow Up Sampling Dec 2022 |
11,580 |
2.49 |
Knockeen |
|
AES63041 |
Follow Up Sampling Dec 2022 |
11,570 |
2.49 |
Knockeen |
|
AES63037 |
Follow Up Sampling Dec 2022 |
11,510 |
2.48 |
Knockeen |
|
AES63016 |
Follow Up Sampling Dec 2022 |
11,460 |
2.47 |
Knockeen |
|
AES63044 |
Follow Up Sampling Dec 2022 |
11,340 |
2.44 |
Knockeen |
|
AES63012 |
Follow Up Sampling Dec 2022 |
11,180 |
2.41 |
Knockeen |
|
AES63008 |
Follow Up Sampling Dec 2022 |
9,920 |
2.14 |
Knockeen |
|
AES63048 |
Follow Up Sampling Dec 2022 |
9,520 |
2.05 |
Knockeen |
|
AES63043 |
Follow Up Sampling Dec 2022 |
9,360 |
2.02 |
Knockeen |
|
AES63027 |
Follow Up Sampling Dec 2022 |
8,820 |
1.90 |
Knockeen |
|
AES63046 |
Follow Up Sampling Dec 2022 |
8,790 |
1.89 |
Knockeen |
|
AES63516 |
Follow Up Sampling Dec 2022 |
8,370 |
1.80 |
Knockeen |
|
AES63036 |
Follow Up Sampling Dec 2022 |
8,300 |
1.79 |
Knockeen |
|
AES63007 |
Follow Up Sampling Dec 2022 |
8,090 |
1.74 |
Knockeen |
|
AES63026 |
Follow Up Sampling Dec 2022 |
8,030 |
1.73 |
Knockeen |
|
AES63010 |
Follow Up Sampling Dec 2022 |
7,890 |
1.70 |
Knockeen |
|
AES63517 |
Follow Up Sampling Dec 2022 |
7,910 |
1.70 |
Knockeen |
|
AES63512 |
Follow Up Sampling Dec 2022 |
7,840 |
1.69 |
Knockeen |
|
AES63017 |
Follow Up Sampling Dec 2022 |
7,550 |
1.63 |
Knockeen |
|
AES63520 |
Follow Up Sampling Dec 2022 |
7,370 |
1.59 |
Knockeen |
|
AES63049 |
Follow Up Sampling Dec 2022 |
7,100 |
1.53 |
Knockeen |
|
AES63515 |
Follow Up Sampling Dec 2022 |
7,040 |
1.52 |
Knockeen |
|
AES63024 |
Follow Up Sampling Dec 2022 |
6,190 |
1.33 |
Knockeen |
|
AES63031 |
Follow Up Sampling Dec 2022 |
6,140 |
1.32 |
Knockeen |
|
AES63013 |
Follow Up Sampling Dec 2022 |
5,720 |
1.23 |
Knockeen |
|
AES63019 |
Follow Up Sampling Dec 2022 |
5,420 |
1.17 |
Knockeen |
|
AES63030 |
Follow Up Sampling Dec 2022 |
5,300 |
1.14 |
Knockeen |
|
AES63034 |
Follow Up Sampling Dec 2022 |
4,960 |
1.07 |
Knockeen |
|
AES63039 |
Follow Up Sampling Dec 2022 |
4,790 |
1.03 |
Knockeen |
|
AES63022 |
Follow Up Sampling Dec 2022 |
4,710 |
1.01 |
Knockeen |
|
AES63514 |
Follow Up Sampling Dec 2022 |
4,300 |
0.93 |
Knockeen |
|
AES63045 |
Follow Up Sampling Dec 2022 |
4,290 |
0.92 |
Knockeen |
|
AES63025 |
Follow Up Sampling Dec 2022 |
3,940 |
0.85 |
Knockeen |
|
AES63032 |
Follow Up Sampling Dec 2022 |
3,550 |
0.76 |
Knockeen |
|
AES63035 |
Follow Up Sampling Dec 2022 |
2,680 |
0.58 |
Knockeen |
|
AES63009 |
Follow Up Sampling Dec 2022 |
1,920 |
0.41 |
Knockeen |
|
AES63047 |
Follow Up Sampling Dec 2022 |
1,480 |
0.32 |
Knockeen |
|
AES63038 |
Follow Up Sampling Dec 2022 |
450 |
0.10 |
Knockeen |
|
AES63001 |
Follow Up Sampling Dec 2022 |
120 |
0.03 |
Knockeen |
|
AES63002 |
Follow Up Sampling Dec 2022 |
120 |
0.03 |
Knockeen |
|
AES63004 |
