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Natural dissociation of olivine to (Mg,Fe)SiO(3) perovskite and magnesiowüstite in a shocked Martian meteorite

We report evidence for the natural dissociation of olivine in a shergottite at high-pressure and high-temperature conditions induced by a dynamic event on Mars. Olivine (Fa(34-41)) adjacent to or entrained in the shock melt vein and melt pockets of Martian meteorite olivine-phyric shergottite Dar al...

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Main Authors: Miyahara, Masaaki, Ohtani, Eiji, Ozawa, Shin, Kimura, Makoto, El Goresy, Ahmed, Sakai, Takeshi, Nagase, Toshiro, Hiraga, Kenji, Hirao, Naohisa, Ohishi, Yasuo
Formato: Artigo
Idioma:Inglês
Publicado: National Academy of Sciences 2011
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Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC3076842/
https://ncbi.nlm.nih.gov/pubmed/21444781
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1016921108
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