Highlights:
JM-22-02 returned 178 m of 0.32% copper equivalent ('CuEq'), including 76 m of 0.52% CuEq and 31 m of 0.68%CuEq, including 10 m of 1.15% CuEq
JM-22-01 returned 155 m of 0.20% CuEq
Mineralized hydrothermal breccia was encountered in both holes
'Jean Marie is a fantastic exploration opportunity for Pacific Empire. Our geologic team believes the results of this drilling program are significant and encountering the mineralized breccia in a 200-metre step-out hole from the historical hole 97-11 demonstrates hydrothermal style porphyry mineralization is open along strike,' commented
JM-22-01 was drilled approximately 100 metres to the west of historical drill hole 97-11 and was drilled to a depth of 400 metres. The hole was collared in Takla Volcanic rocks. Copper mineralization that was observed in the hole consisted of chalcopyrite and bornite finely disseminated in the Takla volcanic andesite and in quartz hematite veinlets. A 13-meter-wide quartz-carbonate breccia zone was intercepted from 163 to 176 metres. Five to ten meter wide dykes of equigranular monzonite cross cut the Takla. Takla volcanic rock was intensely and variably biotitised, with the greatest intensity of alteration close to the contact with the equigranular monzonitic plutonic rocks at 223 meters depth. Chalcopyrite in the Jean Marie intrusive monzonite was found in low angle quartz, hematite veinlets with K-feldspar selvages.
JM-22-02 was drilled a further 100 metres to the northwest of JM22-01. This hole was drilled to a depth of 300 metres. The highest-grade intercept was encountered in from 189 metres to 220 metres, where a 30-metre-wide quartz-carbonate hydrothermal breccia was intersected. This intercept represents a continuation of the high-grade mineralized breccia intercepted 200 metres to the east in hole J97-11. Mineralization in the breccia is found as massive chalcopyrite in the matrix as well as large angular clasts. Takla volcanic rock was variably biotitised, chalcopyrite and bornite was disseminated in the Takla andesitic volcanic rock and in veinlets associated with hematite. The contact with the Jean Marie pluton was intercepted at 220 meters, below the quartz-carbonate breccia. Chalcopyrite in the Jean Marie intrusive monzonite was found in low angle quartz, hematite veinlets with K-feldspar selvages.
About Jean Marie
The Jean Marie property is a copper-molybdenum-silver-gold porphyry prospect located 50 km south of
Drilling in the 1990's returned near surface intercepts of up to 244m of 0.28% copper, 0.007% molybdenum and 1.1 g/t silver, in a broad area located close to the pluton, volcanic contact. Two of the holes intercepted a distinct quartz breccia which returned up to 27 metres of 1.19% copper, and 5.74 g/t silver.
Historical diamond drilling was limited to a maximum depth of 288 metres below surface and mineralization remains unbounded at depth and along strike to the NW and SE. Of the 96 holes drilled on the property since the 1970's 76 are less than 130 metres in depth with numerous short holes that were mineralized over the entire length.
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About Pacific Empire
Pacific Empire is a copper exploration company based in
Contact:
President and Chief Executive Officer
Tel: +1-604-356-6246
E: brad@pemcorp.ca
WEB: www.pemcorp.ca
Neither the
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