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GOLDEN DEEPS LIMITED. — Capital/Financing Update 2012
Dec 18, 2012
64977_rns_2012-12-18_f5322c1c-2f68-43c5-b2a0-3bcee1d6e937.pdf
Capital/Financing Update
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ASX ANNOUNCEMENT & MEDIA RELEASE
19 December 2012
HIGH- G RADE R ESUL T S CONTINUE AT CH R ISTIA N A
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S u rface channel s ampling team i n action at Christiana
HI G HLIGH T S
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Highly successful surface and underground sampling and mapping programmes completed at Christiana historical mine site
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Sampling has defined unexploited high grade zinc-lead-vanadium mineralisation extending over 500m of strike, up to 70m in apparent thickness and over 30m in vertical extent. Mineralisation appears to be open at depth and along strike in both directions.
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Best surface channel sampling results include: ABCS 0 008 11 m e tres @ 1 5 .30% Pb+Zn and 0.02% V 2 O5 ABCS 0 023 16 m e tres @ 9 . 84% Pb+Zn and 0 .02% V2 O 5 ABCS 0 024 10 m e tres @ 1 4 .34% Pb+Zn and 0.01% V 2 O5
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Best underground channel sampling results include: ABUG0027 3 m etres @ 15.93% P b+Zn a n d 0.04% V2O5 ABUG0019 6 m etres @ 1 4.01% P b+Zn an d 0.28% V 2O5
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RC drilling is planned to delineate a maiden JORC resource and to initiate a scoping study into re-opening a mining operation
Golden Deeps Ltd (ABN 12 054 5 7 0 777) www.golde n 1[st] Flo o r, 8 Parliament Pl a ce, West Perth, W A 6005 PO Box 1618, West Pe r th, WA 6872 t : +61 8 9481 7833 f: +61 8 9481 77835 e: [email protected] m
www.golde n deeps.com
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CHANNEL S AMPLIN G
Gol d en Deeps is pleased t o announc e the compl e tion of a key phase i n the explor a tion of the Christiana P rospect at its Grootfo n tein Base M etals Project in Namib i a. The Co m pany’s exp l oration te a m has n o w receive d the maj o rity of th e results f r om an e x tensive underground a n d surface channel sa m pling pro g ramme at t he historic a l Christiana ZincLead-Vanadiu m Mine. Sa m pling inclu d ed all acc e ssible underground de v elopment o n three min e levels do w n to the 2 0 0ft level a s well as op e n pits and surface ex p osures, identifying wid e zones of h igh grade m ineralisati o n (See Ap p endix 1). T he channel sampling s pacing of 2 0m roughl y matches t h e undergr o und cross-cut spacing and provi d es a high l evel of sa m pling detail for the planning of futu r e explorati o n program m es.
Ap p roximately 5 00 metres of strike ha s now been effectively s ampled at s urface and on the 50ft, 100ft and 200ft level s . Almost e v ery chann e l sample has returned highly anomalous zin c , lead and v anadium m i neralisatio n .
The results are extremely e ncouraging as they ind i cate the fol l owing;
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The willemite (Zn 2 SiO4) and descloizite ((Pb,Zn)2( O H)VO4) ric h mineralis a tion is extrem e ly high gr a de in plac e s (up to 5 0 .4% Zn ov e r 1m in t h e channel sample ABUG 0 019 on the 50ft level, a nd 38.28% Z n over 3m in ABCS00 2 4 on surfa c e).
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Minera l isation is predominantly silicate-oxide with lesser sul p hides (sp h alerite, galena ) and carbo n ates (cerru s ite and sm i thsonite).
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Exclud i ng the shallow open pits, which e xtend in some places t o the 50ft l evel, a large a m ount of th e Christiana zinc miner a lisation re m ains intact a nd unmine d .
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Signifi c ant zones o f higher gr a de minera l isation occ u r within m u ch wider z o nes of lower grade Zn-Pb - V minerali s ation.
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Many o f the und e rground cr o ss-cuts d o not reach the interp r eted ore position, indicating mineralisation is m ore perva s ive than s hown only by the ol d mine workin g s (this relates to high grade mini n g practice s when the mine was o pen in 1947-1958).
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The underground w orkings ar e in good c o ndition, indicating a ve r y deep wat e r table and go o d geotech n ical ground conditions
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The mineralised z o ne remain s open alo n g strike in both directi o ns and below the old wo r kings and developmen t .
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The new resul t s demonst r ate the en o rmous pot e ntial of th e Christian a Prospect. A full listi n g of the si g nificant intercepts and c hannel sa m ple details are found i n Appendix 1 .
