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《Geology and Exploration》 2009-05
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Typomorphic Characteristics of Pyrites in the Huaixi copper-gold deposit,Southeastern Zhejiang Province and its Geological Significance

PENG Li-na1,WEI Junhao1,SUN Xiao-yan2,LI Yan-jun1,YE Ze-fu3(1.Faculty of Earth Resources,China University of Geosciences,Wuhan 430074;2.Lingbao gold Co.,LTD,Lingbao 472532;3.No.11 Geological Team of Zhejiang Burean of Geology and Mineral Resource,Wenzhou 325006)  
Pyrite typomorphic characteristics provide abundant genetic informations and effective mineral prospecting messages at depths in the research of varied deposits.The Huaixi deposit is located in a volcanic terrain between two major faults,the Zhenghe-Dapu and the Changle-Nan'ao deep faults in southeastern Zhejiang province,and is a typical vein-type hydrothermal copper-gold polymetallic deposit.That the ω(Fe)/ω(S+As)of pyrites vary from 0.863 to 0.926 with a mean of 0.881,combined with the depleted Fe and S characteristics suggesting this deposit formed in an environment of shallow-moderate depth and moderate temperature.Ratios of ω(Co)/ω(Ni)is mainly between 1 and 5,which indicate that the magmatic hydrothermal fluids are primary.δ34S values of 8 pyrites are from-2.14‰ to +4.14‰,with a mean of +1.67‰ and range of 6.28‰,which are similar to the magmatic sulfur.Pyrites thermoelectric coefficient,trace element aggregative ratios Φ,content of element As and Cu,trace elements assemblage of As+Ag+Hg,Cu+Pb+Zn and Co+Ni together show the variation law of decreases→increases→decreases from lower to the deeper level.Based on researches of pyrite typomorphic characteristics and combined with previously published data,authors evaluated potential of ore prospecting at depth of the Huaixi Cu-Au deposit.
【Fund】: 教育部创新团队发展计划(编号:IRT0755);; 全国危机矿山接替资源找矿项目(编号:No.2007020047)资助
【CateGory Index】: P618.51
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