锡矿山位于湖南省冷水江市,是世界上储量最大的锑矿。为埋藏于泥盆纪石灰岩层中的辉锑矿。西南延伸的背斜岩层中有三层矿床,厚度在2.5至8米之间。矿区露于地表的面积有14 km。北矿山主要产辉锑矿及黄锑矿,后者为硫化物氧化的产物,夹杂在辉锑矿中,南矿山则产辉锑矿,矿石在原地精炼。矿石的主要成分为石英、黄铁矿、辉锑矿与方解石。
锡矿山锑矿硅化灰岩发育广泛。
Silicified limestone is extensively developed in the Xikuangshan antimony deposit.
矿床地质和地球化学特征与我国著名的锡矿山锑矿床具相似性。
The geology of the deposit and the geochemical characteristics are similar to the famous Hsikuanshan antimony deposit in China.
由于燕山晚期岩浆岩的侵入及锡矿山背斜的形成,在背斜两翼产生重力滑动构造。
Because of the magmatite intrusion in Late Yanshan period and the formation of Xikuangshan anticline, gravitation gliding structures are developed at the both wings of the anticline.
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