Bimodal seismicity in the Himalaya controlled by fault friction and geometry
There is increasing evidence that the seismicity of large Himalayan earthquakes can be bimodal, but the underlying mechanisms are unclear. Here, the authors present a model and show that the bimodal seismicity results from a relatively higher friction and a non-planar geometry of the Himalayan megat...
Enregistré dans:
| Auteurs principaux: | Luca Dal Zilio, Ylona van Dinther, Taras Gerya, Jean-Philippe Avouac |
|---|---|
| Format: | article |
| Langue: | EN |
| Publié: |
Nature Portfolio
2019
|
| Sujets: | |
| Accès en ligne: | https://doaj.org/article/56327f7c0c6a4ec987a7a211ba07462f |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
Documents similaires
-
Weak phases production and heat generation control fault friction during seismic slip
par: Hadrien Rattez, et autres
Publié: (2020) -
Control of fault plane geometry on the formation of a normal fault-related anticline: an experimental approach
par: Wei Long, et autres
Publié: (2017) -
Horizontal mantle flow controls subduction dynamics
par: E. Ficini, et autres
Publié: (2017) -
Seismic Microzonation of Tehran based on deterministic seismic hazard analysis and seismic indexes around faults
par: Hamid Saffari, et autres
Publié: (2017) -
Very early identification of a bimodal frictional behavior during the post-seismic phase of the 2015 <i>M</i><sub>w</sub> 8.3 Illapel, Chile, earthquake
par: C. Twardzik, et autres
Publié: (2021)