摘要
固路锑矿床位于晴隆大厂锑矿田中部,支氽向斜与黑山箐背斜夹持部位;矿体严格受地层、岩性、构造、岩相古地理及岩浆岩等因素控制;古地理环境控制了"大厂层"的厚度及其分布,构造控制了锑矿(化)体的分布,有利的岩性(岩相)提供了良好的容矿空间。
Gulu ore deposit lies in the middle of Dachang antimony ore field,the region between Zhitun syncline and Heishanqing anticline.The orebody is strictly controlled by stratum,lithology,structure,environment of ancient geography as well as magmatic rock.The environment of ancient geography dominates the distribution and the thickness of ＂Dachang layer＂.The structure controls the distribution of antimony ore body（antimony mineralization orebody）.The preferential lithology（lithofacies） provides favorable ore-containing space.
出处
《矿产与地质》
2010年第4期294-299,共6页
Mineral Resources and Geology
基金
全国危机矿山接替资源找矿项目(编号:200652096)
西南地区层控型多金属矿床成矿规律总结研究项目(编号:20089943)
国家财政部资补项目(编号:295050028-6)的资助
关键词
锑矿床
矿床地质特征
控矿因素
固路
贵州
antimony deposit
geological characteristic of ore deposit
ore-controlling factors
Gulu
Guizhou
