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

Singh, Sarva Jit ; Kumari, Gulshan ; Singh, Mahabir (2000) Postseismic deformation of a layered half-space due to a very long dip-slip fault Acta Geophysica Polonica, 48 (1). pp. 69-77. ISSN 0001-5725

Full text not available from this repository.

Official URL: http://agp.igf.edu.pl/

Abstract

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.

Item Type:Article
Source:Copyright of this article belongs to Geophysics, Polish Academy of Sciences.
Keywords:Dip-slip; Layered Half-space; Long Fault; Postseismic Deformation; Relaxed Rigidity
ID Code:94002
Deposited On:02 Jul 2012 04:44
Last Modified:02 Jul 2012 04:44

Repository Staff Only: item control page