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About the north flank of western Kunlun, the deformation of Sugaite anticline began in Pliocene (about 4.0 million decades before present). Yingjisha anticline begun in the late Pleistocene. Aketao anticline started off ultimately of your late Pleistocene, and Kekeya anticline and Guman anticline started out during the late Pliocene-early Pleistoce

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reflections towards the stratigraphic models inside the seismic profile. The structural and growth strata type 156involving the fairly steady Tarim Basin in the north as well as the intensely deformed western Tibetan 51The seismic data suggest which the Hotan fold is often a fault-bend fold controlled from the Hotan fault. 333P

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