So m e detail of t he better r e sults of the channel sa m pling is as follows:
Su r face
ABCS0008 47m @ 4.52% Pb+Zn (4.37% Zn and 0.15% Pb) and 0.02% V2[O] 5 including 11m @ 15.30% Pb+Zn (14.94% Zn and 0.36% Pb) and 0.02% V2O ABCS0010 20m @ 3.84% Pb+Zn (3.03% Zn and 0.81% Pb) and 0.26% V2[O] 5 including 5m @ 12.02% Pb+Zn (9.49% Zn and 2.54% Pb) and 0.88% V2O5 ABCS0023 16m @ 10.03% Pb+Zn (9.84% Zn and 0.19% Pb) and 0.02% V2O5
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ABCS0024 10m @ 14.34% Pb+Zn (14.15% Zn and 0.20% Pb) and 0.01% V2O5 including 3m @ 33.58% Pb+Zn (33.28% Zn and 0.3% Pb) and 0.01% V2[O] 5
Un d ergroun d
- ABUG0019 6m @ 14.01% Pb+Zn (13.08% Zn and 0.93%Zn) and 0.28% V2[O] 5 including 2m @ 33.71% Pb+Zn (33.15% Zn and 0.56% Pb) and 0.01% V2O5 ABUG0027 3m @ 15.93% Pb+Zn (15.79% Zn and 0.14% Pb) and 0.04% V2O5 ABUG0034 10m @ 10.39% Pb+Zn (9.51% Zn and 0.88% Pb) and 0.08% V2O5 ABUG0036 10m @ 4.96% Pb+Zn (4.44% Zn and 0.52% Pb) and 0.13% V2[O] 5 including 3m @ 11.05% Pb+Zn (10.55% Zn and 0.50% Pb) and 0.00% V2O5**
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Figure 1 – Ultra high resolution ae r ial photograph y overlain by n e w surface channel sampling r e sults. Open pi t outlines are shown in grey a n d interpreted m ineralisation footprint in red.
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Figure 2 – Schem a tic cross secti o n through the C hristiana deposit showing the depth of surfa c e mining, unde r ground develo p ment, outline f r om sampling i n formation and p lanned drilling .
BACKGRO U ND
The Christiana zinc prosp e ct and min e is located in Golden D eeps’ nort h ernmost te n ement (EPL 3543) of its Grootfo n tein Base Metals project, in nort h ern Nami b ia. Christia n a was for m erly known as “Abena b West”.
Chr i stiana was mined between 1947 a n d 1958, wi t h extensive level devel o pment car r ied out ove r at least 1, 0 00 metres of strike. S o me 540,00 0 t was min e d during th e period fro m open cut s and the u pper level s of the m ine. Exten s ive capital developm e nt in the f orm of underground d r ives and c r oss cuts w ere constr u cted in preparation fo r additional deeper min i ng. The mi n e was clo s ed in 1958 leaving the development accessi b le. Broad z o nes of sha l low high-gr a de zinc, le a d and van a dium mineralisation re m ain in situ.
The 540,000t m ined from Christiana produced the followin g concentra t es, predo m inantly usi n g simple gr a vity conce n tration met h ods;
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73,739t of vanadiu m concentrates grading 72% Pb an d 13% V2O 5 ,
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6,000t o f lead conc e ntrates gr a ding 72% P b
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8,500t o f zinc conc e ntrates grading 55% Z n
Chr i stiana’s hi s tory supports the successful us e of gravity separation technique s which rep r esent a rel a tively low capital expe n diture opti o n for future mine devel o pment, as well as offering a shor t lead time t o producti o n. This co u ld greatly e nhance th e economic s of the Chr i stiana Proj e ct.
Pre v ious miner s targeted the lead-va n adium des c loizite rich mineralisat i on and left behind mu c h of the ve r y high grad e zinc wille m ite rich mi n eralisation. The remna n t mineral r e source is e xpected to be higher in zinc and lower in l e ad and vanadium in c ontrast to historic pro d uction figu r es.
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Figure 3 – Location of the Christia n a Zinc Mine & Prospect
Mo d ern day analogues of t he mineral o gy observ e d at Christi a na occur a t Skorpion Mine in Na m ibia and B e ltana Mine in South Australia. At B eltana, a direct shippi n g zinc prod u ct was pro d uced by t h e blending of high gr a de willemite ores. At S korpion a special ult r a-pure, pre m ium priced zinc catho d e is produ c ed by solvent extractio n and electr o winning fr o m ores of s m ithsonite, h ydrozincit e , tarbuttite a nd willemit e .
O N GOING E XPLORA T ION AT CHRISTI A NA
A s u rvey of the undergrou n d workings and open p its is underway and is due for co m pletion in D ecember, w ith process e d results a v ailable in January 201 3 . The surv e y will provi d e a 3D voi d model of t h e undergr o und mine w orkings an d the open p its, and wi l l provide the basis for f ully deplet e d 3D mod e lling of th e mineralisation. This w ill enable t h e estimati o n of a likely mineral r e source and to accurately target fut u re resourc e drilling pr o grammes.
