Finite element analysis of lateral pressure variations in square steel silos considering parametric impacts. [PDF]
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Journal of Geophysical Research: Solid Earth, 2014 The Coulomb stress change has been widely employed to interpret mainshock-mainshock and mainshock-aftershock triggering as well as interactions amongst earthquake faults and volcanoes.
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Onto what planes should Coulomb stress perturbations be resolved? [PDF]
Journal of Geophysical Research, 2005 [1] Coulomb stress maps are produced by computing the tensorial stress perturbation due to an earthquake rupture and resolving this tensor onto planes of a particular orientation. It is often assumed that aftershock fault planes are ‘‘optimally oriented’’
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