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《Journal of Chengdu University of Technology(Science & Technology Edition)》 2011-01
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Source and characteristics of ore-forming fluids in the Mengya'a Pb-Zn deposit,Tibet

WANG Li-qiang1,GU Xue-xiang2,TANG Ju-xing1,WANG Huan1,CHENG Wen-bin2,JING Liang-bing3,XIANG Hao-yu4 1.Institute of Mineral Resources,Chinese Academy of Geological Sciences,Beijing 100037,China;2.School of Earth Sciences and Resources,China University of Geosciences,Beijing 100083,China;3.Beijing Donia Resources Co.Ltd,Beijing 100012,China;4.Sichuan Institute of Nuclear Geology,Chengdu 610061,China  
The paper studies the source and characteristics of the ore-forming fluids in the Mengya'a Pb-Zn deposit of Tibet and identifies the genetic type of deposit by studying the typical deposit of this area.It analyzes the altered limestone in the surrounding area,the carbon and oxygen isotopes of hydrothermal calcite and the hydrogen and oxygen isotopes of quartz formed in different mineralization periods,studies the fluid inclusions petrographically,and measures their temperatures and salinity.The resuct shows that in the early post-mineralization stage,the ore-forming fluids were was mainly in the form of magmatic water,while in the later stage,they were mixed with plentiful meteoric water.In the mineralization period,ore-forming fluids were generally characterized by medium-high temperatures and intermediate-low salinity and there was an apparent temperature-dropping trend from the early to the late ore-forming stage.The formation of the deposit is closely related to magmatism and the deposit is a zinc-lead one under the skarn type.
【Fund】: 国家科技支撑项目(2006BAB01A01);; 中国地质调查局青藏高原专项项目(1212010818089)
【CateGory Index】: P618.4
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