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To the north flank of western Kunlun, the deformation of Sugaite anticline started out in Pliocene (about four.0 million years in advance of existing). Yingjisha anticline started out during the late Pleistocene. Aketao anticline started out in the long run of the late Pleistocene, and Kekeya anticline and Guman anticline commenced during the late
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reflections to your stratigraphic models in the seismic profile. The structural and expansion strata style 156Effects from apatite fission keep track of thermochronology together with growth strata and balanced cross area point out which the Hotan-Tiklik phase underwent two-phase deformation: (one) enhancement of the Tiklik thrust throughout
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