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A damage model for the continuum rheology of the upper continental crust
Authors:Donald L Turcotte  Margaret T Glasscoe
Institution:Department of Geology, University of California, One Shields Avenue, Davis, CA 95616, USA
Abstract:In orogenic zones it is often considered appropriate to use a continuum rheology to model the deformation of the upper continental crust. In this paper we derive an applicable rheology utilizing fiber-bundle and continuum-damage models. We show that the results are identical and yield a power relation between stress σ and strain rate of the form σ= ρ−1. We constrain the applicable values of ρ utilizing Omori's law for the decay of aftershocks and conclude that ρ−1 is in the range of 5–15. With this strong nonlinear viscous rheology the behavior of the deforming upper crust approaches that of a perfect-plastic material.
Keywords:Damage mechanics  Damage  Crustal deformation  Aftershocks  Rheology
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