Coseismic fault sealing and fluid pressurization during earthquakes

Earthquakes occur because faults weaken with increasing slip and slip rate. Thermal pressurization (TP) of trapped pore fluids is deemed to be a widespread coseismic fault weakening mechanism. Yet, due to technical challenges, experimental evidence of TP is limited. Here, by exploiting a novel exper...

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Detalles Bibliográficos
Autores principales: Yao, Lu, Ma, Shengli, Di Toro, Giulio
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2023
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9995344/
https://www.ncbi.nlm.nih.gov/pubmed/36890136
http://dx.doi.org/10.1038/s41467-023-36839-9

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC9995344/
https://www.ncbi.nlm.nih.gov/pubmed/36890136
http://dx.doi.org/10.1038/s41467-023-36839-9

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