A p rogramme of shallow RC drilling is planned to estimate a JORC compliant mineral res o urce for C h ristiana. T h e drilling w ill initially t a rget nomin a l open pit d epths of less than 100m. The dril l ing will als o provide re p resentative bulk sampl e s for preli m inary metallurgical test work. See F igure 2.
For further information please contact:
Mr L uke Marsh a ll, General Manager - E xploration Phone (08 ) 9481 783 3
Or consult our website: www.golde n deeps.co m
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ABOUT GOLDEN DEEPS LIMITED
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Figure 4 – Th e Grootfontein B ase Metal Proj e ct, Otavi Mountain Land, Na m ibia
Gol d en Deeps L imited is a n ASX listed company ( A SX: GED) f ocused on e xploration for gold and base metal s . The com p any has pr o jects in Vict o ria, Western Australia a nd the Republic of Na m ibia.
The Company’ s current focus is its 1, 1 00km[2 ] Gro o tfontein Ba s e Metal Pr o ject locate d in the Ota v i Mountain Land (OM L ) of Northern Namibia, an area r o ughly bou n ded by a t riangle linking the tow n s of Tsumeb, Grootf o ntein and O tavi. The region hos t s several g lobally sig n ificant cop p er, zinc, lead, silver and vanadium mines, i n cluding th e Tsumeb, Khusib Springs, Abenab, Berg Aukas & Kombat mines.
The region is w ell served b y sealed r o ads, rail t o port, high voltage po w er, teleph o ne and wat e r and is close to maj o r towns a n d mining processing f a cilities, including the K ombat cop p er concen t rator and T sumeb Sm e lter compl e x (one of o nly five op e rating sm e lters in Afri c a).
The Grootfonte i n Project h as a num b er of signi f icant prosp e cts near h istorical pr o duction cen t res located on its licenc e package. T hese prospects include the Askevold Copper tr e nd, the Abenab/Christiana Zinc-Vanadium Lead trend and t h e Khusib S p rings Copp e r prospect.
The Company p lans to ac t ively explor e its Projec t area with a view to d efinition of mineral res o urces.
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Competent Person Declaration
The information in t his report that relates to Ex p loration Resul t s, Mineral Re s ources or Ore Reserves is b ased on infor m ation compile d by Luke Mars h all, who is a m ember of The A ustralasian Institute of Geosc i entists. Mr Marshall has suffi c ient experienc e that is releva n t to the style o f mineralisation and type of d eposit under c onsideration a n d to the activ i ty that he is un d ertaking to qu a lify as a Com p etent Person a s defined in the 2004 Edition o f the “Australasian Code for Reporting of Ex p loration Result s , Mineral Res o urce and Ore R eserves”. Mr M arshall conse n ts to the inclusion in the repo r t of the matter s based on his i n formation in the form and con t ext in which it a ppears.
Forward-Looking Statements
This document ma y include forward-looking stat e ments. Forwa r d-looking stat e ments include , but are not limited to, statements concerning Golden D e eps Limited’s p lanned explo r ation program m e and other s tatements tha t are not histo r ical facts. Wh e n used in this document, the words such a s "could," "plan , " "estimate," " e xpect," "intend," "may”, "pot e ntial," "should, " and similar e x pressions are f orward-looking statements. Al t hough Golden Deeps Limited believes that i ts expectation s reflected in these forward-lo o king statements are reasona b le, such state m ents involve r isks and uncertainties and n o assurance ca n be given that a ctual results w i ll be consistent with these for w ard-looking st a tements.