Follow Up Sampling Dec 2022 |
120 |
0.03 |
Knockeen |
|
AES63005 |
Follow Up Sampling Dec 2022 |
130 |
0.03 |
Knockeen |
|
AES63513 |
Follow Up Sampling Dec 2022 |
100 |
0.02 |
Knockeen |
|
AES63518 |
Follow Up Sampling Dec 2022 |
80 |
0.02 |
Knockeen |
|
AES63006 |
Follow Up Sampling Dec 2022 |
60 |
0.01 |
Knockeen |
Table 4: Results from follow up prospecting at Knockeen (December 2022)
* Li2O % = Li ppm % (x 2.153)
|
Sample_ID |
Programme |
Li_ppm |
Li2O% |
Prospect |
|
AES63504 |
Follow Up Sampling Dec 2022 |
9,720 |
2.09 |
Carriglead |
|
AES63503 |
Follow Up Sampling Dec 2022 |
8,890 |
1.91 |
Carriglead |
|
AES63509 |
Follow Up Sampling Dec 2022 |
7,870 |
1.69 |
Carriglead |
|
AES63501 |
Follow Up Sampling Dec 2022 |
7,460 |
1.61 |
Carriglead |
|
AES63507 |
Follow Up Sampling Dec 2022 |
5,620 |
1.21 |
Carriglead |
|
AES63505 |
Follow Up Sampling Dec 2022 |
5,120 |
1.10 |
Carriglead |
|
AES63508 |
Follow Up Sampling Dec 2022 |
3,280 |
0.71 |
Carriglead |
|
AES63511 |
Follow Up Sampling Dec 2022 |
500 |
0.11 |
Carriglead |
|
AES63506 |
Follow Up Sampling Dec 2022 |
330 |
0.07 |
Carriglead |
|
AES63502 |
Follow Up Sampling Dec 2022 |
290 |
0.06 |
Carriglead |
Table 5: Results from follow up prospecting at Carriglead (December 2022)
* Li2O % = Li ppm % (x 2.153)
#BRES Blencowe Resources Plc – Export Approval for Bulk Samples
Highlights
· Ugandan Government approves landmark one-off permit for Blencowe to export bulk sample graphite from Orom-Cross for key final testing
· Underlines huge support for Orom-Cross advancement to production at all levels within the country
· Blencowe has successfully completed two rounds of smaller sample metallurgical testing on Orom-Cross graphite during 2022, using technical firms in Canada and Australia.
· Mandate signed with experienced Chinese graphite processing specialist Jilin Huiyang New Material Technology Company Ltd to use its existing bulk pilot facility for final metallurgical testing.
· 100 tonnes of bulk sample to be mined immediately and sea-freighted to China.
· Additional 150kgs sample to be mined and fast-track delivered to China by air freight for initial off-site testing in same facility.
Blencowe Resources Plc (“Blencowe Resources” or the “Company”) (LSE: BRES) is pleased to announce it has received an approval from the Ugandan Ministry of Energy and Mineral Development to export materials from its Orom-Cross Graphite Project to Chinese testing facilities to enable final bulk metallurgical test work to be undertaken in 2023. Blencowe has mandated Jilin Huiyang New Material Technology Company Ltd (“Jilin”) to complete this test work in their existing pilot plant facility, which negates the requirement for the Company to build its own bulk testing facility on-site in the near term.
