High-pressure order-disorder transition in Mg\(_2\)SiO\(_4\): Implications for super-Earth mineralog...
High-pressure order-disorder transition in Mg\(_2\)SiO\(_4\): Implications for super-Earth mineralogy
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Ithaca: Cornell University Library, arXiv.org
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English
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Ithaca: Cornell University Library, arXiv.org
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(Mg, Fe)SiO\(_3\) post-perovskite is the highest pressure silicate mineral phase in the Earth's interior. The extreme pressure and temperature conditions inside large extrasolar planets will likely lead to phase transitions beyond pPv. In this work we have explored the high-pressure phase relations in Mg\(_2\)SiO\(_4\) using computations based on d...
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High-pressure order-disorder transition in Mg\(_2\)SiO\(_4\): Implications for super-Earth mineralogy
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TN_cdi_proquest_journals_2771188738
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_journals_2771188738
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2331-8422
DOI
10.48550/arxiv.2301.12701