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Appendix 1 Christiana channel sampling results
| L evel |
Hole ID | Length | Collar Lo | c ation WGS84 Z33 |
c ation WGS84 Z33 |
Dip |
Azimuth |
F |
ro m m |
To m |
Pb+ % |
Z n |
Width m |
Intersection Descrip | t ion |
|||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| East | North | RL | ||||||||||||||||
| Surfac | e | ABCS0001 | 40 | 824991 | 7 863821 |
1295 | 0 | 330 | 2 | 9 | 0. | 3 | 7 | 7m@ 0 | . 18%Zn, 0.12%Pb, 0.02 |
% V2O5** |
||
| 1 3 |
37 | 0.2 | 7 | 24 | 24m@ | 0 .21% Zn,0.06% Pb,0.0 |
2 % V2O5** |
|||||||||||
| ABCS0002 | 49 | 825018 | 7 863790 |
1297 | 0 | 330 | 1 1 |
21 | 1.7 | 3 | 10 | 10m@ | 1 .24% Zn,0.50% Pb,0.0 |
8 % V2O5 |
||||
| ABCS0003 | 50 | 825033 | 7 863817 |
1296 | 0 | 330 | 6 | 18 | 1.3 | 3 | 12 | 12m@ | 1 .01%Zn, 0.33%Pb, 0.0 |
3 %V2O5 |
||||
| 2 5 |
33 | 1.8 | 3 | 8 | 8m@1 | . 49% Zn,0.35% Pb,0.02 |
% V2O5* |
|||||||||||
| ABCS0004 | 43 | 825055 | 7 863827 |
1296 | 0 | 330 | 0 | 20 | 5.2 | 1 | 20 | 20m@ | 3 .48%Zn,1.73%Pb, 0.2 |
7 %V2O5 |
||||
| 2 | 9 | 9.6 | 8 | 7 | 7m@ 5 | . 51%Zn,4.18%Pb, 0.56 |
% V2O5 |
|||||||||||
| 2 4 |
33 | 0. | 7 | 9 | 9m@ 0 | . 44%Zn, 0.26%Pb, 0.06 |
% V2O5 |
|||||||||||
| 2 4 |
28 | 1.1 | 2 | 4 | 4m@0 | . 64% Zn,0.48% Pb,0.10 |
% V2O5 |
|||||||||||
| ABCS0005 | 47 | 825075 | 7 863839 |
1295 | 0 | 330 | 7 | 22 | 0. | 8 | 15 | 15m@ | 0 .53%Zn, 0.27%Pb, 0.0 |
2 %V2O5 |
||||
| 1 1 |
15 | 1.3 | 5 | 4 | 4m@0 | . 92% Zn,0.43% Pb,0.06 |
% V2O5 |
|||||||||||
| ABCS0006 | 65 | 825097 | 7 863823 |
1295 | 0 | 330 | 1 9 |
28 | 0.3 | 9 | 9 | 9m@0 | . 32% Zn,0.07% Pb,0.01 |
% V2O5 |
||||
| ABCS0007 | 46 | 825102 | 7 863848 |
1295 | 0 | 330 | 2 | 19 | 1.4 | 3 | 17 | 17m@ | 1 .28% Zn,0.14% Pb,0.0 |
3 % V2O5 |
||||
| ABCS0008 | 53 | 825117 | 7 863855 |
1295 | 0 | 330 | 3 | 50 | 4.5 | 2 | 47 | 47m@ | 4 .37%Zn, 0.15%Pb, 0.0 |
2 %V2O5 |
||||
| 3 9 |
50 | 15 | .3 | 11 | **11m@ ** | 1 4.94% Zn, 0.36% Pb, 0 |
. 02% V2O5 |
|||||||||||
| ABCS0010 | 53 | 825150 | 7 863873 |
1295 | 0 | 330 | 5 | 25 | 3.8 | 4 | 20 | 20m@ | 3 .03%Zn, 0.81%Pb, 0.2 |
6 %V2O5 |
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| 1 7 |
22 | 12. | 0 2 |
5 | 5m @ 9 | . 49% Zn, 2.54% Pb, 0.8 |
8 % V2O5 |
|||||||||||
| 3 4 |
53 | 2. | 4 | 19 | 19m@ | 1 .87%Zn, 0.53%Pb, 0.0 |
2 %V2O5 |
|||||||||||
| 3 4 |
40 | 6.2 | 1 | 6 | 6m@5 | . 12% Zn,1.08% Pb,0.01 |
% V2O5 |
|||||||||||
| ABCS0012 | 69 | 825177 | 7 863896 |
1296 | 0 | 330 | 0 | 32 | 3.2 | 1 | 32 | 32m@ | 2 .64%Zn, 0.60%Pb, 0.1 |
5 %V2O5* |
||||
| 2 3 |
24 | 23. | 4 4 |
1 | 1m@ 2 | 2 .42% Zn, 1.02% Pb, 0. |
1 6% V2O5** |
|||||||||||
| ABCS0013 | 14 | 825173 | 7 863956 |
