A hydrous melting and fractionation model for mid-ocean ridge basalts: Application to the Mid-Atlantic Ridge near the Azores-Reference-Cited by-同舟云学术

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A hydrous melting and fractionation model for mid-ocean ridge basalts: Application to the Mid-Atlantic Ridge near the Azores

Published:2004-01 Issue:1 Volume:5 Page:n/a-n/a
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Asimow P. D.¹,Dixon J. E.²,Langmuir C. H.³

Affiliation:

1. Division of Geological and Planetary Sciences; California Institute of Technology; Pasadena California 91125 USA

2. Rosenstiel School of Marine and Atmospheric Science, Division of Marine Geology and Geophysics; University of Miami; Miami Florida 33149 USA

3. Lamont-Doherty Earth Observatory; Palisades New York 10964 USA

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference85 articles.

1. Comagmat: A FORTRAN program to model magma differentiation processes;Ariskin;Comp. Geosci.,1993

2. Algorithmic modifications extending MELTS to calculate subsolidus phase relations;Asimow;Am. Mineral.,1998

3. Segment-scale and regional systematics from 33°N to 41°N on the Mid-Atlantic Ridge: Results from the FAZAR Cruise;Asimow;Eos Trans. AGU,1998

4. The importance of water to oceanic mantle melting regimes;Asimow;Nature,2003

5. The effect of pressure-induced solid-solid phase transitions on decompression melting of the mantle;Asimow;Geochim. Cosmochim. Acta,1995

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