Surface deformation due to shear and tensile faults in a half-space
- 1 August 1985
- journal article
- Published by Seismological Society of America (SSA) in Bulletin of the Seismological Society of America
- Vol. 75 (4) , 1135-1154
- https://doi.org/10.1785/bssa0750041135
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
This publication has 42 references indexed in Scilit:
- Comparing tiltmeters for crustal deformation measurement – A preliminary reportGeophysical Research Letters, 1984
- Water table effects on the measurement of earth strainTectonophysics, 1984
- On the cause of long-period crustal movementTectonophysics, 1983
- Borehole tilt measurements: Aperiodic crustal tilt in an aseismic areaTectonophysics, 1981
- QUASI-STATIC DEFORMATIONS DUE TO AN INCLINED, RECTANGULAR FAULT IN A VISCOELASTIC HALF-SPACEJournal of Physics of the Earth, 1980
- Static deformation of a laterally inhomogeneous half-space by a two-dimensional strike-slip fault.Journal of Physics of the Earth, 1978
- A strike-slip fault in a laterally inhomogeneous mediumTectonophysics, 1977
- Inversion of geodetic data. I. Mathematical formulation.Journal of Physics of the Earth, 1977
- Deformation of a homogeneous Earth model by finite dislocationsReviews of Geophysics, 1970
- An elastic treatment of ground movement due to mining—III three dimensional problem, transversely isotropic groundJournal of the Mechanics and Physics of Solids, 1962