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Strategies & Market Trends : Dino's Bar & Grill -- Ignore unavailable to you. Want to Upgrade?

To: teevee who wrote (52908)	12/23/2018 7:37:00 AM
From: howestreetbull	Read Replies (1) \| Respond to of 203936

this would then strengthen the authors comparison to the Hishikari deposit ? --------------------------------------------------------------------------------------------------- The Hishikari deposit is composed of more than 125 veins (generally 1 to 3 m thick, to a maximum of 8 m), which strike at between 30 and 70°, distributed within an altered and mineralised corridor with a width of 500 to 1000 m and strike interval of ~3 km, and dip at from 70°NW to 70°SE. The individual veins are 300 to 400 m long, composed of crustiform banded quartz-adularia with subordinate smectite. The top of the vein system is generally >100 m below the surface, straddling the unconformity between the Shimanto Super Group and the mainly Pleistocene Hishikari Group. Some 60% of the ore is in the Cretaceous basement, the remainder being in the andesitic lowermost unit of the Hishikari Group.