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Experimental and theoretical thermal equations of state of MgSiO(3) post-perovskite at multi-megabar pressures
The MgSiO(3) post-perovskite phase is the most abundant silicate phase in a super-Earth’s mantle, although it only exists within the Earth’s lowermost mantle. In this study, we established the thermal equation of state (EoS) of the MgSiO(3) post-perovskite phase, which were determined by using both...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group
2016
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4780068/ https://www.ncbi.nlm.nih.gov/pubmed/26948855 http://dx.doi.org/10.1038/srep22652 |