Effect of water on olivine-wadsleyite phase boundary in the (Mg, Fe)2SiO4system-Reference-Cited by-同舟云学术

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Effect of water on olivine-wadsleyite phase boundary in the (Mg, Fe)2SiO4system

Published:2002-09 Issue:18 Volume:29 Page:22-1-22-4
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Chen Jiuhua¹,Inoue Toru²,Yurimoto H.³,Weidner Donald J.⁴

Affiliation:

1. Center for High Pressure Research; State University of New York; Stony Brook NY USA

2. Department of Earth Sciences; Ehime University; Matsuyama Japan

3. Earth and Planetary Sciences; Tokyo Institute of Technology; Tokyo Japan

4. Center for High Pressure Research and Department of Geosciences; State University of New York; Stony Brook NY USA

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference26 articles.

1. Olivine-modified spinel-spinel transitions in the system Mg2SiO4-Fe2SiO4: Calorimetric measurements, thermochemical calculation, and geophysical application;Akaogi;J. Geophys. Res,1989

2. Water in earth's mantle: The role of nominally anhydrous minerals;Bell;Science,1992

3. Sharpness of upper mantle discontinuities determined from high-frequency reflections;Benz;Nature,1993

4. Close in ScS and sScS reverberations from the 9 June 1994 Bolivian earthquake;Clarke;Geophys. Res. Lett.,1995

5. Seismic velocities in mantle minerals and the mineralogy of the Earth as determined from seismic profiles;Duffy;J. Geophys. Res.,1989

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