The holes are targeting an interpreted structure which forms a series of breaks in geophysical features extending toward the LP fault and following the trend of
Geology of Tooth Holes
The rocks encountered in the drill program that have been logged to date range from metasediments in the north, into mafic to intermediate volcanics, and back to metasediments to the south. Strong to moderate shearing is ubiquitous. Quartz, quartz-carbonate, and calcite veins, veinlets and stringers are also ubiquitous, ranging from a few percent in most units and up to 25% in areas of stockwork veining. Alteration is variable, with many units exhibiting moderate to strong alteration. Alteration types observed include sericite, silicification, carbonate, chlorite, and biotite. Pyrite is the dominant mineralization seen in the drill holes, minor chalcopyrite also occurs in all holes, and minor arsenopyrite was noted in some holes.
Pakwash Drill Program
Four holes were drilled on the ice on
The holes provided useful geological information in areas which had never been drilled before and which are largely covered with overburden.
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