Mantle-derived helium released through the Japan trench bend-faults

Plate bending-related normal faults (i.e. bend-faults) develop at the outer trench-slope of the oceanic plate incoming into the subduction zone. Numerous geophysical studies and numerical simulations suggest that bend-faults play a key role by providing pathways for seawater to flow into the oceanic...

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Detalles Bibliográficos
Autores principales: Park, Jin-Oh, Takahata, Naoto, Jamali Hondori, Ehsan, Yamaguchi, Asuka, Kagoshima, Takanori, Tsuru, Tetsuro, Fujie, Gou, Sun, Yue, Ashi, Juichiro, Yamano, Makoto, Sano, Yuji
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8203651/
https://www.ncbi.nlm.nih.gov/pubmed/34127710
http://dx.doi.org/10.1038/s41598-021-91523-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8203651/
https://www.ncbi.nlm.nih.gov/pubmed/34127710
http://dx.doi.org/10.1038/s41598-021-91523-6

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