1294 | 0 | 250 | 0 | 13 | 6.0 | 4 | 13 | 13m@ | 4 .56%Zn,1.48%Pb, 0.1 |
3 %V2O5 |
||||
| 1 1 |
13 | 13. | 9 3 |
2 | 2m@ 1 | 1 .30% Zn, 2.63% Pb, 0. |
1 2% V2O5 |
|||||||||||
| ABCS0014 | 58 | 825193 | 7 863904 |
1294 | 0 | 330 | 0 | 47 | 0.8 | 2 | 47 | 47m@ | 0 .52% Zn,0.30% Pb,0.0 |
5 % V2O5 |
||||
| ABCS0015 | 56 | 825205 | 7 863920 |
1294 | 0 | 330 | 1 0 |
53 | 0.2 | 6 | 43 | 43m@ | 0 .14% Zn,0.12% Pb,0.0 |
3 % V2O5 |
||||
| ABCS0016 | 25 | 825257 | 7 863914 |
1294 | 0 | 330 | 9 | 15 | 0.7 | 2 | 6 | 6m@0 | . 62% Zn,0.10% Pb,0.01 |
% V2O5 |
||||
| ABCS0017 | 35 | 825276 | 7 863921 |
1294 | 0 | 330 | 1 4 |
21 | 0.8 | 0 | 7 | 7m@0 | . 70% Zn,0.10% Pb,0.01 |
% V2O5 |
||||
| ABCS0018 | 18 | 825296 | 7 863926 |
1294 | 0 | 330 | 1 6 |
17 | 0.3 | 1 | 1 | 1m@0 | . 16% Zn,0.14% Pb,0.15 |
% V2O5** |
||||
| ABCS0019 | 56 | 825314 | 7 863936 |
1295 | 0 | 330 | 2 2 |
25 | 0.4 | 4 | 3 | 3m@0 | . 40% Zn,0.04% Pb,0.00 |
% V2O5 |
||||
| ABCS0020 | 57 | 825334 | 7 863946 |
1295 | 0 | 330 | 1 1 |
22 | 2.1 | 9 | 11 | 11m@ | 1 .84% Zn,0.35% Pb,0.0 |
0 % V2O5 |
||||
| ABCS0021 | 56 | 825354 | 7 863955 |
1296 | 0 | 330 | 9 | 37 | 1.2 | 2 | 28 | 28m@ | 1 .05%Zn, 0.16%Pb, 0.0 |
1 %V2O5 |
||||
| 2 3 |
25 | 6.3 | 4 | 2 | 2m@6 | . 06% Zn,0.28% Pb,0.00 |
% V2O5 |
|||||||||||
| ABCS0022 | 47 | 825371 | 7 863962 |
1296 | 0 | 330 | 5 | 12 | 1.8 | 3 | 7 | 7m@1 | . 68%Zn, 0.15%Pb, 0.02 |
% V2O5 |
||||
| 2 8 |
31 | 3.2 | 6 | 3 | 3m@2 | . 29% Zn,0.97% Pb,0.00 |
% V2O5 |
|||||||||||
| ABCS0023 | 52 | 825391 | 7 863970 |
1296 | 0 | 330 | 1 8 |
34 | 10. | 0 3 |
16 | **16m@ ** | 9 .84% Zn, 0.19% Pb, 0. |
0 2% V2O5 |
||||
| ABCS0024 | 47 | 825411 | 7 863987 |
1297 | 0 | 330 | 5 | 15 | 14. | 3 4 |
10 | **10m@ ** | 1 4.15% Zn, 0.20% Pb, 0 |
. 01% V2O5 |
||||
| ABCS0025 | 48 | 825427 | 7 863995 |
1297 | 0 | 330 | 0 | 16 | 0.1 | 5 | 16 | 16m@ | 0 .08% Zn,0.07% Pb,0.0 |
7 % V2O5** |
||||
| ABCS0026 | 30 | 824973 | 7 863774 |
1298 | 0 | 330 | 5 | 7 | 0.7 | 7 | 2 | 2m@0 | . 11% Zn,0.67% Pb,0.09 |
% V2O5 |
||||
| 200 Ft | L evel |
ABUG0001 | 28 | 825025 | 7 863875 |
1229 | 0 | 190 | 3 | 22 | 0.3 | 7 | 19 | 19m@ | 0 .31% Zn,0.06% Pb,0.0 |
0 % V2O5 |
||
| ABUG0002 | 108 | 825021 | 7 863876 |
1229 | 0 | 236 | 5 9 |
64 | 1.3 | 0 | 5 | 5M@0 | . 93% Zn,0.37% Pb,0.00 |
% V2O5 |
||||
| ABUG0003 | 30 | 824979 | 7 863844 |
1229 | 0 | 210 | 9 | 17 | 0.5 | 4 | 8 | 8m@0 | . 43% Zn,0.11% Pb,0.00 |
% V2O5 |
||||
| ABUG0004 | 10 | 824959 | 7 863832 |
1229 | 0 | 180 | 5 | 6 | 0.7 | 2 | 1 | 1m@0 | . 44% Zn,0.28% Pb,0.00 |
% V2O5 |
||||
| ABUG0005 | 50 | 825159 | 7 863913 |
1229 | 0 | 240 | 2 6 |
40 | 1.0 | 1 | 14 | 14m@ | 0 .82% Zn,0.19% Pb,0.0 |
