Relationship Between the Growth Rate of Forsterite Phase Transformation and Its Water Content: Implication for the Depth of Metastable Olivine-Reference-Cited by-同舟云学术

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Relationship Between the Growth Rate of Forsterite Phase Transformation and Its Water Content: Implication for the Depth of Metastable Olivine

Published:2012-03 Issue:2 Volume:55 Page:229-238
ISSN:0898-9591
Container-title:Chinese Journal of Geophysics
language:en
Short-container-title:Chinese J. Geophys.

Author:

WANG Shu-Guang¹,LIU Ya-Jing²,NING Jie-Yuan³

Affiliation:

1. Institute of Earthquake Science; China Earthquake Administration; Beijing; 100036; China

2. Department of Geology and Geophysics; Woods Hole Oceanographic Institution; Woods Hole; MA02543; USA

3. School of Earth and Space Sciences; Peking University; Beijing; 100871; China

Publisher

Wiley

Subject

General Medicine

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/cjg2.1717/fullpdf

Reference30 articles.

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

2. Metastable mantle phase transformations and deep earthquakes in subducting oceanic lithosphere;Kirby;Rev. Geophys.,1996

3. The influence of olivine metastability on the dynamics of subduction;Schelming;Earth Planet. Sci. Lett.,1999

4. Stress dependence of the mechanism of the olivine-spinel transformation;Burnley;Nature,1989

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