Water controls the fields of metastable olivine in cold subducting slabs-Reference-Cited by-同舟云学术

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Water controls the fields of metastable olivine in cold subducting slabs

Published:2005-09 Issue:17 Volume:32 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Hosoya Tomofumi¹,Kubo Tomoaki²,Ohtani Eiji¹,Sano Asami¹,Funakoshi Ken-ichi³

Affiliation:

1. Institute of Mineralogy, Petrology and Economic Geology, Graduate School of Science; Tohoku University; Sendai Japan

2. Department of Earth and Planetary Sciences, Faculty of Sciences; Kyushu University; Fukuoka Japan

3. Japan Synchrotron Radiation Research Institute; Hyogo Japan

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference25 articles.

1. Hydroxide in olivine: A quantitative determination of the absolute amount and calibration of the IR spectrum;Bell;J. Geophys. Res.,2003

2. The kinetics of grain boundary nucleated reactions;Cahn;Acta Metall.,1956

3. High-pressure equation of state for NaCl, KCl, and CsCl;Decker;J. Appl. Phys.,1971

4. The 10A phase: A high-pressure expandanle sheet silicate stable during subduction of hydrated lithosphere;Fumagalli;Earth Planet Sci Lett.,2001

5. A new self-organizing mechanism for deep-focus earthquakes;Green;Nature,1989

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