Stability analysis of creeping faults: the role of chemical decomposition of minerals - Archive ouverte HAL
Communication Dans Un Congrès Année : 2011

Stability analysis of creeping faults: the role of chemical decomposition of minerals

Jean Sulem
Nicolas Brantut
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Résumé

The stability of creeping faults is studied under the effect of shear heating, pore fluid pressurization and mineral decomposition. Such reactions enhance the pore fluid pressurization because they release fluid, but they limit the temperature rise because they are endothermic. The stability of stationary slip is investigated by performing a linear perturbation analysis. It is shown that chemical reactions change a stable behaviour into an unstable one when the pore pressure effect is larger than the endothermic effect. It is shown that the opposite effect can also be observed when the dehydration reactions can trigger an arrest of the fault. Mineral decomposition can thus strongly modify the nucleation of seismic slip.
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Dates et versions

hal-00692413 , version 1 (30-04-2012)

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Jean Sulem, Nicolas Brantut. Stability analysis of creeping faults: the role of chemical decomposition of minerals. 9th International Workshop on Bifurcation and Degradation in Geomaterials, May 2011, Porquerolles, France. pp.101-107, ⟨10.1007/978-94-007-1421_2⟩. ⟨hal-00692413⟩
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