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Science 30 August 1996:
Vol. 273. no. 5279, pp. 1202 - 1204
DOI: 10.1126/science.273.5279.1202

Reports

Postseismic Rebound in Fault Step-Overs Caused by Pore Fluid Flow

Gilles Peltzer, Paul Rosen, Francois Rogez, Ken Hudnut

Near-field strain induced by large crustal earthquakes results in changes in pore fluid pressure that dissipate with time and produce surface deformation. Synthetic aperture radar (SAR) interferometry revealed several centimeters of postseismic uplift in pull-apart structures and subsidence in a compressive jog along the Landers, California, 1992 earthquake surface rupture, with a relaxation time of 270 ± 45 days. Such a postseismic rebound may be explained by the transition of the Poisson's ratio of the deformed volumes of rock from undrained to drained conditions as pore fluid flow allows pore pressure to return to hydrostatic equilibrium.

G. Peltzer, P. Rosen, F. Rogez, Jet Propulsion Laboratory, 4800 Oak Grove Drive, Pasadena, CA 91109, USA.
K. Hudnut, U.S. Geological Survey, Pasadena, CA 91125, USA.



THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
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The structural evolution of dilational stepovers in regional transtensional zones.
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Geological Society, London, Special Publications 290, 433-445
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The Coseismic Displacement Fields for the 1992 Landers and 1999 Hector Mine Earthquakes in California, from Regional GPS Observations.
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Interactions between the Landers and Hector Mine, California, Earthquakes from Space Geodesy, Boundary Element Modeling, and Time-Dependent Friction.
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Transient Stress-Coupling Between the 1992 Landers and 1999 Hector Mine, California, Earthquakes.
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Evidence of Nonlinear Elasticity of the Crust from the Mw7.6 Manyi (Tibet) Earthquake.
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Viscoelastic Flow in the Lower Crust after the 1992 Landers, California, Earthquake.
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Science 282, 1689-1692
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Evidence of Shallow Fault Zone Strengthening After the 1992 M7.5 Landers, California, Earthquake.
Y. Li, J. E. Vidale, K. Aki, F. Xu, and T. Burdette (1998)
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