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Experimental evidence for silica-enriched Earth’s lower mantle with ferrous iron dominant bridgmanite
Determination of the chemical composition of the Earth’s mantle is of prime importance to understand the evolution, dynamics, and origin of the Earth. However, there is a lack of experimental data on sound velocity of iron-bearing Bridgmanite (Brd) under relevant high-pressure conditions of the whol...
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| 出版年: | Proc Natl Acad Sci U S A |
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| 主要な著者: | , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2020
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC7668101/ https://ncbi.nlm.nih.gov/pubmed/33093206 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1917096117 |
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