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Pressure-induced structural change in MgSiO(3) glass at pressures near the Earth’s core–mantle boundary
Knowledge of the structure and properties of silicate magma under extreme pressure plays an important role in understanding the nature and evolution of Earth’s deep interior. Here we report the structure of MgSiO(3) glass, considered an analog of silicate melts, up to 111 GPa. The first (r1) and sec...
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| Publicat a: | Proc Natl Acad Sci U S A |
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| Autors principals: | , , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5828608/ https://ncbi.nlm.nih.gov/pubmed/29432162 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1716748115 |
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