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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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| Главные авторы: | , , , , , , , , , |
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| Формат: | Artigo |
| Язык: | Inglês |
| Опубликовано: |
National Academy of Sciences
2011
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| Предметы: | |
| Online-ссылка: | 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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