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deposited for the east close of your Tiklik thrust zone, and Buya syncline forming with the hanging wall 446
fault as well as cooling of samples with the hanging wall in the Tiklik fault within the analyze. The function is 469
layers played an successful function in propagating deformation from western Tibetan Plateau into Tarim 38
comments on an before draft and Xin Wang for help in revising the manuscript. We've been grateful 510
The Pamir salient, defining the NW conclude in the Himalayan–Tibetan orogen, is a popular curved orogen for a reaction for the Indian-Eurasian collision. Its evolution history is important for knowing intracontinental tectonic procedures while in the context of continental collision. On this study, we carry out systematic paleomagnetic scientific studies on four sections in different parts of the NE Pamir to unravel the tectonic evolution with the curved orogen. Our new benefits within the Oytag portion suggest which the clockwise (CW) rotations of the jap Pamir salient predominantly happened from the Oligocene (~ 32–26 Ma) for a reaction into the northward indentation in the Pamir salient and was dominated by huge-scale dextral strike-slip faults due to the fact then. Additionally, the ultimate collision in between Pamir and SW Tian Shan in the most recent Miocene reactivated the dextral Talas-Ferghana Fault (TFF), As a result be to blame for the counter-clockwise (CCW) rotations at Ulugqat.
This transformation in thrust-fault orientation refl ects a Middle Miocene adjust during the kinematic style of plateau development, from long-standing NNE-SSW contraction that mimicked the plate convergence way to your inclusion of latest constructions accommodating east-west motion. This kinematic
proposed An additional deeper detachment mattress together mid-crust to deliver the Tiklik fault, constant 409
Our final results suggest that the fold belt is actually a segmented, Energetic blind wedge thrust process. The Pishan party is generated by a single wedge thrust section alongside its primary edge: the mainshock is created on the reduced-angle fore-thrust Slik ramp, as well as the aftershocks are diffusely distributed over the ramp, overlying anticline, and many unimaged buildings beneath the ramp. Mapped dimensions of other segments counsel which the fold belt is capable of much larger (Mw ≥7:5) plus much more damaging earthquakes.
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As observed previously mentioned, in light on the Hotan thrust zone, the interpretation of seismic profile and its 357
the mineral concentrate under a binocular microscope. AFT analyses of the samples have been carried 172
interpreted the anticline being a fault-propagation fold. Specified the fact that the thrust fault is bounded 426