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The post-stishovite phase transition in hydrous alumina-bearing SiO(2) in the lower mantle of the earth
Silica is the most abundant oxide component in the Earth mantle by weight, and stishovite, the rutile-structured (P4(2)/mnm) high-pressure phase with silica in six coordination by oxygen, is one of the main constituents of the basaltic layer of subducting slabs. It may also be present as a free phas...
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| 主要な著者: | , , , , , , , , , , , , |
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| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
National Academy of Sciences
2007
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1959425/ https://ncbi.nlm.nih.gov/pubmed/17686973 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0706113104 |
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