structural balanced cross-segment final results advise that the full fault slip of Hotan fault reaches ca. 358
Even so, the limited tectonic rotations of the Keliyang and Sanju sections may be stated with the dominant thrust faulting from the foreland from the West Kunlun Mountains. Coupled with the present paleomagnetic information round the Pamir salient, our success help a 4-stage evolution: (one) a about linear orogen prior to the early Eocene; (2) symmetric rotations on either side until the latest Oligocene followed by (3) asymmetric geometries with continued radial thrusting on the western flank and large-scale strike-slip fault around the jap flank; and (four) last collision between the Pamir salient and SW Tian Shan from the late Miocene.
U-Pb and Hf isotopic from your east segment of Tiekelike tectonic belt: constrains around the timing 682
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The India-Eurasian collision has made a broad zone of intracontinental deformation that extends forty six
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Throughout the Paleocene, alluvial supporter conglomerates have been deposited together the northeastern margin of your Pamir, in addition to a thick gypsum device began to be deposited while in the Tarim Basin. All these traces of proof indicate that the north-verging thrusting, foreland basin subsidence, uplift, and northward indentation of your Pamir started within the Paleocene (sixty two–58 Ma).
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The discrepant arrangement of your Carpathian nappes and syntectonic deposits on the Carpathian Foredeep reveals the oroclinal migration in the subduction direction of your System margin over the Late Cenozoic. Formation from the nappes was induced by their detachment from disintegrated segments of the ecu Platform; the segments were shortened due to their vertical rotation in zones ... [Present full summary] of compressional sutures. It finds expression in nearby prevalence on the backward vergence of folding against the commonly forward vergence towards the Carpathian Foredeep. The precompressional configuration of sedimentation areas of unique nappes was reconstructed with application with the palinspastic approach, on The premise in the hitherto undervalued product which emphasizes the affect of your subduction and differentiated morphology in the System basement within the tectonic evolution of your fold and thrust belt.
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