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However, the confined tectonic rotations with the Keliyang and Sanju sections is often defined through the dominant thrust faulting within the foreland of the West Kunlun Mountains. Coupled with the present paleomagnetic information around the Pamir salient, our success guidance a four-phase evolution: (one) a roughly linear orogen ahead of the early Eocene; (2) symmetric rotations on either side right up until the most recent Oligocene accompanied by (3) asymmetric geometries with continued radial thrusting to the western flank and huge-scale strike-slip fault on the japanese flank; and (4) closing collision among the Pamir salient and SW Tian Shan in the late Miocene.
U-Pb and Hf isotopic in the east segment of Tiekelike tectonic belt: constrains around the timing 682
would not allow the Pt strata being carried inside the hanging wall with the Tiklik fault, necessitating A different 407
Surface uplift, river incision, shear zone exhumation, and displacement along active faults have all interacted to form the fashionable landscape during the southeastern margin of the Tibetan Plateau. The Ailao Shan-Crimson River fault, An important composition within the tectonic evolution of southeastern Asia, is an excellent recorder of those procedures. We existing new stratigraphic, structural, and small-temperature ... [Display entire summary] thermochronologic info to check out its late Cenozoic tectonic and geomorphic evolution. The stratigraphic and structural observations suggest that the main bend inside the fault was a releasing bend with important Miocene sedimentation from the early-Center Miocene, but grew to become a restraining bend with ample shortening buildings made once the late Miocene reversal of displacement.
design Within this study. We speculate the lateral fault-ramp connected with the Aqike anticline in 431
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proposed another further detachment bed along mid-crust to produce the Tiklik fault, regular 409
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As mentioned earlier mentioned, in light-weight in the Hotan thrust zone, the interpretation of seismic profile and its 357
Effects from apatite fission track thermochronology in combination with development strata and well balanced cross section reveal which the Hotan-Tiklik segment underwent two-stage deformation: (one) development in the Tiklik thrust over the late Oligocene-early Miocene and all over again Considering that the mid- to late Miocene and (2) activity from the Hotan thrust since the mid- to late Miocene as a result of basinward propagation of thrusting. The well balanced cross section, combined with the apatite fission observe benefits, implies which the Hotan-Tiklik segment contributes a total shortening magnitude of in excess of ca. 34 ± six km. Within this, ca. 4 ± 2 and ca. 23 ± 1 km of the shortenings had been absorbed through the Hotan anticline along with the Hotan detachment fault, respectively, both equally of which were being related to detachment layers. This suggests that detachment levels performed an economical role in propagating deformation in the western Tibetan Plateau into the Tarim Basin.
interpreted the anticline as being a fault-propagation fold. Supplied The truth that the thrust fault is bounded 426