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《Earth Science Frontiers》 2004-01
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REGIONAL METALLOGENIC CHARACTERISTICS IN PROTEROZOIC CHAERTAISHAN GROUP,INNER MONGOLIA

SHENG Cun-li~(1,2), WANG Shou-guang~(1,2), SU Xin-xu~2, MA Run~2 (1.Key Laboratory of Lithospheric Tectonics and Lithoprobing Technology, China University of Geosciences, Ministry of Education, Beijing 100083, China; 2.Geological Survey Institute of Inner Mongolia, Hohhot 010020, China)  
The Proterozoic Cha'ertaishan group is a very important stratum bearing large and ultra-large scale Cu polymetallic deposits in Langshan-Chaertaishan rift, northern margin of North China. In recent years the Proterozoic Cha'ertaishan group has been found in Bayinnuo area, western Inner Mongolia, by the 1∶50 000 regional survey, and a large scale stratabound micro-fine grain disseminated Au deposit has been found in Agulugouzu group. The deposit is characterized by the thermal water sedimentary type, similar to the Tangyaokou deposit. There is a giant east-west direction Au-Cu-Pb-Zn-S(Fe)-Mn thermal water-sedimentary metallogenic system. The system has Au-ore formation compared with the same kind of deposits abroad, and until now some poor ore deposits have been found in this area. So, there is a giant potential of finding Au and Cu polymetallic ore in this area.
【Fund】: 中国地质调查局地质调查综合研究项目
【CateGory Index】: P618.51
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