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Can the Updip Limit of Frictional Locking on Megathrusts Be Detected Geodetically? Quantifying the Effect of Stress Shadows on Near-Trench Coupling
ArticleAbstract: The updip limit of the seismogenic zone of megathrusts is poorly understood. The relative absence ofPalabras claves:fault coupling, interseismic deformation, Nankai Trough, Nepal Main Himalayan Thrust, shallow creep, stress shadowAutores:Bradley K.E., Hill E.M., Hubbard J.A., Lindsey E.O., Mallick R., Rafael V. AlmeidaFuentes:googlescopusSlip rate deficit and earthquake potential on shallow megathrusts
ArticleAbstract: Most destructive tsunamis are caused by seismic slip on the shallow part of offshore megathrusts. ThPalabras claves:Autores:Bradley K.E., Burgmann R., Hill E.M., Hubbard J.A., Lindsey E.O., Mallick R., Moore J.D.P., Rafael V. AlmeidaFuentes:googlescopusStructural Control on Downdip Locking Extent of the Himalayan Megathrust
ArticleAbstract: Geologic reconstructions of the Main Himalayan Thrust in Nepal show a laterally extensive midcrustalPalabras claves:DÚPLEX, fault geometry, fault structure, interseismic deformation, Main Himalayan Thrust, NepalAutores:Bradley K.E., Burgmann R., Hill E.M., Hubbard J.A., Lindsey E.O., Liu Y., Mallick R., Rafael V. Almeida, Tsang L.L.H.Fuentes:googlescopus