Phase transition processes of olivine in the shocked Martian meteorite Tissint: Clues to origin of ringwoodite-, bridgmanite- and magnesiowüstite-bearing assemblages-Reference-Cited by-同舟云学术

Phase transition processes of olivine in the shocked Martian meteorite Tissint: Clues to origin of ringwoodite-, bridgmanite- and magnesiowüstite-bearing assemblages

Published:2016-10 Issue: Volume:259 Page:18-28
ISSN:0031-9201
Container-title:Physics of the Earth and Planetary Interiors
language:en
Short-container-title:Physics of the Earth and Planetary Interiors

Author:

Miyahara Masaaki,Ohtani Eiji,El Goresy Ahmed,Ozawa Shin,Gillet Philippe

Publisher

Elsevier BV

Subject

Space and Planetary Science,Physics and Astronomy (miscellaneous),Geophysics,Astronomy and Astrophysics

Reference61 articles.

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3. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1−x)Al3+xSi3−xO11] in shocked Martian meteorites;Beck;Earth Planet. Sci. Lett.,2004

4. Ringwoodite, natural (Mg,Fe)2SiO4 spinel in the Tenham meteorite;Binns;Nature,1969

5. Chondritic meteorites;Brearley,1998

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