6 Jun 2008 08:48
ο»Ώ
6Β JuneΒ 2008
HIGHLY ENCOURAGINGΒ DRILLΒ RESULTS EXTEND GAMBUTAΒ MINERALISATION
RESOURCE ESTIMATE PENDING
The Directors of Berkeley Resources Limited (AIM:Β BKY.L) are pleased to adviseΒ more encouragingΒ resultsΒ fromΒ theΒ current drilling programme at the Gambuta project in CΓ‘ceresΒ Province, Spain.Β
The ongoingΒ program ofΒ reverse circulation and diamond drillingΒ hasΒ continuedΒ to produceΒ consistentlyΒ positiveΒ resultsΒ which have extended theΒ strike length of the deposit to 1300m,Β with widths ranging from 250mΒ inΒ the south-east to 350mΒ at the north-west limit of drilling.Β Strong mineralisation remains open to the north-westΒ beneath Tertiary cover.Β
Since the announcement of results from the first four diamond drill holes on 10 April 2008,Β 21 RC holes and an additional 6 diamond holes have been completed.Β InΒ theΒ total ofΒ 31Β holesΒ drilledΒ to date,Β 26Β (84%)Β haveΒ encountered mineralisationΒ over depths ranging fromΒ surface to 94m, with most mineralisation within 50m of surface.Β These results provide comprehensive confirmation, and extension, of the historical roto-percussion program in which 21 of the 24Β CISAΒ holes intersected uranium mineralisation.Β Assay results areΒ nowΒ available forΒ an additionalΒ thirteenΒ holesΒ drilled byΒ BerkeleyΒ and include:
|
Hole |
INTERSECTION |
FROM |
|
GAM-003 |
3.0 metres @ 0.0281%Β U3O8 |
8.0m |
|
4.0 metresΒ @ 0.0359%Β U3O8 |
12.0m |
|
|
3.2Β metresΒ @ 0.0540%Β U3O8 |
25.0m |
|
|
6.5Β metresΒ @ 0.0561%Β U3O8 |
29.5m |
|
|
GAM-005 |
3.0 metres @ 0.0218%Β U3O8 |
7.5m |
|
22.2Β metresΒ @ 0.0541%Β U3O8 |
13.8m |
|
|
GAM-006 |
7.0 metres @ 0.0648%Β U3O8 |
43.0m |
|
3.0 metresΒ @ 0.0498%Β U3O8 |
66.0m |
|
|
GAMR-011 |
3.0 metres @ 0.1045%Β U3O8 |
30.0m |
|
3.0 metresΒ @ 0.0414%Β U3O8 |
64.0m |
|
|
2.0Β metresΒ @ 0.0686%Β U3O8 |
83.0m |
|
|
GAMR-013 |
3.0Β metresΒ @ 0.2465%Β U3O8 |
27.0m |
|
5.0Β metresΒ @ 0.0408%Β U3O8 |
35.0m |
|
|
5.0 metres @ 0.0791%Β U3O8 |
45.0m |
|
|
3.0 metresΒ @ 0.0263%Β U3O8 |
56.0m |
|
|
GAM-017 |
19.0 metres @ 0.0495%Β U3O8 |
7.0m |
|
18.0 metresΒ @ 0.0992%Β U3O8 |
33.0m |
|
|
4.0Β metresΒ @ 0.0494%Β U3O8 |
60.0m |
|
|
GAMR-018 |
7.0Β metresΒ @ 0.0485%Β U3O8 |
7.0m |
Results of the downhole probes forΒ the remainingΒ BerkeleyΒ holes suggestΒ that assay results will yieldΒ similar gradesΒ and thicknessesΒ for shallowΒ and deeperΒ mineralisation.Β
Drilling to date has twinned a number ofΒ theΒ historical roto-percussion holes; completed profiles through the historically defined mineralised zone;Β successfully tested beneath the previously undrilled Tertiary cover in the central section of the deposit:Β and extendedΒ itΒ beneathΒ TertiaryΒ cover to the north-west.Β The complete set of available assay results are summarisedΒ in the table below.
