Latest results include 6.90 Metres at 11.39 g/t Gold (0.33 oz/t over
22.64 ft) and 0.80 Metres at 47.70 g/t Gold (1.39 oz/t over 2.62 ft)
TSX: GEA
TORONTO, Aug. 12 /CNW/ - Gold Eagle Mines Ltd. (TSX: GEA) ("Gold Eagle"
or the "Company") is pleased to announce the latest series of drill results on
the Bruce Channel Discovery ("BCD") at its 100% owned Gold Eagle property
located in Red Lake, Ontario. The Gold Eagle property is situated along the
prolific Red Lake Trend, west of Goldcorp Inc's operating Red Lake and
Campbell Mines and immediately southwest of Goldcorp Inc's past producing
Cochenour-Willans Mine.
Highlights:
- Drilling continues to intersect significant grades and widths
- Drilling continues to encounter multiple high grade zones with
visible gold
- The BCD mineralized envelope extends a minimum of 1,450 metres
vertically with a horizontal footprint of approximately 800 metres
northeast-southwest by 450 metres northwest-southeast
- The BCD mineralized envelope remains open in all directions
- The surface drilling program is continuing as planned
- Phase 1 Closure Plan for the Advanced Underground Exploration Program
accepted by the Ministry of Northern Development and Mines
Highlights of latest drilling:
Hole Number Metres Grams/Tonne Feet Ounces/Ton
(g/t) (oz/t)
------------------------------------------------------------------------
BC 29-9 2.40 17.07 7.87 0.50
------------------------------------------------------------------------
including 0.50 39.60 1.64 1.15
------------------------------------------------------------------------
BC 29-9 0.40 37.30 1.31 1.09
------------------------------------------------------------------------
BC 29-10 1.40 15.38 4.59 0.45
------------------------------------------------------------------------
including 0.70 28.20 2.30 0.82
------------------------------------------------------------------------
BC 29-11 0.80 47.70 2.62 1.39
------------------------------------------------------------------------
BC 33-4 6.90 11.39 22.64 0.33
------------------------------------------------------------------------
including 1.50 22.72 4.92 0.66
------------------------------------------------------------------------
BC 33-4 1.00 25.80 3.28 0.75
------------------------------------------------------------------------
The BCD is a significant gold structure intersected at approximately 800
metres beneath the shallow Bruce Channel waterway. The mineralized envelope is
currently estimated to extend a minimum of 1,450 metres vertically, with a
horizontal footprint of approximately 800 metres northeast-southwest and
approximately 450 metres northwest-southeast. The BCD mineralized envelope
remains open in all directions.
In common with Goldcorp Inc's Red Lake Mine, Campbell Mine and
Cochenour-Willans Mine, the BCD lies within the Balmer Assemblage. The
structural and mineralogical characteristics are very similar to the
aforementioned mines. Gold is found in both its native form as well as within
sulphide rich zones - particularly those with 'felted' fine grained
arsenopyrite. A number of high grade structures have been identified within
the BCD mineralized envelope and these structures exhibit horizontal and
vertical continuity.
BC 29 Series
The BC 29 Series of holes are testing the open area south of the
significant high grade intersections encountered in the BC 19 Series (BC 19-15
and BC 19-16; See press release dated February 13, 2008) which has been named
the "Upper Main Zone". The Upper Main Zone is one of a number of high grade
gold structures that have so far been intersected within the BCD. In
particular, the Upper Main Zone has demonstrated very strong continuity along
strike and to depth. The BC 29 Series are collared at the same location as the
BC 21, BC 25 and BC 27 Series.
See map, "Drill Plan (BC Series-12Aug08)", on the company website
http://www.goldeaglemines.com/_bin/images/maps.cfm
BC 29-9
-------
BC 29-9 was wedged off the mother hole at a depth of 560.00 metres and
directed upwards and north of the trace of BC29 - 8. The hole was drilled to a
final depth of 1,626.00 metres and intersected several mineralized structures
with visible gold within the Balmer Assemblage between 1,122.80 and 1,612.80
metres, a core length of 490.00 metres.
The hole encountered meta-sedimentary rocks of the Bruce Channel
Assemblage from the wedge to a depth of 638.00 metres. Chloritic altered mafic
volcanic rocks between 638.00 and 679.50 metres marked the transition into the
Balmer Assemblage, followed by serpentinized ultramafic rocks to a depth of
1,113.00 metres. Biotite altered mafic meta-volcanics with ubiquitous weak
disseminated pyrrhotite mineralization dominated between 1,113.00 and 1,393.75
metres.
A strongly sheared carbonate zone between 1,393.75 and 1,404.65 metres
was followed by a heavily altered interval comprising biotite, chlorite and
silicification between 1,416.50 and 1,445.85 metres. This interval was
brecciated throughout, associated with quartz veining, and mineralization
comprising ubiquitous disseminated pyrrhotite and pyrite with patches of
felted arsenopyrite and visible gold.