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- W2378800765 abstract "Nan Yuela lead zinc ore located in northern Qiangtang massif in Leiwuqi County,Tibet,the layer expose in the mine lot are mainly upper Triassic Jia peila formation(T3 j),and the lithology is sandstone,conglomerate,and mudstone which press from both sides in limestone.This deposit is mainly controlled by stratum,rock mass and fault structure zone.Jia peila formation(T3j)is the Ore formation,the ore body contain in the upper part of(T3 j)which is fragmentation dolomitic limestone.In this paper,by introduce the geological background,diggings features and metallogenic evolution,analyzing the cause of formation,and ore body petrochemistry abnormal in brief.infering the second mineralized zone and deep ore body exploration have considerable prospect." @default.
- W2378800765 created "2016-06-24" @default.
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- W2378800765 date "2013-01-01" @default.
- W2378800765 modified "2023-09-23" @default.
- W2378800765 title "Geological characteristics and prospecting direction of Nan Yuela Lead-zinc Deposit, Leiwuqi County, Tibet" @default.
- W2378800765 hasPublicationYear "2013" @default.
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