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Crystal structure, equation of state, and elasticity of phase H (MgSiO(4)H(2)) at Earth’s lower mantle pressures
Dense hydrous magnesium silicate (DHMS) phases play a crucial role in transporting water in to the Earth’s interior. A newly discovered DHMS, phase H (MgSiO(4)H(2)), is stable at Earth’s lower mantle, i.e., at pressures greater than 30 GPa. Here we report the crystal structure and elasticity of phas...
Wedi'i Gadw mewn:
| Cyhoeddwyd yn: | Sci Rep |
|---|---|
| Prif Awduron: | , |
| Fformat: | Artigo |
| Iaith: | Inglês |
| Cyhoeddwyd: |
Nature Publishing Group
2015
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| Pynciau: | |
| Mynediad Ar-lein: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4616034/ https://ncbi.nlm.nih.gov/pubmed/26493639 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/srep15534 |
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