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Strategies for effective unmanned aerial vehicle use in geological field studies based on cognitive science principles
The effects of pre-stress assumptions on dynamic rupture with complex fault geometry in the San Gorgonio Pass, California, region
Considering fault interaction in estimates of absolute stress along faults in the San Gorgonio Pass region, southern California
Onset of slip partitioning under oblique convergence within scaled physical experiments
Dynamic models of earthquake rupture along branch faults of the eastern San Gorgonio Pass region in California using complex fault structure
Mechanical Models Suggest Fault Linkage through the Imperial Valley, California, U.S.A.
Sensitivity of deformation to activity along the Mill Creek and Mission Creek strands of the southern San Andreas fault
Influence of Fault Geometry on the Spatial Distribution of Long‐Term Slip with Implications for Determining Representative Fault‐Slip Rates
Sensitivity of uplift patterns to dip of the San Andreas fault in the Coachella Valley, California
How much can off-fault deformation contribute to the slip rate discrepancy within the eastern California shear zone?
Sensitivity of the Southern San Andreas Fault System to Tectonic Boundary Conditions and Fault Configurations
Secondary normal faulting in the Lake Mead fault system and implications for regional fault mechanics
The hypothesized presence of a detachment underlying the Lake Mead region has created a dichotomy in the interpretations of the roles of strike-slip faults of the Lake Mead fault system in accommodating regional deformation. Our detailed field mapping reveals a previously unnamed left-lateral strike-slip segment of the Lake Mead fault system and a dense cluster of dominantly west-dipping and related normal faults located near Pinto Ridge. We suggest that the strike-slip fault that we refer to as the Pinto Ridge fault: (1) was kinematically related to the Bitter Spring Valley fault; (2) was responsible for the creation of the normal fault cluster at Pinto Ridge; and (3) utilized these normal faults as linking structures between separate strike-slip fault segments to create a longer, through-going fault. Results from numerical models demonstrate that the observed location and curving strike patterns of the normal fault cluster are consistent with the faults having formed as secondary structures as the result of the perturbed stress field around the slipping Pinto Ridge fault, regardless of whether or not the Pinto Ridge fault merges into a regional detachment at depth. Calculations of mechanical efficiency of various normal fault geometries within extending terranes suggest that a preferred west dip of normal faults likely reflects a west-dipping anisotropy at depth, such as a detachment. The apparent terminations of numerous strike-slip faults of the Lake Mead fault system into west-dipping normal faults suggest that a west-dipping detachment may be regionally coherent.