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- W2356181483 abstract "Tamu-Kalangu lead-zinc-copper ore belt located at the boundary between western Kunlun and the Tarim basin is a large metallogenic belt.With the study of compositions of ore-bearing formations,metallogenic elements,sulfur isotopes,REE compositions and H,O isotopes of fluid inclusions for ore-bearing formations,the deposits in the belt can be divided into the lead-copper(cobalt)deposits of sandstone type and the lead-zinc deposits of carbonate type.They were formed at different stages in the same metallogenic system.The metallogenic element assembles in sandstone type deposits are Cu-Co-Pb-Ag-As(Ni-Zn-Cd),sulfur isotope is rich in light sulfur,and the contents of Ba show the thermal activity in seafloor is delicacy.The metallogenic element assembles in carbonate type deposit are Pb-Zn-Cd-As-Ag-Ba,and the feature of sulfur isotopic distribution shows that the metallogenic material was derived from deoxidation of seawater and seafloor hydrothermal.The lead-zinc deposits of carbonate type should be a main prospecting goal.At same time,the lead-copper deposits of sandstone type and the cobalt in copper-bearing sand-shale should be noticed." @default.
- W2356181483 created "2016-06-24" @default.
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- W2356181483 date "2003-01-01" @default.
- W2356181483 modified "2023-09-24" @default.
- W2356181483 title "CHARACTERITICS OF GEOLOGY AND GEOCHEMISTRY OF ORE-BEARING FORMATION IN TAMU-KALANGU LEAD-ZINC- COPPER ORE BELTS IN WESTERN KUNLUN MOUNTAIN" @default.
- W2356181483 hasPublicationYear "2003" @default.
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