Jilin has over 30 years direct experience in graphite processing and has completed similar bulk sample testing for other leading international graphite companies in the past. This is a key step in the process to pre-qualify Orom-Cross end-products as concentrates through to OEMs in order to ultimately achieve binding offtake contracts for production from the Project.
As Ugandan Mining Law does not allow for the export of unprocessed raw materials this approval is a landmark decision by the Government, who fully understand the need and requirement for this testing to occur as a key action for the advancement of Orom-Cross towards first production. Blencowe acknowledges and appreciates the support of the Government of Uganda and the Ministry of Energy and Mineral Development in this matter.
The export permits for 100t of bulk raw ore materials and 400 litres of local groundwater will enable the Company to export a representative bulk sample from the initial 5 years of production, which will be used to assess the metallurgical processes on a commercial scale including differing plant components to maximise the grade, recovery and flake sizing from the Project. The addition of the groundwater sample will enable the test facilities to assess the water characteristics in terms of the reagents required under proposed site operating conditions.
Works to excavate and transport the bulk samples will begin immediately and will be freighted by sea to China to have the testing completed as quickly as practically possible. In addition, 150kgs of the same samples will be air-freighted to same Jilin facility more quickly to undergo metallurgical testing and build knowledge before the larger samples arrive.
Blencowe has already been able to share significant data with Jilin having previously completed two stages of bench scale metallurgical testing with SGS in Canada (30kgs) and more recently a further round of testing via a small pilot plant (130kgs) in Perth, Australia. This next-level proposed test in China, using their existing infrastructure and experience, will be done on a considerably larger scale, which will give all parties more knowledge of the end concentrates that can be produced on a production scale from Orom-Cross. It is hoped that this program will initially lead to non-binding MOUs for offtake, and ultimately to binding sale agreements for a substantial portion of the initial 50,000tpa product to be produced from stage one within Orom-Cross. There may also be potential for EPC and funding contracts emanating from this relationship, potentially providing one solution to the CAPEX requirement for initial stage production.
Cameron Pearce, Executive Chairman commented;
“China is currently the most mature graphite market worldwide and entering into an offtake relationship there would be very valuable to us given the highly attractive economics at Orom-Cross, which already has an NPV8 of US$482M based on an initial 14-year mine life, from just ~2% drilled from our broader graphite resource.
This bulk sample trial is significant as a precursor that ultimately leads us to a full offtake agreement, which in turn would enable us to kick start production with a critical mass of product sold to drive profitability and cash flow. If successful it can also lead to building an EPC relationship and potential funding solutions.
The graphite market is evolving very quickly and we will see a lot of change ahead as the world expands from current 15-20 million electric vehicles (EVs) towards the targeted 100 million by 2030. This in turn will drive up the demand for flake graphite as a non-replaceable input required to produce lithium-ion batteries to power these EVs and leading analysts forecast a 300% rise in world demand for graphite by 2030. We are already seeing prices rise in anticipation of this looming shortage. The Chinese graphite market remains the largest and will likely remain so for some time ahead, thus establishing a strong and commercial relationship with both Chinese and other Asian partners is decisive for Orom-Cross and a natural progression for the Company.“
For further information please contact:
|
Blencowe Resources Plc Sam Quinn |
www.blencoweresourcesplc.com Tel: +44 (0)1624 681 250
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Investor Relations Sasha Sethi |
Tel: +44 (0) 7891 677 441
|
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Tavira Securities Jonathan Evans |
Tel: +44 (0)20 3192 1733 jonathan.evans@tavirasecurities.com
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First Equity Limited Jason Robertson |
Tel: +44(0)20 7330 1833 jasonrobertson@firstequitylimited.com
|
Twitter https://twitter.com/BlencoweRes
LinkedIn https://www.linkedin.com/company/72382491/admin/
Background
Orom-Cross Graphite Project
Orom-Cross is a potential world class graphite project both by size and end-product quality, with a high component of more valuable larger coarse flakes within the deposit.