The GambutaΒ mineralisation occurs in a 1300m byΒ 250-350mΒ wideΒ north-westerly trending litho-structural zone adjacent to a protrusion in the granite batholith. Host rock lithologiesΒ and mineralisationΒ areΒ similar to those recordedΒ atΒ Berkeley's Retortillo project.Β Within this zone theΒ most strongly mineralisedΒ areasΒ occur withinΒ a 150m wide zone ofΒ steeply dipping shears and fracturesΒ to depths of about 100m.Β
ThisΒ structurally disrupted zone has been intruded by aplitic dykesΒ thatΒ appear to result in some concentration of mineralisationΒ into thin, higher-grade zonesΒ (+0.06% U3O8).Β In profiles that show intact Tertiary cover, theΒ deeperΒ primary mineralisationΒ isΒ overlain byΒ a wider (up toΒ ~350m) zone of secondaryΒ lower grade (~0.03% U3O8)Β mineralisationΒ whichΒ extends up to within about 30m of surface. This secondary mineralisation is aboutΒ 10m thickΒ in the central section, but thinsΒ laterally to about 2-5m.Β
Interpretation of theΒ drillingΒ results, recent geological mapping,Β and an airborne radiometric and magnetic survey,Β indicateΒ potential for extensions of the mineralised structural zone to the north-west,Β parallel to the interpreted sub-surface granite contact. Superimposing topography ontoΒ the geologicalΒ and geophysical interpretationsΒ of thisΒ slightly plunging mineralisedΒ zone suggestsΒ potential forΒ mineralisationΒ to extend aboutΒ 1kmΒ to the north-westΒ beforeΒ it is likely to beΒ truncated byΒ incisedΒ topography. The granite contact reducesΒ the potential for extensions to the south and east.
Although fire season regulationsΒ require cessation of drilling activity in early June,Β the consistency ofΒ Berkeley'sΒ results to date, together with remaining assaysΒ and the historical information,Β willΒ generateΒ sufficientΒ data toΒ enable calculation of an inferred resource estimate inΒ the next quarter. This estimate will beΒ followed by a new drilling campaign aimed at infill and testing the limits of the potential north-west extension.Β
Enquiries - Managing Director: Matt Syme Tel:Β Β +61 417 906 717
Β
RBC Capital Markets: Martin Eales Tel: +44 20 7029 7881
Β
TABLE 1. DRILL DETAILS and INTERSECTIONSΒ (200ppm cut-off)
|
HOLE_ID |
UTM_E (m) |
UTM_N (m) |
RL |
Inclination |
EOH |
From |
To |
Interval |
%U3O8 |
|
GAM-001 |
291,730 |
4,404,118 |
387 |
-60 to 000 |
103.0 |
0.0 |
8.0 |
8.0 |
0.0586 |
|
10.0 |
11.0 |
1.0 |
0.0218 |
||||||
|
19.0 |
20.0 |
1.0 |
0.0512 |
||||||
|
34.0 |
35.5 |
1.5 |
0.0301 |
||||||
|
37.5 |
38.5 |
1.0 |
0.0389 |
||||||
|
45.0 |
46.0 |
1.0 |
0.0768 |
||||||
|
55.0 |
56.0 |
1.0 |
0.0343 |
||||||
|
58.5 |
59.5 |
1.0 |
0.0338 |
||||||
|
GAM-002 |
292,381 |
4,403,899 |
369 |
-60 to 000 |
85.0 |
0.0 |
12.5 |
12.5 |
0.0741 |
|
21.5 |
22.5 |
1.0 |
0.0312 |
||||||
|
24.0 |
25.0 |
1.0 |
0.0394 |
||||||
|
28.0 |
32.0 |
4.0 |
0.0997 |
||||||
|
34.5 |
35.5 |
1.0 |
0.0340 |
||||||
|
GAM-003 |
292,368 |
4,403,827 |
353 |
-80 to 000 |
36.0 |
8.0 |
11.0 |
