Federica Di MicheleAndriy StyaharDonato PeraJon Bryan MayRoberto AloisioBruno RubinoPierangelo Marcati
Abstract In this paper, we analyse how the combination of fault zone shape and material properties affects the propagation of seismic waves in a two-dimensional domain. We focus on SH wave propagation through several faults with different thicknesses and bending radii, but the theory is easily generalized to the three-dimensional case. We show how the density of energy released is mostly a function of the radius and does not depend on the velocity inside a fault zone.
Robert J. BernhardJoseph R. Milner
Erik BurmanDaniel ElfversonPeter HansboMats G. LarsonKarl Larsson
Sanjay MittalVarun BhattD.N. Srinath
Koji HasegawaMasanori KoshibaMichio Suzuki
Wiem ZaabiYemna BensalemHafedh Trabelsi