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《JOURNAL OF CHANGCHUN UNIVERSITY OF SCIENCE AND TECHNOLOGY》 2000-02
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SULFUR ISOTOPIC COMPOSITION AND ITS GEOLOGICAL SIGNIFICANCE OF THE CAMBRIAN GOLD DEPOSITS IN WESTERN QINLING,CHINA

LIU Jia_jun 1,ZHENG Ming_hua 2,LIU Jian_ming 3,ZHOU De_an 4 (1.OLOG, Institute of Geochemistry, CAS, Guiyang 550002,China;2.Chengdu University of Technology and Sciences, Chengdu 610059, China;3.The Research Center of Mineral Resources Exploration, C  
The gold deposits in Cambrian silicolite formation of western Qinling mountain are a new unique type of stratabound gold deposit which were discovered in China’s territory. The evidence of sulfur isotopic composition in silicolite formation of the deposits shows that the δ 34 S values vary in a wide range but they are characterized by enrichment in heavy sulfur. It is clear that the sulfur of sedimentary pyrite in ore-forming silicolite formation is meanly derived from sea-water sulfate by bacterium fractionation in a close or half-close basin. From eastern Yaxiang gold occurrence to western La’erma gold deposit the trend of δ 34 S value of sedimentary pyrite is upwards which means the depth of the basin was becoming shallow from east to west. The sulfur isotopic composition of hydrothermal minerals and barite vary in a wide range too. The sulfur of these minerals was derived from a same source and supplied by sedimentary sulfur of Cambrian silicolite formation although they are in different δ 34 S values.
【Fund】: 国家自然科学基金!(49773197);; 中国科学院 1997年度“百人计划”;; 中国科学院地球化学研究所所长基金资助项目
【CateGory Index】: P597.2
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