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Link between the Nankai underthrust turbidites and shallow slow earthquakes
Trench sediments such as pelagic clay or terrigenous turbidites have long been invoked to explain the seismogenic behavior of the megathrust fault (i.e., décollement). Recent numerous studies suggest that slow earthquakes may be associated with huge megathrust earthquake; however, controls on the sl...
Autores principales: | Park, Jin-Oh, Jamali Hondori, Ehsan |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2023
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC10333230/ https://www.ncbi.nlm.nih.gov/pubmed/37429888 http://dx.doi.org/10.1038/s41598-023-37474-6 |
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