Coulomb pre-stress and fault bends are ignored yet vital factors for earthquake triggering and hazard

Successive locations of individual large earthquakes (M(w) > 5.5) over years to centuries can be difficult to explain with simple Coulomb stress transfer (CST) because it is common for seismicity to circumvent nearest-neighbour along-strike faults where coseismic CST is greatest. We demonstrate t...

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Detalles Bibliográficos
Autores principales: Mildon, Z. K., Roberts, G. P., Faure Walker, J. P., Toda, S.
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/PMC6588554/
https://www.ncbi.nlm.nih.gov/pubmed/31227694
http://dx.doi.org/10.1038/s41467-019-10520-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6588554/
https://www.ncbi.nlm.nih.gov/pubmed/31227694
http://dx.doi.org/10.1038/s41467-019-10520-6

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