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Postseismic deformation of a layered half-space due to a very long dip-slip fault

Singh S., Kumari G., Singh M.

Acta Geophysica Polonica

2000

Vol. 48, nr 1

69-77

The relaxed rigidity method is used for calculating the postseismic deformation of an elastic layer (lithosphere) overlying a yiscoelastic half-space (asthenosphere) caused by a very long dip-slip fault in the layer. The integrals involved are evaluated approximately by replacing the integrand by a finite sum of exponential terms. Detailed numerical results showing the variation of the surface displacements with the epicentral distance for various source depths and for various values of the relaxed rigidity of the half-space are presented graphically.