Ore genesis and fluid evolution of the Qiaomaishan Cu–W deposit, in the Middle-Lower Yangtze River Metallogenic Belt: Evidence from in situ analyses of apatite and scheelite

Huasheng Qi,Xiaoyong Yang,Sanming Lu,Cheng Tang,Jingya Cao,Lili Zhao,Jianghong Deng,Chao Sun,Zhuang Zhao,Insung Lee

Ore Geology Reviews（2020）

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摘要

•The F-rich magma was originated from a W-rich mixed source under high fO2.•Early-stage fluids were inherited from the primary granodioritic magmatic fluids.•Late-stage fluids were modified by fluid-rock interactions with host carbonates.

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关键词

Apatite,Scheelite,Sr–S isotopes,Fluid evolution,Qiaomaishan,Middle-Lower Yangtze River Metallogenic Belt

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