Sedighe Khodaparast
Department of Geology,Faculty of Science, Tarbiat Modares University, Tehran, Iran
[ 1 ] - Structural evidence on strike slip Kinematic inversion of the Kushk-e-Nosrat Fault zone, Central Iran
NW-tending faults in Central Iran are expected to represent dominant dextral components due to their orientation with respect to the northward motion of the Arabian Plate with respect to Eurasia. However, previously published works, as well as the focal mechanism solution of the area's earthquakes, indicate evidence of sinistral kinematic along the major faults in Central Iran. Here we present ...
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