Enterayon, Inc. (OTC: ETYN)
Prince George Showing
Enterayon, Inc. announces the Prince George Showing has powerful indicators for precious metals. Read the details below. Analysis indicates that the Prince George Showing quartz vein is mineralized with pyrite, minor chalcopyrite, sphalerite and trace galena.
The Prince George showing is located near the headwaters of the south fork of the Marmot River, 13.5 kilometres southeast of Stewart.
The showing consists of a quartz vein, up to 1.2 metres wide, striking 059 degrees and dipping 65 degrees northwest. The vein is hosted in granodiorite of the Eocene Hyder Pluton, just southwest of the contact with argillite, siltstone and sandstone of the Middle Jurassic Salmon River Formation. The vein contains massive to disseminated pyrite and minor chalcopyrite, galena and sphalerite. Samples of heavily mineralized quartz have assayed up to 66.3 grams per tonne gold and 411 grams per tonne silver (Minister of Mines Annual Report 1921, page 62).
High Grade Showing
The High Grade occurrence is located near the headwaters of the south fork of the Marmot River, 15 kilometres southeast of Stewart. Various gold bearing quartz veins were extensively explored by trenching and tunnelling in this area during the late 1920’s.
The occurrence consists of three veins developed in volcanic breccia and lithic tuff of the Lower Jurassic Unuk River Formation (Hazelton Group) just east of the Eocene Hyder Pluton.
The upper vein strikes 119 to 134 degrees for at least 150 metres, dips 45 to 55 degrees northeast and is 0.6 to 2.7 metres wide. Mineralization consists of stringers and massive lenses of pyrite, galena and arsenopyrite in a quartz-carbonate gangue. A grab sample assayed 7.56 grams per tonne gold (Assessment Report 16652, page 11).
The middle vein, 150 metres southwest of the upper vein, strikes 125 degrees for 100 metres, dips 45 degrees northeast and is up to 2.1 metres wide. The quartz vein is mineralized with pyrite, minor chalcopyrite, sphalerite and trace galena.
The lower vein, 300 metres south of the upper vein, strikes 085 to 089 degrees for 1000 metres, dips 45 to 50 degrees north and is up to 1.0 metre wide. It contains brecciated and silicified wallrock with numerous lenses and veinlets of quartz with pyrite and minor chalcopyrite. A sample of quartz with disseminated pyrite assayed 86.2 grams per tonne gold and 123.0 grams per tonne silver (Minister of Mines Annual Report 1926, page 89).
Link here for the fabulous images of this important geological area: http://www.enterayon.com/horseshoe.html
Gold and silver deposits are the focus of Enterayon’s determination to mine those veins.
Source:
Enterayon, Inc.
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