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Bulletin of the Seismological Society of America; April 1992; v. 82; no. 2; p. 1018-1040
© 1992 Seismological Society of America
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Internal deformation due to shear and tensile faults in a half-space

YOSHIMITSU OKADA

NATIONAL RESEARCH INSTITUTE FOR EARTH SCIENCE AND DISASTER PREVENTION, TSUKUBA, IBARAKI, 305 Japan

Abstract

A complete set of closed analytical expressions is presented in a unified manner for the internal displacements and strains due to shear and tensile faults in a half-space for both point and finite rectangular sources. These expressions are particularly compact and systematically composed of terms representing deformations in an infinite medium, a term related to surface deformation and that is multiplied by the depth of observation point. Several practical suggestions to avoid mathematical singularities and computational instabilities are also presented. The expressions derived here represent powerful tools both for the observational and theoretical analyses of static field changes associated with earthquake and volcanic phenomena.




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