Spherical versus flat models of coseismic and postseismic deformations
- 10 June 1999
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 104 (B6) , 13115-13134
- https://doi.org/10.1029/1999jb900097
Abstract
No abstract availableKeywords
This publication has 31 references indexed in Scilit:
- Time‐dependent residual deformations associated with the June 9, 1994 Bolivia EarthquakeGeophysical Research Letters, 1997
- Gravitational viscoelastic postseismic relaxation on a layered spherical EarthJournal of Geophysical Research, 1997
- Global displacements caused by point dislocations in a realistic Earth modelJournal of Geophysical Research, 1996
- Stress Triggering of the 1994 M = 6.7 Northridge, California, Earthquake by Its PredecessorsScience, 1994
- Change in Failure Stress on the Southern San Andreas Fault System Caused by the 1992 Magnitude = 7.4 Landers EarthquakeScience, 1992
- Quasi-static deformation due to a dislocation source in a Maxwellian viscoelastic earth model.Journal of Physics of the Earth, 1985
- Preliminary reference Earth modelPhysics of the Earth and Planetary Interiors, 1981
- Vertical displacements from a rectangular fault in layered elastic-gravitational media.Journal of Physics of the Earth, 1981
- Focal process of the great Chilean earthquake May 22, 1960Physics of the Earth and Planetary Interiors, 1974
- Deformation of a homogeneous Earth model by finite dislocationsReviews of Geophysics, 1970