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《Geology of Anhui》 2001-02
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H,O ISOTOPE GEOCHEMISTRY AND TRANSPORT-REACTION DYNAMIC PROCESSES OF ORE-FORMING FLUID FOR Cu,Au DEPOSITS IN THE YUESHAN OREFIELD,ANHUI PROVINCE

ZHOU Tao-fa,YUE Shu-cang ,YUAN Feng( Department of Resources and Environment Science,Hefei University of Technology ,Hefei 230009,China)  
H,O isotope geochemistry and transport reaction dynamic processes of ore forming fluid for Cu,Au deposits in the Yueshan orefield,Anhui province have been investigated and discussed.It is concluded that the ore forming fluid of the two types of Cu,Au deposits ,the skarn type and the vein hydrothermal ones was magmatic water with a complex evolutional history with some input of meteoric water.The ore forming solutions of the major mineralization stages of ore deposits were magmatic water predominant,and the two types of deposits are the products of comagmatic hydrothermal system that evolved in different geological and geochemical environments.They were formed from a series of complex transport reaction dynamic processes such as the equitemperature transport reaction processes and the temperature gradient transport reaction processes of the ore forming fluid.
【Fund】: 国家自然科学基金项目(编号:49802007)
【CateGory Index】: P597.2
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