Water in Hawaiian peridotite minerals: A case for a dry metasomatized oceanic mantle lithosphere
Author:
Affiliation:
1. Jacobs, NASA Johnson Space Center; Houston Texas USA
2. Department of Earth and Ocean Sciences; University of South Carolina; Columbia South Carolina USA
Funder
AHP: NSF
MB: NSF
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Reference183 articles.
1. The importance of water to oceanic mantle melting regimes;Asimow;Nature,2003
2. The significance of multiple saturation points in the context of polybaric near-fractional melting;Asimow;J. Petrol.,2004
3. Calculation of peridotite partial melting from thermodynamic models of minerals and melts, IV: Adiabatic decompression and the composition and mean properties of mid-ocean ridge basalts;Asimow;J. Petrol.,2001
4. A hydrous melting and fractionation model for mid-ocean ridge basalts: Application to the mid-Atlantic ridge near the Azores;Asimow;Geochem. Geophys. Geosyst.,2004
5. Hydrogen partition coefficients between nominally anhydrous minerals and basaltic melts;Aubaud;Geophys. Res. Lett.,2004
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