Complete agreement of the post-spinel transition with the 660-km seismic discontinuity

The 660-km seismic discontinuity, which is a significant structure in the Earth’s mantle, is generally interpreted as the post-spinel transition, as indicated by the decomposition of ringwoodite to bridgmanite + ferropericlase. All precise high-pressure and high-temperature experiments nevertheless...

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Detalles Bibliográficos
Autores principales: Ishii, Takayuki, Huang, Rong, Fei, Hongzhan, Koemets, Iuliia, Liu, Zhaodong, Maeda, Fumiya, Yuan, Liang, Wang, Lin, Druzhbin, Dmitry, Yamamoto, Takafumi, Bhat, Shrikant, Farla, Robert, Kawazoe, Takaaki, Tsujino, Noriyoshi, Kulik, Eleonora, Higo, Yuji, Tange, Yoshinori, Katsura, Tomoo
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/PMC5910398/
https://www.ncbi.nlm.nih.gov/pubmed/29679056
http://dx.doi.org/10.1038/s41598-018-24832-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5910398/
https://www.ncbi.nlm.nih.gov/pubmed/29679056
http://dx.doi.org/10.1038/s41598-018-24832-y

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