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《Geology and Exploration》 2010-04
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Geological Characteristics of Skarn Iron Deposits and Their Mineralization Material Source in the Pingshun Area,Shanxi Province

ZHANG Hai-dong1,LIU Jian-chao1,CHEN Zheng-le2,LIU Shu-wen1,GE Xiao-hong1,CHENG Huan1,ZHANG Xue (1.Resource College of Chang an University,Xi an 710054;2.Institute of Geomechanics,Chinese Academy of Geological Sciences,Beijing 100081)  
The skarn-type iron deposits mainly occur in the contact zone between Yanshan intermediate rocks and Middle Ordovician carbonate rocks in the Ping Shun area of Shanxi Province.The mineralization and alteration show pronounced zoning,and albitization is an important ore-hunting indicator.The 208Pb/204Pb and 207Pb/204Pb 206Pb/204Pb ratios of pyrite are in the ranges of 17.741~18.301 (averaged 17.993) and 15.433~15.551 (averaged 15.495),respectively.The208Pb/204Pb and 207Pb/204Pb 、206Pb/204Pb ration of early intrusive rocks samples are 17.859~18.474,and 15.429~15.431,respectively,while later intrusive rocks samples are 17.959~18.223 (averaged 18.088),and 15.434~15.566 (averaged 15.536),respectively.The Pb isotopic compositions of various kinds of samples from the deposit and the chemical composition of part 7th hole’s core samples in Beiluoxia show that the ore material of megnetite originated from intermediate intrusive rocks of the middle stage as well as ultramafic-mafic intrusive rocks of the early stage.Ultramafic-mafic intrusive rocks are assimilated by intermediate rocks,leading to lots of iron entering the suldenite of late stage.The later sodic alteration caused iron precipitation and then formation of magnetite,which served as the material source for mineralization indirectly.
【Fund】: 全国危机矿山项目(编号:200614004) (编号:200899500)资助
【CateGory Index】: P618.31
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