Silver Spruce Resources Announces Preliminary Mineralogical Results from the Big Easy Gold/Silver Prospect

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Silver Spruce Resources Inc. (TSXV:SSE) announced preliminary mineralogical studies from the Big Easy gold/silver prospect in eastern Newfoundland.

Silver Spruce Resources Inc. (TSXV:SSE) announced preliminary mineralogical studies from the Big Easy gold/silver prospect in eastern Newfoundland.

As quoted in the press release:

Native silver (Ag), electrum (Au/Ag), acanthite (Ag2S) and unidentified silver-sulfide-selenide (Ag-S-Se) minerals are noted, mainly in “ginguro” bands (narrow erratic black bands) in banded silica (quartz) veins. The Ag-S-Se minerals occur as very fine disseminations (2-3 microns) enclosed within pyrite (FeS2), while the native silver, electrum and acanthite are found as discrete polyminerallic grains up to 30 microns in size, averaging 10-15 microns. A sample of core from the brecciated, gold/silver rich section in DDH BE-11-3 showed one 200 micron grain of pyrite with native Ag, electrum and acanthite in fractures, which is different from numerous smaller pyrite grains in the same polished section – indicating that it may have been re-emplaced from another zone deeper in the system during the periodic re-activation of the boiling / hot spring system. The native Ag-electrum-acanthite mineral assemblage is also associated with well preserved boiling textures (bladed features – quartz after calcite) as shown in a sample from DDH BE-12-10.

Silver Spruce’s  President and CEO, Peter Dimmell, said:

The mineral assemblages and vein textures are characteristic of an epithermal, low sulphidation, gold/silver system, like many others world-wide, especially Nevada (Sleeper, Round Mountain) and Japan (Hishikari), where silver selenide minerals are found. The brecciated zone in DDH BE-11-3, with the isolated grain showing different characteristics from the rest of the grains may indicate better potential for Bonanza grades, typical of these systems, at depth.

To view the whole press release, click here. 

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