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《Geology and Prospecting》 2006-03
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CHARACTERISTICS OF KENDEKEKE Fe-Co MULTI-METAL DEPOSIT IN EAST KUNLUN,QINGHAI PROVNCE

YI You-chang~1,JIAO Ge-jun~2,ZHANG Fen-ying~2(1.Qinghai Bureau of Nonferrous Metals Geology and Mineral Exploration,Xining 810007;2.Institute of Mineral Resources Reconnaissance,Qinghai Bureau of Nonferrous Metals Geology and Mineral Exploration,Xining 810007)  
Kendekeke Fe-Co multi-metal deposit in Qinghai is located in the southwest edge of Qaidam basin and middle parts of Qimantage rear arc rift zone.Orebodies are distributed in the upper Ordovician carbonaceous mud calc-iron-silicate formation of hydrothermal spout sediments,and obviously controlled by strata and structures.Indo-Sinian and Yanshanian dykes are developed.Wallrock alteration assemblages near orebodies are complex and wallrock alteration zonation is not obvious,presenting involving of mutil-hydrothermal fluids in mineralization.It is concluded that Kendekeke Fe-Co multi-metal deposit is belong to hydrothermal spout sediment/transformation type,and constitutes Pb-Zn,Co-Bi-Au,and Fe mineralizing series.
【Fund】: 中国地质调查局项目(编号:200010200122)资助
【CateGory Index】: P618.62
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