Stagnant forearc mantle wedge inferred from mapping of shear-wave anisotropy using S-net seafloor seismometers

Shear-wave anisotropy in Earth’s mantle helps constrain the lattice-preferred orientation of anisotropic minerals due to viscous flow. Previous studies at the Japan Trench subduction zone using land-based seismic networks identified strong anisotropy in the mantle wedge, reflecting viscous flow indu...

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Detalles Bibliográficos
Autores principales: Uchida, Naoki, Nakajima, Junichi, Wang, Kelin, Takagi, Ryota, Yoshida, Keisuke, Nakayama, Takashi, Hino, Ryota, Okada, Tomomi, Asano, Youichi
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7655809/
https://www.ncbi.nlm.nih.gov/pubmed/33173070
http://dx.doi.org/10.1038/s41467-020-19541-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7655809/
https://www.ncbi.nlm.nih.gov/pubmed/33173070
http://dx.doi.org/10.1038/s41467-020-19541-y

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