Modeling the Holocene slip history of the Wasatch fault (Utah): Coseismic and postseismic Coulomb stress changes and implications for paleoseismicity and seismic hazard
Author:
Affiliation:
1. Institut für Geologie, Leibniz Universität Hannover, Callinstraße 30, D-30167 Hannover, Germany
2. U.S. Geological Survey, 1711 Illinois Street, Golden, Colorado 80401, USA
Publisher
Geological Society of America
Subject
Geology
Link
https://pubs.geoscienceworld.org/gsa/gsabulletin/article-pdf/131/1-2/43/4604567/43.pdf
Reference80 articles.
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2. Three-dimensional finite-element modelling of coseismic Coulomb stress changes on intra-continental dip-slip faults;Bagge;Tectonophysics,2016
3. Postseismic Coulomb stress changes on intra-continental dip-slip faults due to viscoelastic relaxation in the lower crust and lithospheric mantle: Insights from 3D finite-element modelling;Bagge;International Journal of Earth Sciences,2017
4. Redistribution of dynamic stress during coseismic ruptures: Evidence for fault interaction and earthquake triggering;Belardinelli;Journal of Geophysical Research,1999
5. Viscosity estimates for the crust and upper mantle from patterns of lacustrine shoreline deformation in the eastern Great Basin;Bills;Journal of Geophysical Research,1994
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2. Influence of Fault System Geometry and Slip Rates on the Relative Role of Coseismic and Interseismic Stresses on Earthquake Triggering and Recurrence Variability;Journal of Geophysical Research: Solid Earth;2023-11
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