A 21-year Mining Licence for the Project was issued by the Ugandan Government in 2019 following extensive historical work on the deposit and Blencowe completed a successful Pre-Feasibility Study in 2022. The Company has now moved into the Definitive Feasibility Study phase as it drives towards first production.
Orom-Cross presents as a large, shallow open-pitable deposit, with a maiden JORC Indicated & Inferred Mineral Resource deposit of 24.5Mt @ 6.0% Total Graphite Content, with only a small percentage of the overall deposit drilled to date. Development of the resource is expected to benefit from a low strip ratio and free dig operations, thereby ensuring lower operating and capital costs.
#FCM First Class Metals PLC – Exercise of Warrants and Issue of Equity
First Class Metals PLC (LSE:FCM) announces that it has received several notices to exercise warrants over a total of 450,582 Ordinary Shares (the “Warrant Shares“), for which funds of GBP 46,683.20 have been received by the Company.
Application will be made to the Financial Conduct Authority (“FCA”) for admission of the above Ordinary Shares to the standard listing segment of the Official List and to trading on the London Stock Exchange’s Main Market for listed securities, with admission and dealings in the new shares expected to take place from 8.00am on 16th January 2023.
Following Admission, the Company’s issued share capital will consist of 69,969,289 Ordinary Shares with voting rights. This figure of 69,969,289 may be used by shareholders in the Company as the denominator for the calculations by which they will determine if they require to notify their interest in, or a change to their interest in, the share capital of the Company under the UK Financial Conduct Authority’s Disclosure Guidance and Transparency Rules.
For further information, please contact:
First Class Metals PLC
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James Knowles, Executive Chairman |
07488 362641 |
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Marc J Sale, CEO |
07711 093532 |
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Ayub Bodi, Executive Director |
07860 598086 |
First Equity Limited
(Financial Adviser & Broker)
|
Jonathan Brown |
|
0207 3742212 |
|
Jason Robertson |
|
0207 3742212 |
#GRX GreenX Metals Limited- Result of AGM
GreenX Metals Limited (GreenX or the Company) advises, that the 2022 Annual General Meeting (AGM) of the Company was held today, 16 November 2022, at 10.00am (AWST).
The resolutions voted on were in accordance with the Notice of AGM previously advised to shareholders.
All resolutions were decided on and carried by way of a poll.
In accordance with Section 251AA of the Corporations Act 2001 and ASX Listing Rule 3.13.2, the details of the poll and the proxies received in respect of each resolution are set out over page.
The Company has also released a new Constitution which will be available to view at www.greenxmetals.com.
For further information please contact:
Dylan Browne
Company Secretary
+61 8 9322 6322
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Resolution |
Number of Proxy Votes |
Number of Votes cast on the Poll |
Result |
|||||
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For |
Against |
Abstain |
Proxy’s Discretion |
For |
Against |
Abstain |
||
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1. Remuneration Report |
3,645,078 |
6,500 |
15,062,316 |
25,000 |
3,670,078 |
6,500 |
15,062,316 |
Carried on vote by poll |
|
2. Re-election of Mr Mark Pearce as a Director |
18,711,578 |
– |
2,316 |
25,000 |
18,736,578 |
– |
2,316 |
Carried on vote by poll |
|
3. Adoption of New Constitution |
18,711,578 |
– |
2,316 |
25,000 |
18,736,578 |
– |
2,316 |
Carried on vote by poll |
|
4. Approval of Additional 10% Placement Capacity |
18,511,578 |
200,000 |
2,316 |
25,000 |
18,536,578 |
200,000 |
2,316 |
Carried on vote by poll |