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《Resources Survey & Environment》 2010-04
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Geological characteristics and genesis discussion of Jisong Lead deposit in Shannan area,Cona County,Tibet

ZENG Fan-miao1,XIAO Zhi-jian1,WU Xu-ling1,XIONG Hui-liang2,ZHOU Rong-qiu2(1 Institute of Geological Survey of Jiangxi Province,Nanchang 330201,China)(2 Donghui Tibet Mining Industry Co.,Ltd.,Lhasa,Tibet,850000,China)  
Jisong lead deposit in Shannan area,Cona County,Tibet,is located in the south of the crustal block of Lhagoi Kangri continental apron of Himalayan plate,belonging to the Lhagoi Kangri metallogenic belt.The exploration results during the past 3 years show that the ore-forming geological conditions of the deposit are relatively favourable.The NE-trending fault and its secondary faults are the major ore-transmitting and ore-hosting structures.The external contact zone between strongly altered intermediate-basic dykes and carbonaceous slates,especially those silicification and epidotization zones,are conducive to the enrichment of ore bodies,the intensity of wall-rock alteration are closely related to the mineralization intensity.It is suggested that the deposit is a middle-low temperature hydrothermal metasomatic deposit occurred mainly in the silicified fracture zones and shows fine prospects for ore prospecting of the deposit.
【Fund】: 西藏山南错那县吉松铅普查项目(编号:5400000730975)资助
【CateGory Index】: P618.42
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