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Re-Os Dating of Molybdenite from Tongchanggou Mo-Polymetallic Deposit in Northwest Yunnan and Its Metallogenic Environment
详细信息   
摘要

The Tongchanggou Mo-polymetallic deposit lies in the western margin depression belt of the Yangtze landmass and is adjacent to Yidun island arc and Garze-Litang suture zone. The ore deposit is a large-size or even a superlarge deposit. Re-Os isotopic dating technique was applied, and six molybdenite samples were analyzed for Re-Os isotopic compositions, and the model ages obtained are from82.34±1.28 to88.27±1.23 Ma,  with the isochron age being85±10 Ma. The result suggests that Mo mineralization occurred in Yanshanian period, during which Zhongza block and Yangtze landmass collided intensively and gradually turned into post-collision stage.

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