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Possible lateral stress interactions in a sequence of large interplate thrust earthquakes on the subducting Cocos and Rivera plates

Large interplate earthquakes in the Mexican subduction zone may cluster in space and time. This clustering could be due to stress interactions between large events. We investigate this possibility by calculating the coseismic Coulomb failure stress change due to seven large thrust earthquakes (Mw>...

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Vydáno v:Geofísica Internacional
Hlavní autoři: Miguel A. Santoyo, Takeshi Mikumo, Carlos Mendoza
Médium: Artigo
Jazyk:Inglês
Vydáno: Universidad Nacional Autónoma de México 2007
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On-line přístup:https://www.redalyc.org/articulo.oa?id=56846401
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