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Surface deformation due to shear and tensile faults in a half-space

Bulletin of the Seismological Society of AmericaPublished 1 August 1985
Yoshimitsu Okada
Citations5,168
SJR quartileQ1
SJR score1.09
SNIP1.13

Abstract

Abstract A complete suite of closed analytical expressions is presented for the surface displacements, strains, and tilts due to inclined shear and tensile faults in a half-space for both point and finite rectangular sources. These expressions are particularly compact and free from field singular points which are inherent in the previously stated expressions of certain cases. The expressions derived here represent powerful tools not only for the analysis of static field changes associated with earthquake occurrence but also for the modeling of deformation fields arising from fluid-driven crack sources.

Keywords

Earth and Planetary Sciences