Bimodal seismicity in the Himalaya controlled by fault friction and geometry

There is increasing evidence that the Himalayan seismicity can be bimodal: blind earthquakes (up to Mw ~ 7.8) tend to cluster in the downdip part of the seismogenic zone, whereas infrequent great earthquakes (Mw 8+) propagate up to the Himalayan frontal thrust. To explore the causes of this bimodal...

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Detalles Bibliográficos
Autores principales: Dal Zilio, Luca, van Dinther, Ylona, Gerya, Taras, Avouac, Jean-Philippe
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6318329/
https://www.ncbi.nlm.nih.gov/pubmed/30604751
http://dx.doi.org/10.1038/s41467-018-07874-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6318329/
https://www.ncbi.nlm.nih.gov/pubmed/30604751
http://dx.doi.org/10.1038/s41467-018-07874-8

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