The effects of pressure, fO2, fS2 and melt composition on the fluid–melt partitioning of Mo: Implications for the Mo-mineralization potential of upper crustal granitic magmas-Reference-Cited by-同舟云学术

The effects of pressure, fO2, fS2 and melt composition on the fluid–melt partitioning of Mo: Implications for the Mo-mineralization potential of upper crustal granitic magmas

Published:2022-11 Issue: Volume:336 Page:1-14
ISSN:0016-7037
Container-title:Geochimica et Cosmochimica Acta
language:en
Short-container-title:Geochimica et Cosmochimica Acta

Author:

Fang Jing,Audétat Andreas

Funder

China Scholarship Council

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference86 articles.

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2. Source and evolution of molybdenum in the porphyry Mo(–Nb) deposit at Cave Peak, Texas;Audétat;J. Petrol.,2010

3. Compositional evolution and formation conditions of magmas and fluids related to porphyry Mo mineralization at Climax, Colorado;Audétat;J. Petrol.,2015

4. The metal content of magmatic-hydrothermal fluids and its relationship to mineralization potential;Audétat;Econ. Geol.,2019

5. Molybdenite saturation in silicic magmas: Occurrence and petrological implications;Audétat;J. Petrol.,2011

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