Intraplate strike-slip zones commonly display intricate 3-D geometries, with rapid changes in
structural style along strike and with depth. Strike-slip deformation typically results in …

Abstract The Kachchh Basin, located in Gujarat (India) at the western trailing edge of the
Indian plate, comprises several east–west trending seismically active faults. The Kachchh …

Pre-existing weakness due to repeated tectonic, metamorphic, and magmatic events is a
fundamental feature of the continental lithosphere on Earth. Because of this, continental …

The Ravne Fault is an actively propagating NW–SE trending dextral strike-slip fault in the
Julian Alps of NW Slovenia, which has been responsible for two moderate sized …

Mediterranean tectonics results in tight orogenic arcs enclosing back‐arc basins of oceanic
or thinned continental lithosphere. The Gibraltar Arc cannot be explained solely by the …

La dorsal neuquina es un lineamiento estructural de escala regional desarrollado a los
39ºS, que se extiende por más de 270 km con orientación EO, marcando el límite natural …

Abstract The East China Sea Shelf Basin lies between the Pacific Subduction and Indian-
Eurasian Collision tectonic domains and records Cenozoic tectonic inversion, especially in …

Abstract The Bohai Bay Basin (BBB) is a Meso–Cenozoic intracontinental petroliferous
basin, where four pre-existing continental-scale fault zones intersect, in East China. The …

Experimental models scaled for density and viscosity were performed to investigate the
effects of indentation obliquity and rheological stratification on the deformation patterns …

Abstract The Southern Andes are regarded as a typical subduction orogen formed by
oblique plate convergence. However, there is considerable uncertainty as to how …