$Iron isotope fractionation during magmatic-hydrothermal evolution: A case study from the Duolong porphyry Cu-Au deposit, Tibet$
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Iron isotope fractionation during magmatic-hydrothermal evolution: A case study from the Duolong porphyry Cu-Au deposit, Tibet

Ore-forming fluids ultimately precipitate Fe-bearing sulfides and oxides in hydrothermal ore deposits and the Fe isotopic composition of these minerals can trace magmatic-hydrothermal evolution. Here, we report on the Fe isotopic compositions of a suite of hydrothermal minerals (magnetite, pyrite, a...

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Bibliographic Details
Main Authors:	Li, J., Qin, K., Li, G., Evans, Noreen, Huang, F., Zhao, J.
Format:	Journal Article
Published:	Pergamon 2018
Online Access:	http://hdl.handle.net/20.500.11937/69633

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