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《Journal of East China Institute of Technology》 2006-01
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The Discover and Genetic Signification of Cu,Pb,Zn Minerals in Ni-Mo Sulfide Layer of the Lower Cambrian,South China

CHEN Yi-ping,PAN Jia-yong,XIA Fei,GUO Guo-lin,CHEN Shao-hua,CAO Shuang-lin,YAN Zhao-bin(Key Laboratory of Nuclear Resources and Environment East China Institute of Technology,Ministry of Education,Nanchang,330013,China)  
South China Yangtze block had firstly attracted the attention of the scholars in China with its well developed submarine hydrothermal exhalative mineralization feature.Low Cambrian black rock series contain several large or super-large barite deposits and Ni-Mo-U-V-enriched layers which were all related to the submarine hydrothermal exhalative genesis in the South China.To furtherly study the cause of formation and the geochemical character of metal and nonmetal deposits which distribute in black shales of South China Yangtze block.It will be great significance for a better understanding of the biologic and the environment evolution of late Sinian to early Cambrian in south China and even the globe.In this paper,several copper,lead and zinc minerals such as chalcopyrite,Tetrahedrite,spharite,galena were detected from the Ni-Mo ore of the Lower Cambrian Ni\\Mo sulfide layers in the South China based on electron microprobe analysis.Copper,lead and zinc minerals occured in nickel and molybdenum ores,which provides the direct evidence that the Ni-Mo layer was formed by submarine hydrothermal exhalative origin.
【Fund】: 国家自然科学基金(40073007 40272080)
【CateGory Index】: P618.41
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