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《Bulletin of Mineralogy,Petrology and Geochemistry》 2013-03
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Characteristics and Geological Significance of C、O Isotopes of Calcite in the Yindonggou Pb-Zn-Ag Deposit,North Neixiang,Henan Province

XIANG Shi-hong1,2,XUE Chun-ji1,CAO Ji-hu2, ZHANG Xu2,LI Yong-feng2,LI Bing-qi2 1.State Key Laboratory of Geological Processes and Mineral Resources,School of Earth Sciences, China University of Geosciences,Beijing 100083,China 2.Bureau of Non-ferrous Metals Geological and Mineral Resources,Zhengzhou 450016,China  
The large Ag-Pb-Zn deposit in the northern Neixiang County,Henan Province,is found in the Erlangping Terrain,which is on the north side of the Zhu Xia fault in the North Qinling orogenic belt,and formed in deterioration volcano-sedimentary of the back-arc environment during the late Proterozoic-early Paleozoic.About 100 mineral veins were found as filling fault structures of the vertical orogenic belt or presenting layered and bedded single veins.We select calcite samples of Y1,Y6,Y10 and Z2 to test their C、O isotope.The results show that δ13C ranges from-5.45‰~-2.19‰ and δ18O ranges from 10.03‰~14.50‰,the C、O isotope of CO2 in ore fluid δ13C∑C ranges from 0.06‰~1.42‰,indicating that sulfur is mainly from the underthrusted slab metamorphically devolatilized when the Qinling Group underthrusted northward beneath the Erlangping Terrane along the Zhu-Xia fault.
【Fund】: 地质过程与矿产资源国家重点实验室科学基金资助项目(GPMR0 936);; 河南省科技发展计划项目(2010-021);; 河南省有色金属地质矿产局科技创新项目(ysdk2010-6)
【CateGory Index】: P597
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