DV22-300 encountered a wide interval of multi-phase veins and breccia, intersecting 19.85m (13.90m true width) averaging 584 g/t Ag, 0.92 %Pb, 0.56% Zn and 0.19 g/t Au, with bonanza grade silver mineralization grading 4,326 g/t Ag, 4.21% Pb, 1.36% Zn and 1.00 g/t Au over 1.60m (1.12m true width) within a sulphide and silver sulphosalt matrix vein breccia in the main veined interval.
'With an increase in vein intensity and silver grades, the Wolf Vein area is emerging as a large system, rivaling our Torbrit Deposit. With an established plunge length of over 500 meters from the historic underground workings, we are continuing to step out along this trend towards the Kitsol Vein, where we recently announced similar, high-grade mineralization over 1,400 meters away. The increasing gold and base metal content, in addition to the silver, is highly encouraging, as well as the significant widths that are potentially amenable to bulk underground mining techniques,' said
The mineralized interval in DV22-300 is a southwesterly step-out along strike and down dip from DV21-273, which returned 17.50m averaging 214 g/t Ag and 0.47% Pb including 1.22 m averaging 1,532 g/t Ag, 0.44 g/t Au, 2.11 % Pb and 1.07% Zn (see Dolly Varden news release,
The Wolf Vein is a steep dipping, high-grade silver vein deposit that is part of the current Mineral Resource Estimate at Dolly Varden's
Results have been received for the first six exploration drill holes testing the Wolf Vein extension. All holes were drilled from the same pad with varying azimuths and dips (see Table 2). These drill holes tested below the Upper Hazelton sediment cap and have encountered a robust, multi-phase vein and breccia mineralizing system that remains wide open along strike to the south and down dip. The associated strong potassic alteration, a key indicator for silver mineralization at the
Mineralization at the Wolf Vein consists of multiple epithermal silica vein and brecciation events along a NE trending, steeply NW dipping zone (Figures 4 and 5). Silver mineralization includes: silver sulphosalts, tennantite, argentite and argentiferous galena hosted in vein and vein breccia mineralization.
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