Origin and evolution of ore-forming fluids of the Larong W-(Mo) deposit, eastern Tibet: Constraints from fluid inclusions, H-O isotopes, and scheelite geochemistry

Jun Liu,Wenchang Li,Xiangping Zhu,Chao Li,Qing Zhou,Fucheng Yang

Ore Geology Reviews（2020）

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摘要

•The primary ore-forming fluids of the Larong porphyry W-(Mo) deposit are of magmatic origin.•Fluid-rock interaction and CO2 loss are the key factors for the mineralization of W and Mo.•Decomposition of plagioclase might provide abundant Ca2+ for the precipitation of scheelite.

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关键词

Larong W-(Mo) deposit,Fluid inclusions,H-O isotopes,Scheelite geochemistry,Continental collision setting,Eastern Tibet

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