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About the north flank of western Kunlun, the deformation of Sugaite anticline started in Pliocene (about 4.0 million decades just before existing). Yingjisha anticline commenced within the late Pleistocene. Aketao anticline started ultimately of your late Pleistocene, and Kekeya anticline and Guman anticline started off within the late Pliocene-early Pleistocene (from 2.14 to 1.eight million a long time in advance of existing). Consequently, it really is deduced which the tectonic deformation mainly occurred with the Pliocene to the Quaternarg along the front belts of Pamir-western Kunlun-southwest Tianshan in China.

zone Using the interpretation of seismic profile, though from the Tiklik thrust zone, with out knowledge to 354

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insights in to the type, timing and kinematics of deformation throughout this phase of the Western 78

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We also doc exhumation of your 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 first rapid cooling phase happened from ca. 27 to seventeen Ma with removal of canopy rocks and exhumation of your shear zone. The next accelerated cooling episode disclosed by our AHe facts commenced at 14-13 Ma, Long lasting 2-three Myr. The Ailao Shan array could possibly have risen to its modern day elevation with higher-relief topography developing because of river incision. We interpret the onset of this speedy exhumation to reflect renewed plateau development connected to lessen crustal move.

Active blind-thrust methods pose hidden but harmful earthquake hazards in convergent mountain fronts world wide, exemplified by The newest 2015 Mw six.four Pishan event within the Hetian fold belt on the western Kunlun selection front, northwest Tibetan plateau. Integrated Examination of surface geology, topography, seismic reflection profiles, and Pishan seismicity delineates the surface and subsurface geometries from the Hetian fold belt.

event could mark the underthrusting with the Tarim block beneath the western Tibetan Plateau, while 494

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The depth area acquired from your conversion in the TWT time profile Together with the velocity facts 806

stage, the hanging wall of Tiklik fault slipped alongside the fault to uplift AFT samples in the examine 421

The arc-formed thrust belt in the entrance of West Kunlun Mountains shaped in Cenozoic Along with the northward thrust and lateral rotation of Pamir syntax. We below current our new discipline investigation and seismic profile interpretation info to review the fault program, which offers The premise to understand the elaborate arc-formed foreland thrust belt. The outcomes show which the thrust belt generally is made up of thrust faults with steady striking into the arc form from the thrust belt, but in the center portion happen some thrust fault Keeping dextral strike-slip element.

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