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The Pre - cambrian alumino - siliceous slate is the host rock of antimony deposit inHunan.
湖南前寒武系的 硅铝 质板岩是锑矿主要赋矿岩性.
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Banpo antimony deposit is a typical fracture - controlling and hydrothermal fluid filling deposit.
半坡锑矿床是典型的断裂控矿,热液充填型矿床.
Silicified limestone is extensively developed in the Xikuangshan antimony deposit.
锡矿山锑矿硅化灰岩发育广泛.
Xikuangshan antimony deposit was discovered in 1541, when mistaken tin, Gu Ming tin mines.
锡矿山锑矿发现于1541年,当时误以为锡, 故名锡矿山.
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