0 % V2O5 |
||||
| ABUG0006 | 39 | 825162 | 7 863916 |
1229 | 0 | 330 | 3 0 |
31 | 0.4 | 5 | 1 | 1m@0 | . 40% Zn,0.05% Pb,0.00 |
% V2O5 |
||||
| ABUG0007 | 30 | 825162 | 7 863916 |
1229 | 0 | 90 | 1 4 |
25 | 0.5 | 1 | 11 | 11m@ | 0 .45% Zn,0.05% Pb,0.0 |
0 % V2O5 |
||||
| ABUG0008 | 21 | 825192 | 7 863916 |
1229 | 0 | 320 | 0 | 17 | 0.4 | 0 | 17 | 17m@ | 0 .33% Zn,0.07% Pb,0.0 |
0 % V2O5 |
||||
| 50 Ft L | e vel |
ABUG0009 | 11 | 824990 | 7 863793 |
1275 | 0 | 340 | 7 | 11 | 0.4 | 7 | 4 | 4m@0 | . 34% Zn,0.13% Pb,0.09 |
% V2O5** |
||
| ABUG0010 | 13 | 825016 | 7 863807 |
1275 | 0 | 315 | NSI | |||||||||||
| ABUG0011 | 14 | 825033 | 7 863819 |
1275 | 0 | 335 | 9 | 13 | 0.4 | 7 | 4 | 4m@0 | . 28% Zn,0.19% Pb,0.10 |
% V2O5** |
||||
| ABUG0012 | 23 | 825040 | 7 863823 |
1275 | 0 | 346 | 1 2 |
23 | 4.4 | 5 | 11 | 11m@ | 3 .64%Zn, 0.81%Pb, 0. |
27 %V2O5 |
||||
| 2 2 |
23 | 14. | 2 7 |
1 | 1m@ 1 | 1 .20% Zn, 3.07% Pb, 0. |
6 4% V2O5 |
|||||||||||
| ABUG0013 | 8 | 825055 | 7 863829 |
1275 | 0 | 338 | 1 | 6 | 0.4 | 0 | 5 | 5m@0 | . 34% Zn,0.06% Pb,0.12 |
% V2O5 |
||||
| ABUG0014 | 17 | 825077 | 7 863836 |
1275 | 0 | 314 | 1 0 |
16 | 0.7 | 8 | 6 | 6m@0 | . 55% Zn,0.23% Pb,0.05 |
% V2O5 |
||||
| ABUG0015 | 17 | 825088 | 7 863843 |
1275 | 0 | 330 | 0 | 4 | 1.2 | 8 | 4 | 4m@0 | . 92% Zn,0.36% Pb,0.15 |
% V2O5 |
||||
| ABUG0016 | 23 | 825101 | 7 863851 |
1275 | 0 | 330 | 1 6 |
20 | 5.5 | 7 | 4 | 4m@4 | . 87% Zn,0.70% Pb,0.16 |
% V2O5 |
||||
| ABUG0016A | 5 | 825091 | 7 863868 |
1275 | 0 | 60 | 1 | 4 | 9.7 | 4 | 3 | 3m@6 | . 91% Zn,2.83% Pb,0.14 |
% V2O5 |
||||
| ABUG0018 | 18 | 825114 | 7 863859 |
1275 | 0 | 344 | 4 | 12 | 1.1 | 0 | 8 | 8m@0 | . 90% Zn,0.20% Pb,0.04 |
% V2O5 |
||||
| ABUG0019 | 40 | 825134 | 7 863866 |
1275 | 0 | 317 | 1 3 |
35 | 5.7 | 8 | 22 | 22m@ | 5 .42%Zn, 0.35%Pb, 0.1 |
0 %V2O5 |
||||
| 2 1 |
27 | 14. | 0 1 |
6 | 6m@ 1 | 3 .08% Zn, 0.93% Pb, 0. |
2 8% V2O5 |
|||||||||||
| ABUG0020 | 20 | 825147 | 7 863879 |
1275 | 0 | 336 | 5 | 20 | 7.3 | 4 | 15 | 15m@ | 6 .74%Zn, 0.60%Pb, 0.1 |
9 %V2O5 |
||||
| 1 6 |
20 | 18. | 8 0 |
4 | 4m@ 1 | 8 .36% Zn, 0.44% Pb, 0. |
0 3% V2O5 |
|||||||||||
| ABUG0021 | 13 | 825159 | 7 863886 |
1275 | 0 | 331 | 0 | 12 | 5.3 | 6 | 12 | 12m@ | 3 .08%Zn,2.28%Pb, 0.8 |
5 %V2O5 |
||||
| 1 0 |
11 | 28. | 3 5 |
1 | 1m@ 8 | . 65% Zn, 19.70% Pb, 7. |
0 2% V2O5 |
|||||||||||
| ABUG0022 | 44 | 825168 | 7 863892 |
1275 | 0 | 337 | 0 | 44 | 22. | 1 1 |
44 | **44m@ ** | 2 0.39% Zn, 1.71% Pb, 0 |
. 53% V2O5 |
||||
| 1 6 |
28 | 39. | 6 6 |
12 | **12m@ ** | 3 7.52% Zn, 2.15% Pb, 0 |
. 70% V2O5 |
|||||||||||
| ABUG0023 | 7 | 825179 | 7 863898 |
