Shock compression response of forsterite above 250 GPa-Reference-Cited by-同舟云学术

Shock compression response of forsterite above 250 GPa

Published:2016-08-05 Issue:8 Volume:2 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Sekine Toshimori¹,Ozaki Norimasa²³,Miyanishi Kohei²,Asaumi Yuto²,Kimura Tomoaki⁴,Albertazzi Bruno²,Sato Yuya²,Sakawa Youichi⁵,Sano Takayoshi⁵,Sugita Seiji⁶^ORCID,Matsui Takafumi⁷,Kodama Ryosuke²³

Affiliation:

1. Department of Earth and Planetary Systems Science, Hiroshima University, Higashi-Hiroshima 739-8526, Japan.

2. Graduate School of Engineering, Osaka University, Suita 565-0871, Japan.

3. Photon Pioneers Center, Osaka University, Suita 565-0871, Japan.

4. Geodynamics Research Center, Ehime University, Matsuyama 790-8577, Japan.

5. Institute of Laser Engineering, Osaka University, Suita 565-0871, Japan.

6. Graduate School of Frontier Sciences, The University of Tokyo, Kashiwa 277-856, Japan.

7. Planetary Exploration Research Center, Chiba Institute of Technology, Narashino 275-0016, Japan.

Abstract

Shocked forsterite above 250 GPa indicates incongruent crystallization of MgO, its phase transition, and remelting.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference44 articles.

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2. Equation of state of forsterite;Ahrens T. J.;J. Geophys. Res.,1971

3. Shock-wave compression of single crystal forsterite;Jackson I.;J. Geophys. Res.,1979

4. S. P. Marsh LASL Shock Hugoniot Data (University Calf. Press Berkeley 1980) 658 pp.

5. Shock compression measurements of single-crystal forsterite in the pressure range 15–93 GPa;Syono Y.;J. Geophys. Res.,1981

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