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Reasons from stress, strain, kinematics, and Mohr-Coulomb failure through stereonet fault-slip analysis, area-balanced cross sections in Move, quartz/calcite paleopiezometry on EBSD-indexed CPO, and geodetic-plus-trench slip-rate estimates while treating heterogeneous-fault paleostress inversion, map-pattern vergence errors, seismic processing artifacts as false faults, and outcrop-face shear-sense bias as first-class failure modes.