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overlying late Paleozoic strata happen to be confirmed by each outcrops and borehole information. In just one hundred twenty

zone with the interpretation of seismic profile, even though within the Tiklik thrust zone, devoid of info to 354

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cross-area coupled with the apatite fission-monitor success propose which the Hotan-Tiklik segment 34

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cross-area of seismic profiles to ascertain the timing and shortening magnitude of the Hotan 148

interpreted to mark thrusting and exhumation of your surrounding orogens throughout the Tarim Basin 461

The western Kunlun thrust belt defines the boundary amongst the steady Tarim Basin while in the north plus the intensely deformed Cenozoic Tibetan Plateau from the south. On account of its critical tectonic placement, knowing its tectonic evolution should have important implications for propagation of deformation from Tibet to its neighboring cratonal locations for the duration of India-Eurasia convergence. We listed here present new structural analyses based on industry investigations and seismic reflection profiles over the Hotan-Tiklik segment of your western Kunlun thrust belt. The final results reveal that the structural portion crosses two key thrust zones: the Tiklik zone inside the hinterland for the south and also the Hotan zone within the foreland into the north.In these, the Hotan thrust zone is thin skinned, with its deformation characterised by fault-bend folding and fault slipping along detachment levels, whereas the Tiklik thrust zone involves basement, with its deformation pushed from the now steeply dipping Tiklik fault.

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with the structural and apatite fission-track results in this study. See the textual content for detailed conversations. 823

The impact of syntectonic sedimentation on thrust belt deformation: a kinematic product example from your triangle zone in the Western Kunlun thrust belt

The West Kunlun vary, alongside the northwest margin on the Tibetan Plateau includes a crucial record of plateau development and its northwards growth. Even so, aside from the nicely-documented Miocene tectonism, its long-term record of exhumation/uplift continues to be enigmatic. Listed here we report an integrated small-temperature thermochronology review (apatite fission monitor and corresponding zircon (U-Th)/He) throughout a N-S transect from the West Kunlun selection that reveals a prolonged small-temperature thermochronological report, characterized by a posh mosaic of thermal histories from the individual terrane elements all through amalgamation to kind the Tibetan Plateau. Our new information expose two well known cooling episodes during the Cretaceous plus the Neogene, along with several other additional subdued and/or localized cooling episodes.

terrane is divided in the Tarim block on the north by the north-vergent Tiklik fault, as well as the 87

of Buya managed the deformation from the Buya region. These variables or their integration would 444

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