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Synthesis of inverse ringwoodite sheds light on the subduction history of Tibetan ophiolites
Tibetan ophiolites are shallow mantle material and crustal slabs that were subducted as deep as the mantle transition zone, a conclusion supported by the discovery of high-pressure phases like inverse ringwoodite in these sequences. Ringwoodite, Mg(2)SiO(4), exhibits the normal spinel structure, wit...
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| 出版年: | Sci Rep |
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| 主要な著者: | , , , , , |
| フォーマット: | Artigo |
| 言語: | Inglês |
| 出版事項: |
Nature Publishing Group UK
2018
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| 主題: | |
| オンライン･アクセス: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5882966/ https://ncbi.nlm.nih.gov/pubmed/29615696 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-23790-9 |
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