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《Geology and Exploration》 2010-05
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A Discussion on Geological Characters,Genesis and Ore-Search Prospect of the Wangzhuang Sb Deposit in Henan Province

YANG Lin1,WANG Hao1,YAN Shi2,ZHANG Wen-bo1(1.No.3 Geology Party,Henan Bureau of Geology and Mineral Resources,Zheng zhou 450016;2.No.6Geology Party,Henan Bureau of Geology and Mineral Resources,Zheng zhou 450016)  
The Wangzhuang antimony deposits in Henan province is located in the Wulichuan-antimony grade V ore belt,northern Qingling subzone of the Qinling fold belt,produced in the metamorphic rocks of the Proterozoic Qinling group,strictly controlled by the NWW trending Shuanhuaishu fault.Base on studies of geologic characteristics,mineral-forming sources,physical and chemical environments of the deposit,we suggest that the mineral material stems mainly from the deep source area,and hydatogenesis mainly comes from the mixed water of magma water and atmospheric precipitation.The ore-forming thermal regime is low to medium temperature.For the first time,we suggest that the Wangzhuang antimony deposit is of hydrothermal type controlled by the fault zone with low-medium temperature.At the same time,from metallogenic regularity research,we point out the direction of ore-search in this area,and forecast that the Shuanghuaishu fault and the adjoining portion with its secondary fault,marble distribution area and the deep subsurface on the side of the mineralized body No.II are the prospective sections.
【Fund】: 河南省地质矿产厅地质勘查及科研项目[豫地字(1991)第507号文]资助
【CateGory Index】: P618.51
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