Subducting volcaniclastic-rich upper crust supplies fluids for shallow megathrust and slow slip

Recurring slow slip along near-trench megathrust faults occurs at many subduction zones, but for unknown reasons, this process is not universal. Fluid overpressures are implicated in encouraging slow slip; however, links between slow slip, fluid content, and hydrogeology remain poorly known in natur...

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Detalles Bibliográficos
Autores principales: Gase, Andrew C., Bangs, Nathan L., Saffer, Demian M., Han, Shuoshuo, Miller, Peter K., Bell, Rebecca E., Arai, Ryuta, Henrys, Stuart A., Kodaira, Shuichi, Davy, Richard, Frahm, Laura, Barker, Daniel H. N.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2023
Materias:
Earth, Environmental, Ecological, and Space Sciences
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10431706/
https://www.ncbi.nlm.nih.gov/pubmed/37585538
http://dx.doi.org/10.1126/sciadv.adh0150

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10431706/
https://www.ncbi.nlm.nih.gov/pubmed/37585538
http://dx.doi.org/10.1126/sciadv.adh0150

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