Major Element and Halogen (F, Cl) Mineral–Melt–Fluid Partitioning in Hydrous Rhyodacitic Melts at Shallow Crustal Conditions
Author:
Affiliation:
1. School of the Environment, Washington State University, Pullman, WA 99164, USA
2. Department of Earth and Planetary Sciences, AMNH, New York, NY 10024, USA
3. School of the Environment, The University of Auckland, Auckland, New Zealand
Funder
National Science Foundation
Publisher
Oxford University Press (OUP)
Subject
Geochemistry and Petrology,Geophysics
Link
http://academic.oup.com/petrology/article-pdf/58/12/2465/24653297/egy011.pdf
Reference97 articles.
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3. Fluid saturation and volatile partitioning between melts and hydrous fluids in crustal magmatic systems: the contribution of experimental measurements and solubility models;Baker;Earth-Science Reviews,2012
4. Behavior of halogens during the degassing of felsic magmas;Balcone-Boissard;Geochemistry, Geophysics, Geosystems,2010
5. The effect of fluorine on the viscosity of dacitic melts;Barber;Geological Society of America, Abstracts with Programs,2007
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