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《Sichuan Nonferrous Metals》 2011-02
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Analysis on geological characteristics and ore-forming processes of copper deposit of Shesuo in Tibet autonomous region

SUN Jiandong,SUN Yan,ZHANG Lin,ZHAO Han,CHENG Chaojie,ZHOU Liqin(Chengdu University of Technology,Chengdu 610059,Sichuan)  
Shesuo copper bed is located in the AngLonggang Day-Bangor degradation arc.The orebody is lies among the limestone,marble and quartz flash long rocks and granodiorite contact belt and surrounding rock of the first litho logic section of the lower cretaceous Langshan group,Showing as nervation and lenticular shapes,lay-like structures and irregular exhibition cloth,it is distributed discontinuously in Skarn internal and external contact belt and confining rock fracture zone and is classified as 3 copper bodies of I,Ⅱ,Ⅲ and 14 copper mineralization bodies.According to the mineral composition and interwoven relationship,the ore-forming process is divided into two metallogenic epochs and five mineralization stages,The bed resulted from skarn type copper deposits with an ore-forming age of 116Ma,which belongs to the late Yanshan Period.
【CateGory Index】: P618.41
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