To the north flank of western Kunlun, the deformation of Sugaite anticline commenced in Pliocene (about 4.0 million many years in advance of existing). Yingjisha anticline began during the late Pleistocene. Aketao anticline started out eventually in the late Pleistocene, and Kekeya anticline and Guman anticline began during the late Pliocene-early

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