Glass compositions, plume-ridge interaction, and hydrous melting along the Galápagos Spreading Center, 90.5°W to 98°W
Author:
Affiliation:
1. Department of Geology and Geophysics; University of Hawaii; 2525 Correa Road, Honolulu Hawaii 96822 USA
2. Rosenstiel School of Marine and Atmospheric Science; University of Miami; 4600 Rickenbacker Causeway, Miami Florida 33149 USA
Publisher
American Geophysical Union (AGU)
Subject
Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1029/2004GC000709/fullpdf
Reference62 articles.
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2. The importance of water to oceanic melting regimes;Asimow;Nature,2003
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. Hydroxide in olivine: A quantitative determination of the absolute amount and calibration of the IR spectrum;Bell;J. Geophys. Res.,2003
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