1275 | 0 | 333 | 3 | 5 | 0.8 | 7 | 2 | 2m@0 | . 49% Zn,0.38% Pb,0.16 |
% V2O5** |
||||
| ABUG0024 | 7 | 825180 | 7 863899 |
1275 | 0 | 9 | 2 | 6 | 0.4 | 7 | 4 | 4m@0 | . 23% Zn,0.24% Pb,0.10 |
% V2O5** |
||||
| ABUG0025 | 21 | 825185 | 7 863902 |
1275 | 0 | 0 | 3 | 20 | 0.3 | 6 | 17 | 17m@ | 0 .26% Zn,0.10% Pb,0.0 |
3 % V2O5** |
||||
| ABUG0026 | 6 | 825200 | 7 863905 |
1275 | 0 | 0 | 1 | 6 | 0.3 | 2 | 5 | 5m@0 | . 24% Zn,0.08% Pb,0.06 |
% V2O5** |
||||
| ABUG0027 | 18 | 825216 | 7 863905 |
1275 | 0 | 357 | 1 3 |
16 | 15. | 9 3 |
3 | 3m@ 1 | 5 .79% Zn, 0.14% Pb, 0. |
0 4% V2O5** |
||||
| ABUG0028 | 15 | 825231 | 7 863906 |
1275 | 0 | 326 | 5 | 14 | 0.8 | 7 | 9 | 9m@0 | . 75% Zn,0.12% Pb,0.02 |
% V2O5 |
||||
| ABUG0029 | 7 | 825244 | 7 863914 |
1275 | 0 | 342 | 4 | 7 | 1.5 | 5 | 3 | 3m@1 | . 44% Zn,0.12% Pb,0.01 |
% V2O5 |
||||
| ABUG0030 | 13 | 825258 | 7 863921 |
1275 | 0 | 331 | 3 | 9 | 1.3 | 6 | 6 | 6m@1 | . 19% Zn,0.18% Pb,0.03 |
% V2O5 |
||||
| ABUG0031 | 10 | 825272 | 7 863928 |
1275 | 0 | 331 | 1 | 2 | 0.5 | 4 | 1 | 1m@0 | . 40% Zn,0.14% Pb,0.11 |
% V2O5** |
||||
| ABUG0032 | 7 | 825296 | 7 863935 |
1275 | 0 | 333 | 2 | 6 | 1.0 | 9 | 4 | 4m@0 | . 99% Zn,0.09% Pb,0.01 |
% V2O5 |
||||
| ABUG0033 | 39 | 825327 | 7 863944 |
1275 | 0 | 342 | 1 2 |
38 | 0.6 | 7 | 26 | 26m@ | 0 .44% Zn,0.23% Pb,0.0 |
7 % V2O5 |
8
==> picture [5 x 41] intentionally omitted <==
==> picture [55 x 41] intentionally omitted <==
==> picture [28 x 41] intentionally omitted <==
| L evel |
Hole ID | Length | Collar Lo | c ation WGS84 Z33 |
c ation WGS84 Z33 |
Dip | Azimuth | F | ro m m |
To m |
Pb+ % |
Z n |
Width m |
Intersection Descrip | t ion |
|||
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| East | North | RL | ||||||||||||||||
| Vertic | a l channels |
ABUG0034 | 11 | 825107 | 7 863875 |
1286 | ‐90 | 0 | 0 | 10 | 10. | 3 9 |
10 | **10m@ ** | 9 .51% Zn, 0.88% Pb, 0. |
0 8% V2O5 |
||
| ABUG0035 | 11 | 825118 | 7 863895 |
1286 | ‐90 | 0 | 0 | 6 | 4.2 | 9 | 6 | 6m@4 | . 00% Zn,0.29% Pb,0.00 |
% V2O5 |
||||
| ABUG0036 | 11 | 825146 | 7 863889 |
1286 | ‐90 | 0 | 0 | 10 | 4.9 | 6 | 10 | 10m@ | 4 .44%Zn, 0.52%Pb, 0.1 |
3 %V2O5 |
||||
| 7 | 10 | 11. | 0 5 |
3 | 3m@ 1 | 0 .55% Zn, 0.50% Pb, 0. |
0 0% V2O5 |
|||||||||||
| ABUG0037 | 4 | 825175 | 7 863907 |
1279 | ‐90 | 0 | 0 | 4 | 4.2 | 6 | 4 | 4m@3 | . 50% Zn,0.76% Pb,0.29 |
% V2O5 |
||||
| ABUG0038 | 15 | 825258 | 7 863919 |
1290 | ‐90 | 0 | 0 | 15 | 2.2 | 4 | 15 | 15m@ | 2 .08% Zn,0.15% Pb,0.0 |
1 % V2O5 |
||||
| ABUG0039 | 6 | 825162 | 7 863947 |
1294 | ‐90 | 0 | 0 | 6 | 5.6 | 9 | 6 | 6m@4 | . 22% Zn,1.47% Pb,0.05 |
% V2O5 |
||||
| ABUG0040 | 17 | 825162 | 7 863947 |
