Mo isotope fractionation during hydrothermal evolution of porphyry Cu systems
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Title
Mo isotope fractionation during hydrothermal evolution of porphyry Cu systems
Authors
Keywords
Mo isotopes, MoS<sub>2</sub>, Porphyry Cu, Isotope fractionation
Journal
MINERALIUM DEPOSITA
Volume 50, Issue 3, Pages 281-291
Publisher
Springer Nature
Online
2014-07-04
DOI
10.1007/s00126-014-0537-0
References
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Note: Only part of the references are listed.- Fluid inclusion evidence for hydrothermal fluid evolution in the Darreh-Zar porphyry copper deposit, Iran
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- The solubility of molybdenum dioxide and trioxide in HCl-bearing water vapour at 350°C and pressures up to 160 bars
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- An experimental study of the solubility of molybdenum in H2O and KCl–H2O solutions from 500°C to 800°C, and 150 to 300MPa
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- (2008) Nader Taghipour et al. RESOURCE GEOLOGY
- Experimental study of the behavior of copper and zinc in a boiling hydrothermal system
- (2007) Hiroki Nagaseki et al. GEOLOGY
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