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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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| Pubblicato in: | Nat Commun |
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| Autori principali: | , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2019
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| Soggetti: | |
| Accesso online: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6318329/ https://ncbi.nlm.nih.gov/pubmed/30604751 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-07874-8 |
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