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《Geochimica》 1998-06
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STABLE ISOTOPE COMPOSITIONS OF MICRO-DISSEMINATED GOLD AND GENETIC DISCUSSION

Liu Jianming;Liu Jiajun; Zheng Minghua; Gu Xuexiang (Mineral Resources Center,Chinese Academy of Sciences,Beijing 100101 )(Institute of Geochemistry,CAS,Guiyang 550002)(Chengdu College of Technology,Chengdu 610059)  
In Southwest China, over hundred ore deposits and occurrences of sedimenthosted micro- disseminated gold were discovered during the last two decades. A systematical research on stable isotope geochemistry of the ores and their hostrocks have been carried out. Very complex and scattered isotopic compositions of oxygen and hydrogen are probably typical for basin derived fluid, because it was derived from fluid- containing sediments of various sources, and it has experienced a long- term isotopic exchange with rocks and organic matters. Carbon and oxygen isotopes of calcite in the ores and their hostrocks indicate that CO2 in was produced mainly by dissolution of marine carbonates. Sulfur isotope composition of sulfides in the ores and their hostrocks exhbits the same characteristics of sedimentation- diagenesis derived H2S. Lead isotope composition shows a source of upper-crust or orogenic belt. It is gold-organic complexes that have probably resulted in gold mobilization from sediments and then transportation in basin fluids.
【Fund】: 中国科学院矿床地球化学开放实验室基金;;国家攀登预选项目!95-预-39
【CateGory Index】: P597
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