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Showing 1 to 4 of 4 for “"restraining bend"”.

  1. Geologic mapping and zircon (U-Th)/He thermochronology of the Avawatz Mountains, California; Implications for the eastern terminus of the Garlock fault

    … of the Garlock fault, orwithin a transpressional restraining bend along the SDVF. Here we present detailed geologic mapping, structural analysis, and low-temperature thermochronology data to test these proposed structural and evolutionary models and to resolve the timing and kinematics of …

    unr Repository record for Geologic mapping and zircon (U-Th)/He thermochronology of the Avawatz Mountains, California; Implications for the eastern terminus of the Garlock fault (opens in a new tab)

  2. Evolution of Deformation Along Restraining Bends Based on Case Studies of Different Scale and Complexity

    … crustal pop-ups, fault duplex structures, restraining bends, and flower structures. Depending on the plate velocity, plate obliquity, crustal rheology, length-scale, and climate, the evolution of faulting into translational and vertical strain can range in complexity and fault slip …

    vt Repository record for Evolution of Deformation Along Restraining Bends Based on Case Studies of Different Scale and Complexity (opens in a new tab)

  3. SEISMIC VELOCITY, RADIAL ANISOTROPY IN THE CRUST AND UPPER MANTLE OF NORTHEASTERN TIBETAN PLATEAU FROM SURFACE WAVE TOMOGRAPHY

    … at ~120 km depth is imaged right beneath a restraining bend of the Kunlun fault and is probably caused by anomalously high temperature and partial melting resulted from localized asthenosphere upwelling after the delamination of a thick lithosphere root beneath the bend. In the second part …

    houston Repository record for SEISMIC VELOCITY, RADIAL ANISOTROPY IN THE CRUST AND UPPER MANTLE OF NORTHEASTERN TIBETAN PLATEAU FROM SURFACE WAVE TOMOGRAPHY (opens in a new tab)

  4. Fault Behavior and Kinematic Evolution of the Eastern California Shear Zone

    … the morphology, structure, and controls of restraining bend growth along the numerous faults of the ECSZ via field mapping and numerical deformational modeling. I found that the ECSZ restraining bends are small (kilometer-scale), exhibit high-angle, doubly fault-bound geometries with …

    vt Repository record for Fault Behavior and Kinematic Evolution of the Eastern California Shear Zone (opens in a new tab)