Cargando…
Diagenetic and shear-induced transitions of frictional strength of carbon-bearing faults and their implications for earthquake rupture dynamics in subduction zones
Subduction-related diagenetic reactions affect fault strength and are thus important for understanding earthquake rupture dynamics in subduction zones. Carbonaceous material (CM) is found worldwide in active plate-boundary and intracontinental faults, yet the effect of its transformation on friction...
Autores principales: | Kaneki, Shunya, Hirono, Tetsuro |
---|---|
Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
|
Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6536680/ https://www.ncbi.nlm.nih.gov/pubmed/31133653 http://dx.doi.org/10.1038/s41598-019-44307-y |
Ejemplares similares
-
Role of Weak Materials in Earthquake Rupture Dynamics
por: Hirono, Tetsuro, et al.
Publicado: (2019) -
Preservation of amorphous ultrafine material: A proposed proxy for slip during recent earthquakes on active faults
por: Hirono, Tetsuro, et al.
Publicado: (2016) -
Cascadia low frequency earthquakes at the base of an overpressured subduction shear zone
por: Calvert, Andrew J., et al.
Publicado: (2020) -
Lithospheric folding by flexural slip in subduction zones as source for reverse fault intraslab earthquakes
por: Romeo, I., et al.
Publicado: (2018) -
Surface faulting earthquake clustering controlled by fault and shear-zone interactions
por: Mildon, Zoë K., et al.
Publicado: (2022)