摘要
后塘乡观音山锑矿位于雪峰弧钨、锑、金低温成矿带之上,又位于龙山-白马山东西向构造与雪峰弧重叠部位。矿区内有二组断层构造线,一组为NW向(F4、F5),一组为EW破碎带(即F1、F2、F3),锑矿脉主要赋存于断层破碎带中;区内出露地层简单,为元古界板溪群;该区岩浆活动频繁,广泛发育中酸性基性-超基性侵入岩和火山岩。
Houtang village Guanyinshan Sb mine locates on the low temperature hydrotherm metallogenic belt of W,Sb,Au, Sb-Au, which is also the junction of Longshan-Baimashan east-west structure and Xuefeng arc. There＇ s two groups fault in this area; one group is north-west（ F4）, another is east-west fracture zone（F1, F2, F3 ） where the main Sb ore vein lies in. The stratum is simple, which formed at mesoproterozoic and sinian period. The intermedi- ate-acidic-basic-ultrabasic intrusion rock and igneous rock developed extensively in the area.
出处
《湖南有色金属》
CAS
2009年第6期6-11,共6页
Hunan Nonferrous Metals
关键词
观音山
锑矿
地质特征
控矿因素
Guanyinshan
Sb mine
geological features
ore-controlling factors
