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attained from inverse modeling of track annealing conduct in apatite utilizing the HeFTy software 818

zone Along with the interpretation of seismic profile, when inside the Tiklik thrust zone, with no details to 354

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would not allow the Pt strata to become carried in the hanging wall of the Tiklik fault, demanding A different 407

insights in to the fashion, timing and kinematics of deformation across this section of your Western seventy eight

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Our analyses expose the central and northern Qilian Shan underwent rapid cooling in the course of the Cretaceous on account of a much-industry tectonic occasion. From the Eocene-Oligocene, a duration of thrust-connected cooling happened together the Shule Nan Shan, Tuolai Nan Shan and Tuolai Shan faults. Reactivation in the proximal thrust faults and initiation with the western segment in the Haiyuan fault happened at ca. sixteen Ma and drove final accelerated Miocene cooling and denudation to the surface area. We argue which the Qilian Shan thrust belt has persisted as the stationary and internally deformed northern boundary on the Himalayan-Tibetan orogen Considering that the early Cenozoic, involved overprinting out-of-sequence advancement starting off by Eocene related to initiation of India-Asia collision, as well as the basins and ranges over the northern Tibetan Plateau have considering the fact that experienced multi-stage of advancement.

Our outcomes suggest that the fold belt is really a segmented, Lively blind wedge thrust technique. The Pishan event is produced by a person wedge thrust segment alongside its leading edge: the mainshock is produced over the minimal-angle fore-thrust Slik ramp, as well as aftershocks are diffusely distributed over the ramp, overlying anticline, plus some unimaged structures beneath the ramp. Mapped measurements of other segments counsel that the fold belt is able to much bigger (Mw ≥seven:5) and a lot more harmful earthquakes.

reflections to the stratigraphic units while in the seismic profile. The structural and advancement strata model 156

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earthquake: seismic hazards of an Lively blind wedge thrust method within the Western Kunlun array 600

Cenozoic tectonic rotations in different portions of the NE Pamir: implications for the evolution with the arcuate orogen

The arc-shaped thrust belt inside the front of West Kunlun Mountains fashioned in Cenozoic Using the northward thrust and lateral rotation of Pamir syntax. We listed here present our new field investigation and seismic profile interpretation data to check the fault process, which delivers The idea to grasp the advanced arc-shaped foreland thrust belt. The outcome reveal that the thrust belt primarily includes thrust faults with steady hanging on the arc form on the thrust belt, but in the middle portion manifest some thrust fault holding dextral strike-slip part.

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