Vancouver —
Geophysics, as well as reverse-circulation and diamond drilling, will be carried out.
Recently, SRK carried out computer-modelling and field mapping, and relogged drill core. The study found that gold mineralization in the Fromenda Main zone is hosted in a deformed mafic intrusion near the southeastern contact between the intrusion and the metasedimentary sequence. The mafic intrusion, which has seen only limited exploration, is associated with a magnetic high that extends over 1 km.
Targets in this area are centred around discrete strong resistivity lows.
Gold mineralization in the Gemap Kukunapi area is associated with east-west-trending quartz-pyrite-arsenopyrite-chalcopyrite veins. These targets fall into four categories:
– the intersection of east-west structures with major northeast-trending fold/thrust-style deformation;
– saddle-reef and axial planar veins associated with regional northeast-trending fold/thrust belts;
– sheared margins of granitoid bodies intersected by northeast and east-west structures; and
– mafic intrusions in sharp contrast with enveloping metasediments.
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