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《Conributions To Geology and Mineral Resources Research》 2000-04
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GEOCHEMICAL CHARACTERISTICS OF REGIONAL PALEOFLUID OF CENTRAL HUNAN

LU Xin wei 1,MA Dong sheng 2,WANG Wu yi 1 (1.Institute of Geography,Chinese Academy of Sciences,Beijing 100101; 2.State Key Laboratory for Research of Mineral Deposits,Nanjing University,Nanjing 210093,China)  
Ore forming fluid evolved from regional fluid.Regional fluid leaches source bed or ore bearing formation and forms ore forming fluid.So the research on regional fluid for recognizing ore forming fluid and metallogeny not only has theoretical significance,but also has practical value in exploration of ore deposits.Using the method of geochemistry,the paper systematically studies regional paleofluid of central Hunan.The study result shows that the regional paleofluid in central Hunan,originated from meteoric water and is lower in temperature,salinity and weak alkali reduction.The physicochemical property of regional paleofluid is similar to typical ore forming fluid of mineralization epoch of central Hunan(Mesozoic era)and the typical ore forming fluid evolved from it.
【Fund】: 国家自然科学基金!(编号 :497330 12 )资助
【CateGory Index】: P596
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