Within the intrusion, the mineralized zone is variably silicic, chloritic, and contains variable concentrations of pyrite, arsenopyrite and gold. The rocks are very fractured and sometimes very brecciated. The attitude of a dominant fracture and tectonic fabric cannot at this time be determined with certainty but is interpreted as parallel to the footwall contact of the intrusion. The width of the mineralized zone in the intrusion and the gold distribution are illustrated on the sections and in the drill logs.Within the footwall rocks, the mineralized zone consists of variably silicic, sericitic, and brecciated rocks with variable concentrations of pyrite, arsenopyrite and gold. A planar fabric of sericite and quartz-rich bands is prominent and also interpreted as parallel to the intrusion-footwall contact.
Northquest Ltd. Announces Additional Drilling Results From The Pistol Bay Gold Project, Nunavut, Canada
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