Abstract：The Shuangsanzi area is located in the southwest end of the Ulanhot-Balinyouqi Cu-polymetal metallogenic belt, where five Ag-Pb-Zn blind orebodies have been found. The orebodies are mainly controlled by the early NEEtrending faults and intensively distributed in and around the pyroclastic breccia. The deposits genetically belong to magmatic hydrothermal type. They occur in a zone of NEE direction, with irregular-shaped geophysical anomaly and rich Ag, Cu, Pb, Zn and As soil anomaly. All of those are important prospecting information and indicators in the area.
赵金才, 闫志强, 迟永坤, 周文光, 董存杰, 杨淑红. 内蒙古克什克腾旗双山子银铅锌矿地质特征及成因[J]. 地质与资源, 2010, 19(2): 134-137,150.
ZHAO Jin-cai, YAN Zhi-qiang, CHI Yong-kun, ZHOU Wen-guang, DONG Cun-jie, YANG Shu-hong. GEOLOGY AND GENESIS OF THE SHUANGSANZI Ag-Pb-Zn DEPOSIT IN INNER MONGOLIA. GEOLOGY AND RESOURCES, 2010, 19(2): 134-137,150.
2010, Vol. 19 
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