Deep Ductile Shear Zone Facilitates Near?Orthogonal Strike?Slip Faulting in a Thin Brittle Lithosphere
نویسندگان
چکیده
Some active fault systems comprise near-orthogonal conjugate strike-slip faults, as highlighted by the 2019 Ridgecrest and 2012 Indian Ocean earthquake sequences. In conventional Mohr-Coulomb failure theory, orthogonal faulting requires a zero frictional coefficient (pressure-insensitive), which is unlikely in brittle lithosphere. The simulations developed here show that faults can form layer inheriting geometry of shear zones nucleated deep ductile (pressure-insensitive) layer. particular, if sufficiently thinner than root, preserved at surface. preservation further facilitated depth-dependent strength Conversely, within are to angles. Our model thus offers possible explanation for reveals significant interactions between structure upper lithosphere their roots.
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ژورنال
عنوان ژورنال: Geophysical Research Letters
سال: 2021
ISSN: ['1944-8007', '0094-8276']
DOI: https://doi.org/10.1029/2020gl090744