Abstract
— This paper regards the on-fault displacement field generated by an earthquake on its own fault plane, with special attention to the tangential displacement vector. It is the continuation and the completion of a previous paper (Armigliato et al., 2003) concerning the analysis of the normal on-fault displacement component. It is here recognised that in addition to the discontinuous shear displacement, which is the main contribution to the seismic dislocation on the fault, there is a tangential displacement contribution that is continuous across the fault. The continuous tangential displacement is exclusively produced by the presence of the free earth's surface. The tangential displacement vector has non-vanishing components in both directions, parallel as well as perpendicular to the imposed uniform shear slip, the first being predominant on the second. We perform a set of computations aimed at evaluating the dependence of the tangential displacement magn itude on the relevant fault parameters for basic cases of rectangular faults embedded in a homogeneous half-space.
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(Received April 24, 2001, accepted March 15, 2002)
Corresponding author: Stefano Tinti, Università di Bologna, Dipartimento di Fisica, Settore di Geofisica, Viale Berti Pichat, 8, I-40127 Bologna, Italy. E-mail: steve@ibogfs.df.unibo.it
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Armigliato, A., Tinti, S. & Manucci, A. Self-induced Deformation on the Fault Plane During an Earthquake Part II: Continuous Tangential Displacements. Pure appl. geophys. 160, 1679–1693 (2003). https://doi.org/10.1007/s00024-003-2374-4
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DOI: https://doi.org/10.1007/s00024-003-2374-4