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Evidence for the stability of ultrahydrous stishovite in Earth’s lower mantle
The distribution and transportation of water in Earth’s interior depends on the stability of water-bearing phases. The transition zone in Earth’s mantle is generally accepted as an important potential water reservoir because its main constituents, wadsleyite and ringwoodite, can incorporate weight p...
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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/PMC6955296/ https://ncbi.nlm.nih.gov/pubmed/31843935 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1914295117 |
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