Seismic anisotropy of the D″ layer induced by (001) deformation of post-perovskite

Crystallographic preferred orientation (CPO) of post-perovskite (Mg,Fe)SiO(3) (pPv) has been believed to be one potential source of the seismic anisotropic layer at the bottom of the lower mantle (D″ layer). However, the natural CPO of pPv remains ambiguous in the D″ layer. Here we have carried out...

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Detalles Bibliográficos
Autores principales: Wu, Xiang, Lin, Jung-Fu, Kaercher, Pamela, Mao, Zhu, Liu, Jin, Wenk, Hans-Rudolf, Prakapenka, Vitali B.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5501973/
https://www.ncbi.nlm.nih.gov/pubmed/28416793
http://dx.doi.org/10.1038/ncomms14669

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5501973/
https://www.ncbi.nlm.nih.gov/pubmed/28416793
http://dx.doi.org/10.1038/ncomms14669

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