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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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| Publicado no: | Sci Rep |
|---|---|
| Main Authors: | , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2018
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| Assuntos: | |
| Acesso em linha: | 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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