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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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| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
2020
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| Témata: | |
| On-line přístup: | 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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