3.0 |
0.0281 |
|
12.0 |
16.0 |
4.0 |
0.0359 |
||||||
|
20.5 |
22.5 |
2.0 |
0.0340 |
||||||
|
23.3 |
24.2 |
1.0 |
0.0707 |
||||||
|
25.0 |
28.2 |
3.2 |
0.0540 |
||||||
|
29.5 |
36.0 |
6.5 |
0.0561 |
||||||
|
GAM-004 |
292,368 |
4,403,828 |
353 |
-70 to 180 |
61.7 |
11.5 |
12.3 |
0.8 |
0.0218 |
|
14.5 |
21.5 |
7.0 |
0.0431 |
||||||
|
22.5 |
23.5 |
1.0 |
0.0397 |
||||||
|
24.5 |
25.5 |
1.0 |
0.0531 |
||||||
|
27.0 |
29.2 |
2.2 |
0.0256 |
||||||
|
34.0 |
35.0 |
1.0 |
0.0285 |
||||||
|
GAM-005 |
292,368 |
4,403,827 |
353 |
-80 to 000 |
36.0 |
7.5 |
10.5 |
3.0 |
0.0218 |
|
13.8 |
36.0 |
22.2 |
0.0541 |
||||||
|
GAMR-006 |
292,368 |
4,404,014 |
397 |
-90 |
100.0 |
40.0 |
41.0 |
1.0 |
0.0239 |
|
43.0 |
50.0 |
7.0 |
0.0648 |
||||||
|
55.0 |
57.0 |
2.0 |
0.0301 |
||||||
|
66.0 |
69.0 |
3.0 |
0.0498 |
||||||
|
76.0 |
77.0 |
1.0 |
0.0232 |
||||||
|
79.0 |
80.0 |
1.0 |
0.0235 |
||||||
|
85.0 |
86.0 |
1.0 |
0.0229 |
||||||
|
90.0 |
91.0 |
1.0 |
0.0635 |
||||||
|
GAMR-007 |
292,067 |
4,403,971 |
402 |
-90 |
82.0 |
28.0 |
29.0 |
1.0 |
0.0529 |
|
31.0 |
33.0 |
2.0 |
0.0228 |
||||||
|
GAMR-008 |
292,315 |
4,404,012 |
404 |
-90 |
90.0 |
34.0 |
35.0 |
1.0 |
0.0348 |
|
45.0 |
46.0 |
1.0 |
0.0241 |
||||||
|
49.00 |
51.00 |
2.00 |
0.0307 |
||||||
|
53.00 |
54.00 |
1.00 |
0.0441 |
||||||
|
55.00 |
57.00 |
2.00 |
0.0393 |
||||||
|
GAM-009 |
292,176 |
4,404,007 |
397 |
-90 |
112.4 |
30.95 |
33.00 |
2.05 |
0.0339 |
|
45.00 |
45.50 |
0.50 |
0.0255 |
||||||
|
54.50 |
56.00 |
1.50 |
0.0495 |
||||||
|
65.50 |
67.50 |
2.00 |
0.0431 |
||||||
|
71.50 |
72.00 |
0.50 |
0.0515 |
||||||
|
72.50 |
73.00 |
0.50 |
0.0219 |
||||||
|
74.50 |
75.00 |
0.50 |
0.0538 |
||||||
|
81.00 |
81.50 |
0.50 |
0.0661 |
||||||
|
82.50 |
84.80 |
2.30 |
0.0242 |
||||||
|
GAMR-010 |
291,993 |
4,403,945 |
399 |
-90 |
81.0 |
25.00 |
27.00 |
2.00 |
0.0373 |
|
GAMR-011 |
291,624 |
4,404,299 |
416 |
-90 |
107.0 |
30.00 |
33.00 |
3.00 |
0.1045 |
|
43.00 |
44.00 |
1.00 |
0.0257 |
||||||
|
64.00 |
67.00 |
3.00 |
0.0414 |
||||||
|
83.00 |
85.00 |
2.00 |
0.0686 |
||||||
|
GAMR-012 |
291,700 |
4,404,349 |
413 |
-90 |
110.0 |
49.00 |
51.00 |
2.00 |
0.0264 |
|
GAMR-013 |
291,550 |
4,404,250 |
416 |
-90 |
105.0 |
27.00 |
30.00 |
3.00 |
0.2465 |
|
35.00 |
40.00 |
5.00 |
0.0408 |
||||||
|
45.00 |
50.00 |
5.00 |
0.0791 |
||||||
|
56.00 |
59.00 |
3.00 |
0.0263 |
||||||
|
82.00 |
84.00 |
2.00 |
0.0511 |
||||||
|
90.00 |
91.00 |
1.00 |
0.0269 |
||||||
|
93.00 |
94.00 |
1.00 |
0.0332 |
||||||
|
GAMR-017 |
291,933 |
4,404,097 |
373 |
-90 |
80.0 |
7.00 |
26.00 |
19.00 |
0.0495 |
|
29.00 |
30.00 |
1.00 |
0.0941 |
||||||
|
33.00 |
51.00 |
18.00 |
0.0992 |
||||||
|
60.00 |
64.00 |
4.00 |
0.0494 |
||||||
|
GAMR-018 |
292,069 |
4,404,163 |
369 |
-90 |
76.0 |
7.00 |
14.00 |
7.00 |
0.0485 |
|
22.00 |
23.00 |
1.00 |
0.0235 |
||||||
|
GAMR-019 |
291,401 |
4,404,095 |
421 |
-90 |
99.0 |
36.00 |
38.00 |
2.00 |
0.0200 |
The Grid has a datum of UTMΒ 30N ED50.Β
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