tiklik.com - An Overview

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However, the confined tectonic rotations with the Keliyang and Sanju sections is often discussed through the dominant thrust faulting within the foreland of your West Kunlun Mountains. Coupled with the present paleomagnetic info across the Pamir salient, our success guidance a four-phase evolution: (1) a roughly linear orogen ahead of the early Eocene; (2) symmetric rotations on either side until finally the latest Oligocene followed by (3) asymmetric geometries with continued radial thrusting over the western flank and huge-scale strike-slip fault to the japanese flank; and (4) closing collision amongst the Pamir salient and SW Tian Shan within the late Miocene.

connected area geology, particularly while in the Aqike and Buya regions, continue being unclear and need 396

cross-area coupled with the apatite fission-observe outcomes suggest the Hotan-Tiklik segment 34

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The Pamir salient, defining the NW close on the Himalayan–Tibetan orogen, is actually a distinguished curved orogen as being a reaction on the Indian-Eurasian collision. Its evolution background is important for comprehension intracontinental tectonic processes during the context of continental collision. During this examine, we carry out systematic paleomagnetic research on 4 sections in different portions of the NE Pamir to unravel the tectonic evolution in the curved orogen. Our new success with the Oytag area recommend that the clockwise (CW) rotations of your japanese Pamir salient predominantly occurred during the Oligocene (~ 32–26 Ma) like a reaction to your northward indentation from the Pamir salient and was dominated by substantial-scale dextral strike-slip faults because then. Also, the ultimate collision among Pamir and SW Tian Shan in the most up-to-date Miocene reactivated the dextral Talas-Ferghana Fault (TFF), Therefore be to blame for the counter-clockwise (CCW) rotations at Ulugqat.

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action of the Tiklik fault considering that mid- to late-Miocene is in step with the unconformity between 451

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The West Kunlun range, together the northwest margin with the Tibetan Plateau has a significant file of plateau formation and its northwards enlargement. Having said that, besides the properly-documented Miocene tectonism, its extended-term record of exhumation/uplift stays enigmatic. Right here we report an built-in very low-temperature thermochronology examine (apatite fission track and corresponding zircon (U-Th)/He) throughout a N-S transect with the West Kunlun range that reveals a protracted minimal-temperature thermochronological record, characterised by a complex mosaic of thermal histories from the person terrane factors throughout amalgamation to variety the Tibetan Plateau. Our new knowledge reveal two popular cooling episodes in the course of the Cretaceous plus the Neogene, along with several other far more subdued and/or localized cooling episodes.

Cenozoic fold and thrust belt in japanese part of the piedmount of west Kunlun and its taper wedge mechanics

Maigaiti slope is sort of two hundred km in length, but it surely has not evident deformation, and taper wedge angle of the fold and thrust belt is under All those active orogenies, It truly is usually means the gypsum-mudstone of Aertashi Formation and the shape of Cenozoic deposition are essential things, the gypsum-mudstone controls α of taper wedge, the shapes of basement and dispositive wedge Management β of taper wedge.

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