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Ferromagnesian postperovskite silicates in the D″ layer of the Earth
Natural olivine with 12 mol % Fe(2)SiO(4) and synthetic orthopyroxenes with 20% and 40% FeSiO(3) were studied beyond the pressure–temperature conditions of the core–mantle boundary. All samples were found to convert entirely or partially into the CaIrO(3) postperovskite structure, which was recently...
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| Autors principals: | , , , , , , , , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2004
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC528774/ https://ncbi.nlm.nih.gov/pubmed/15520393 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0407135101 |
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