Carbon-oxygen isotopic geochemistry of the Yangla Cu skarn deposit, SW China: Implications for the source and evolution of hydrothermal fluids

Li-Juan Du,Bo Li,Zhilong Huang,Jiaxi Zhou,Guo-Fu Zou,Zai-Fei Yan

Ore Geology Reviews（2017）

引用 35|浏览2

暂无评分

摘要

•Ore fluids were associated with magmatism in the Yangla mining district.•Carbonate host rocks likely contributed CO2 to the late-sub ore stage ore fluids.•Both CO2 degassing and fluid-rock interaction are the key to the calcite deposition.

查看译文

关键词

Yangla Cu skarn deposit,Hydrothermal calcite,C-O isotopes,Fluid source and evolution,Sanjiang region (SW China)

AI 理解论文

溯源树

样例

生成溯源树，研究论文发展脉络

Chat Paper

正在生成论文摘要