Diamond anvil cell study of the transformation mechanism from the olivine to spinel phase in Co2SiO4, Ni2SiO4, and Mg2GeO4-Reference-Cited by-同舟云学术

Diamond anvil cell study of the transformation mechanism from the olivine to spinel phase in Co2SiO4, Ni2SiO4, and Mg2GeO4

Published:1995-09-10 Issue:B9 Volume:100 Page:17715-17723
ISSN:0148-0227
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:J. Geophys. Res.

Author:

Burnley Pamela C.,Bassett William A.,Wu Tzy-chung

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Link

http://www.agu.org/journals/jb/v100/iB09/95JB01578/95JB01578.pdf

Reference28 articles.

1. High-pressure synthesis of a “modified” spinel and some geophysical implications;Akimoto;Phys. Earth Planet. Inter.,1970

2. Olivine to spinel transformation in Mg2SiO4via faulted structures;Boland;Nature,1983

3. The fate of olivine in subdueting slabs: A reconnaissance study;Burnley;Am. Mineral,1995

4. The importance of martensitic-like transformation between olivine and spinel in subducting slabs - New results at extreme over pressures;Burnley;Eos, Trans. AGU,1993

5. Burnley , P. C. The effect of nonhydrostatic stress on the olivine-spinel transformation in Mg 2 GeO 4 1990

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