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贵州省晴隆大厂锑矿田矿床地质特征及其外围成矿预测
引用本文:蒋杰, 李卫锋. 贵州省晴隆大厂锑矿田矿床地质特征及其外围成矿预测[J]. 地质与资源, 2009, 18(4): 288-291. doi: 10.13686/j.cnki.dzyzy.2009.04.013
作者姓名:蒋杰  李卫锋
作者单位:青海西部稀贵金属有限公司,北京,100012;南京交通职业技术学院,江苏,南京,211188
摘    要:晴隆大厂锑矿田是黔西南地区大型锑矿田,矿田内上二叠统“大厂层”是主要的含矿层位,矿体主要赋存于次生石英岩和黏土岩中.区域性的2条北东向断裂与次级的褶皱和断裂是矿田的主要控矿构造.扭张性断裂和层间断裂发育,是重要的容矿构造.通过总结控矿因素圈定了2个具有找矿前景的靶区.

关 键 词:锑矿床  成矿预测  大厂锑矿田  贵州省
收稿时间:2008-10-07
修稿时间:2008-11-24

GEOLOGICAL CHARACTERISTICS AND PROGNOSIS IN THE PERIPHERY OF DACHANG ANTIMONY OREFIELD IN GUIZHOU PROVINCE
JIANG Jie, LI Wei-feng. GEOLOGICAL CHARACTERISTICS AND PROGNOSIS IN THE PERIPHERY OF DACHANG ANTIMONY OREFIELD IN GUIZHOU PROVINCE[J]. Geology and Resources, 2009, 18(4): 288-291. doi: 10.13686/j.cnki.dzyzy.2009.04.013
Authors:JIANG Jie  LI Wei-feng
Affiliation:1.Qinghai West Rare and Precious Metal Co. Ltd., Beijing 100012, China;; 2.Department of Highway Engineering, Nanjing Institute of Communication Technology, Nanjing 211188, China
Abstract:The large scale Dachang antimony orefield is located in the southwest of Guizhou Province.The Upper Permian Dachang layeris the major ore-bearing layer.The orebodies occur mainly in the top of the strongly altered secondary quartzite and the lower part of clay rock.The regional NE-trending faults and second-order folds and faults are the major ore-controlling structures.The tenso-shear faults and interstratified faults are developed,serving as important host structures.Based on the ore-controlling factors in the orefield,two prospective targets are delineated.
Keywords:ore-forming prognosis  antimony deposit  Dachang antimony orefield  Guizhou Province
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