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• W2042663243 abstract "The study examines the influence of depth on the development of steep normal faults above a gently dipping fault which is reactivated in its deeper part and abandoned in its upper part. The isotropic and anisotropic Mohr-Coulomb-Anderson theory is used to determine the ability of any part of a fault to be reactivated by calculating the difference between the stress deviator necessary to induce reactivation and that required to induce fracturing. When linear depth-dependent properties are assumed, it appears that a new normal fault can branch off a gentle pre-existing fault only if the friction coefficient of the latter is much less than that used by Byerlee, and if the ratio (cohesion of fault/cohesion of intact rock) is non-negligible. For a 30° dip fault, the friction coefficient has to be less than 0.35 (friction angle less than 20°). Neither pore fluid pressure nor constant excess fluid pressure affects the above conditions. When the cohesion of the surrounding rocks increases with depth, steep normal faults can branch off Byerlee faults with dips as gentle as 30°. A low shear strength of the lowest part of the preexisting fault also increases the chances of reactivation of the deeper part and abandonment of the upper part." @default.
• W2042663243 created "2016-06-24" @default.
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• W2042663243 date "1992-08-01" @default.
• W2042663243 modified "2023-09-25" @default.
• W2042663243 title "The influence of depth on reactivation in normal faulting" @default.
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• W2042663243 doi "https://doi.org/10.1016/0191-8141(92)90030-z" @default.
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