GEOLOGICAL CHARACTERISTICS AND PROGNOSIS IN THE PERIPHERY OF DACHANG ANTIMONY OREFIELD IN GUIZHOU PROVINCE
JIANG Jie1, LI Wei-feng2
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 layer" is 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.
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.
JIANG Jie, LI Wei-feng. GEOLOGICAL CHARACTERISTICS AND PROGNOSIS IN THE PERIPHERY OF DACHANG ANTIMONY OREFIELD IN GUIZHOU PROVINCE. GEOLOGY AND RESOURCES, 2009, 18(4): 288-291.
2009, Vol. 18 
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