overlying late Paleozoic strata are already verified by each outcrops and borehole knowledge. Within just a hundred and twenty
Even so, the constrained tectonic rotations with the Keliyang and Sanju sections might be discussed through the dominant thrust faulting within the foreland of the West Kunlun Mountains. Coupled with the present paleomagnetic data within the Pamir salient, our benefits help a four-phase evolution: (1) a about linear orogen prior to the early Eocene; (2) symmetric rotations on either side right up until the latest Oligocene accompanied by (3) asymmetric geometries with ongoing radial thrusting within the western flank and enormous-scale strike-slip fault about the eastern flank; and (four) last collision concerning the Pamir salient and SW Tian Shan from the late Miocene.
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insights into your fashion, timing and kinematics of deformation across this section of the Western 78
The Pamir salient, defining the NW finish of the Himalayan–Tibetan orogen, is often a distinguished curved orogen as being a reaction on the Indian-Eurasian collision. Its evolution heritage is important for comprehension intracontinental tectonic processes within the context of continental collision. During this examine, we carry out systematic paleomagnetic scientific tests on four sections in several parts of the NE Pamir to unravel the tectonic evolution of your curved orogen. Our new final results within the Oytag area counsel the clockwise (CW) rotations of your eastern Pamir salient predominantly transpired during the Oligocene (~ 32–26 Ma) like a reaction towards the northward indentation with the Pamir salient and was dominated by large-scale dextral strike-slip faults due to the fact then. Additionally, the final collision involving Pamir and SW Tian Shan in the latest Miocene reactivated the dextral Talas-Ferghana Fault (TFF), As a result be responsible for the counter-clockwise (CCW) rotations at Ulugqat.
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We also document exhumation on the shear zone from two minimal-temperature thermochronologic transects. New apatite (U-Th)/He information and published thermochronologic success reveal two accelerated cooling episodes, backed by stratigraphic and geomorphic observations. The very first rapid cooling section transpired from ca. 27 to 17 Ma with elimination of cover rocks and exhumation of your shear zone. The next accelerated cooling episode exposed by our AHe details commenced at 14-thirteen Ma, lasting two-3 Myr. The Ailao Shan variety might have risen to its modern elevation with significant-relief topography acquiring resulting from river incision. We interpret the onset of this swift exhumation to reflect renewed plateau advancement linked to lower crustal stream.
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reflections to the stratigraphic units inside the seismic profile. The structural and advancement strata design 156
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stage, the hanging wall of Tiklik fault slipped together the fault to uplift AFT samples inside the study 421
The arc-formed thrust belt while in the front of West Kunlun Mountains formed in Cenozoic Together with the northward thrust and lateral rotation of Pamir syntax. We in this article existing our new industry investigation and seismic profile interpretation data to study the fault system, which provides The premise to comprehend the intricate arc-shaped foreland tiklik.com thrust belt. The outcomes show which the thrust belt predominantly contains thrust faults with regular hanging towards the arc shape of the thrust belt, but in the middle portion come about some thrust fault holding dextral strike-slip component.