GOLD DOMINANT PORPHYRY TARGET
The central part of the low resistivity, high conductivity zone known as the T1 target has not been drill tested to date and lies at the center of a large-scale alteration halo measuring 2,000 meters on 2000 meters. The core of the T1 resistivity anomaly measures 500 x 1000 meters at a depth of 900 meters below surface, increasing in size to 1500 x 1500 meters on a 1000 meter vertical profile and remains open at a depth below 1900 meters.
The gold-copper alteration and mineralization defined to date at T1 is interpreted to be related to a sulphide-rich intrusive body at depth that was responsible for the sericite-potassium feldspar (kspar) alteration and sulphide extent fine-grained with gold-copper mineralization. intersected in previous widely spaced drill holes. Seven fringing holes delineated the area defining a 200-500 meter thick tabular zone of phyllic alteration hosting sericite-kspar alteration zones containing 20-160 meter thick gold-copper mineralization grading 0.20 to 0.84 g/t gold and 0.05-0.11% (500-1100 ppm) copper (see table below). This mineralization is interpreted to have been emplaced by upwelling hydrothermal and epithermal breakouts driven by a large porphyry system directly below.
“The MobileMT survey results are very encouraging and show improved definition of the large T1 gold-dominant porphyry target. With the definition of an area approximately one cubic kilometer (1 km-3) in size, there is more than enough room to encounter considerable tonnage. The next drill program is scheduled for winter 22/23,” says
TREND OF LOW RESISTIVITY AT FIVE KM
The T1 target is one of three distinct low resistivity, high conductivity MobileMT targets defined over a strike length of five kilometers along a prominent north/south trending inferred regional fault. This trend remains open in both directions on the Orestone claims. The low resistivity target T1 coincides with strong induced polarization (IP) chargeability highs and magnetic lows. The other two low resistivity targets along the trend coincide with magnetic lows, but no IPs have been conducted in these areas.
Neither the
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