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...

Descripción completa

Detalles Bibliográficos
Autores principales: Park, Jin-Oh, Jamali Hondori, Ehsan
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/PMC10333230/
https://www.ncbi.nlm.nih.gov/pubmed/37429888
http://dx.doi.org/10.1038/s41598-023-37474-6

Internet

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

Ejemplares similares