1288 | 0 | 152 | 0 | 17 | 5.9 | 7 | 17 | 17m@ | 3 .93% Zn,2.05% Pb,0.3 |
2 % V2O5 |
||||
| ABUG0047 | 12 | 825156 | 7 863887 |
1275 | ‐90 | 0 | 0 | 12 | 2.3 | 8 | 12 | 12m@ | 1 .89% Zn,0.50% Pb,0.2 |
0 % V2O5 |
||||
| 100 ft | le vel |
ABUG0048 | 16 | 825156 | 7 863887 |
1260 | 0 | 143 | 1 | 5 | 1.0 | 7 | 4 | 4m@0 | . 81% Zn,0.26% Pb,0.10 |
% V2O5 |
||
| ABUG0049 | 59 | 825152 | 7 863867 |
1260 | 0 | 351 | 1 9 |
21 | 2.3 | 7 | 2 | 2m@1 | . 78% Zn,0.59% Pb,0.00 |
% V2O5 |
||||
| ABUG0050 | 25 | 825138 | 7 863862 |
1260 | 0 | 333 | 1 7 |
18 | 0.5 | 7 | 1 | 1m@0 | . 42% Zn,0.15% Pb,0.00 |
% V2O5** |
||||
| ABUG0051 | 13 | 825135 | 7 863861 |
1260 | 0 | 293 | 5 | 13 | 1.6 | 9 | 8 | 8m@1 | . 46% Zn,0.23% Pb,0.13 |
% V2O5 |
||||
| ABUG0052 | 28 | 825124 | 7 863858 |
1260 | 0 | 337 | 1 8 |
19 | 1.4 | 8 | 1 | 1m@1 | . 40% Zn,0.08% Pb,0.00 |
% V2O5** |
||||
| ABUG0053 | 16 | 825110 | 7 863854 |
1260 | 0 | 338 | 3 | 5 | 2.1 | 2 | 2 | 2m@1 | . 52% Zn,0.60% Pb,0.15 |
% V2O5** |
||||
| ABUG0054 | 13 | 825095 | 7 863850 |
1260 | 0 | 347 | 8 | 12 | 2.0 | 1 | 4 | 4m@1 | . 52% Zn,0.49% Pb,0.00 |
% V2O5 |
||||
| ABUG0055 | 13 | 825074 | 7 863845 |
1260 | 0 | 347 | 3 | 11 | 0.8 | 7 | 8 | 8m@0 | . 77% Zn,0.10% Pb,0.03 |
% V2O5 |
||||
| ABUG0056 | 6 | 825059 | 7 863843 |
1260 | 0 | 353 | 3 | 6 | 0.5 | 5 | 3 | 3m@0 | . 49% Zn,0.05% Pb,0.00 |
% V2O5 |
||||
| ABUG0057 | 16 | 825044 | 7 863837 |
1260 | 0 | 334 | 2 | 16 | 1.5 | 8 | 14 | 14m@ | 1 .18% Zn,0.40% Pb,0.1 |
1 % V2O5 |
||||
| ABUG0058 | 2 | 825029 | 7 863829 |
1260 | 0 | 333 | NSI | |||||||||||
| ABUG0059 | 3 | 825011 | 7 863823 |
1260 | 0 | 342 | 0 | 3 | 1.6 | 2 | 3 | 3m@1 | . 36% Zn,0.26% Pb,0.08 |
% V2O5 |
||||
| ABUG0060 | 4 | 824995 | 7 863814 |
1260 | 0 | 326 | 0 | 2 | 0.6 | 3 | 2 | 2m@0 | . 34% Zn,0.29% Pb,0.04 |
% V2O5 |
-
Intervals are a combination of handheld X R F and laboratory assays
-
** Intervals are b y handheld X R F only
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----- Start of picture text -----
APPENDIX 2 Underground Level Plans showing sample locations .
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Figure 5 – 50ft l e vel plan showing channel sa m ple locations and interpreted m ineralisation f o otprint in red outline
----- End of picture text -----
9
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Figure 6 – 100ft level plan sho w ing channel sa m ple locations a nd interpreted mineralisation f ootprint in red o utline
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Figure 7 – 200ft level plan sho w ing channel sa m ple locations a nd interpreted mineralisation f ootprint in red o utline
10