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the early stages of the India–Asia continental collision can also be lacking. The western Tarim Basin within the northeastern margin of your Pamir supplies an excellent possibility to research their formation and evolution.

zone Along with the interpretation of seismic profile, whilst from the Tiklik thrust zone, without having details to 354

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on the Tiklik fault. In addition, the kinematic evolution observed over is compatible While using the Speak to 447

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map on the examined area While using the places with the Tiklik-Hotan portion and also the fission-track 787

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The western Kunlun thrust belt defines the boundary involving the steady Tarim Basin while in the north along with the intensely deformed Cenozoic Tibetan Plateau while in the south. As a consequence of its significant tectonic placement, comprehension its tectonic evolution should have essential implications for propagation of deformation from Tibet to its neighboring cratonal regions all through India-Eurasia convergence. We in this article current new structural analyses according to field investigations and seismic reflection profiles through the Hotan-Tiklik section from the western Kunlun thrust belt. The results point out that the structural portion crosses two big thrust zones: the Tiklik zone inside the hinterland to the south as well as Hotan zone while in the foreland towards the north.In just these, the Hotan thrust zone is skinny skinned, with its deformation characterised by fault-bend folding and fault slipping alongside detachment levels, whereas the Tiklik thrust zone consists of basement, with its deformation driven because of the now steeply dipping Tiklik fault.

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in between the comparatively steady Tarim Basin while in the north as well as intensely deformed western Tibetan fifty one

earthquake: seismic dangers of an Energetic blind wedge thrust method within the Western Kunlun selection 600

show which the structural section crosses two key thrust zones: the Tiklik zone in the hinterland 25

The arc-formed thrust belt during the entrance of West Kunlun Mountains shaped in Cenozoic With all the northward thrust and lateral rotation of Pamir syntax. We right here present our new industry investigation and seismic profile interpretation facts to review the fault program, which offers The premise to be familiar with the advanced arc-shaped foreland thrust belt. The results suggest the thrust belt mostly consists of thrust faults with dependable placing for the arc condition with the thrust belt, but in the middle part arise some thrust fault holding dextral strike-slip part.

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