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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Detalles Bibliográficos
Autores principales: Bindi, Luca, Griffin, William L., Panero, Wendy R., Sirotkina, Ekaterina, Bobrov, Andrey, Irifune, Tetsuo
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5882966/
https://www.ncbi.nlm.nih.gov/pubmed/29615696
http://dx.doi.org/10.1038/s41598-018-23790-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5882966/
https://www.ncbi.nlm.nih.gov/pubmed/29615696
http://dx.doi.org/10.1038/s41598-018-23790-9

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