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- W2364402178 abstract "The Gangdisi metallogenetic belt is one of the important poly-metallic ore-forming belts in Tibet.The tungsten-molybdenum- bismuth poly-metallic ore deposit first found in the Jiagang snowy mountain of Shenzha county in the northern part of the belt is of a new type of deposit different from porphyry-type copper poly-metallic deposit in the southern part of it.Discovery of this deposit is a significant breakthrough in prospecting of endogenetic deposit in North Tibet.This paper for the first time gives a precise Re-Os isotopic dating (model age 21.37±1.35 Ma) of molybdenite in the deposit.The U-Pb isotopic age is 22.22Ma for the ore-control intrusion adamellite.Ore formation of the deposit is somewhat later than development of the rock body.For this the authors argue that the deposit formed in intracontinental extensional environment after continental collision at the middle Himalayan stage when intermediate-acid magma was active,the ore matter was mainly sourced from magma and the deposit is of big quartz vein type.Mineralization of W,Mo,Bi,Cu,Pb,Zn and so on in the snowy mountain Jiagang is the most important ore-forming event at the metallogenetic sub-belt Angzicuo-Bengnazangbu- Jiagang snowy mountain-Serirong in the northern Gangdisi metallogenetic belt." @default.
- W2364402178 created "2016-06-24" @default.
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- W2364402178 date "2006-01-01" @default.
- W2364402178 modified "2023-09-25" @default.
- W2364402178 title "RE-OS ISOTOPIC AGES OF TUNGSTEN-MOLYBDENUM (BISMUTH) POLY-METALLIC ORE DEPOSIT IN THE JIAGANG SNOWY MOUNTAIN,SHENZHA COUNTY,TIBET AND THE IMPLICATIONS" @default.
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