Over the north flank of western Kunlun, the deformation of Sugaite anticline commenced in Pliocene (about four.0 million many years in advance of present). Yingjisha anticline started while in the late Pleistocene. Aketao anticline begun ultimately on the late Pleistocene, and Kekeya anticline and Guman anticline started inside the late Pliocene-early Pleistocene (from two.fourteen to one.8 million a long time in advance of present). Consequently, it is actually deduced that the tectonic deformation largely befell in the Pliocene for the Quaternarg alongside the entrance belts of Pamir-western Kunlun-southwest Tianshan in China.
zone Along with the interpretation of seismic profile, although during the Tiklik thrust zone, without having data to 354
U-Pb and Hf isotopic within the east phase of Tiekelike tectonic belt: constrains about the timing 682
cross-area combined with the apatite fission-monitor results advise the Hotan-Tiklik segment 34
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the fault underwent considerable action at late Oligocene to early Miocene, leading to the 344
The structural Assessment of the seismic profile suggests that the growth strata began to establish 338
action of your Tiklik fault considering that mid- to late-Miocene is consistent with the unconformity amongst 451
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The impact of syntectonic sedimentation on thrust belt deformation: a kinematic model example from your triangle zone in the Western Kunlun thrust belt
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three important phases for kinematic evolution in the tiklik.com Hotan-Tiklik traverse. The initial stage previous to late 411
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