Hydrogen partitioning between nominally anhydrous upper mantle minerals and melt between 3 and 5 GPa and applications to hydrous peridotite partial melting-Reference-Cited by-同舟云学术

Hydrogen partitioning between nominally anhydrous upper mantle minerals and melt between 3 and 5 GPa and applications to hydrous peridotite partial melting

Published:2009-05 Issue:1-2 Volume:262 Page:42-56
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Tenner Travis J.,Hirschmann Marc M.,Withers Anthony C.,Hervig Richard L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference59 articles.

1. The influence of pressure, mineral composition and water on trace element partitioning between clinopyroxene, amphibole and basanitic melts;Adam;European Journal of Mineralogy,2003

2. Static compression of hydrous silicate melt and the effect of water on planetary differentiation;Agee;Earth and Planetary Science Letters,2008

3. A hydrous melting and fractionation model for mid-ocean ridge basalts: application to the Mid-Atlantic Ridge near the Azores;Asimow;Geochemistry Geophysics Geosystems,2004

4. Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts;Aubaud;Geophysical Research Letters,2004

5. Intercalibration of FTIR and SIMS for hydrogen measurements in glasses and nominally anhydrous minerals;Aubaud;American Mineralogist,2007

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