Buoyant hydrous mantle plume from the mantle transition zone

Magmatism at some intraplate volcanoes and large igneous provinces (LIPs) in continental areas may originate from hydrous mantle upwelling (i.e. a plume) from the mantle transition zone (MTZ) at 410–660 km depths in the Earth’s deep interior. However, the ultimate origin of the magmatism, i.e. why m...

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Detalles Bibliográficos
Autores principales: Kuritani, Takeshi, Xia, Qun-Ke, Kimura, Jun-Ichi, Liu, Jia, Shimizu, Kenji, Ushikubo, Takayuki, Zhao, Dapeng, Nakagawa, Mitsuhiro, Yoshimura, Shumpei
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6484022/
https://www.ncbi.nlm.nih.gov/pubmed/31024064
http://dx.doi.org/10.1038/s41598-019-43103-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6484022/
https://www.ncbi.nlm.nih.gov/pubmed/31024064
http://dx.doi.org/10.1038/s41598-019-43103-y

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