On the north flank of western Kunlun, the deformation of Sugaite anticline commenced in Pliocene (about four.0 million several years prior to present). Yingjisha anticline started in the late Pleistocene. Aketao anticline started off ultimately from the late Pleistocene, and Kekeya anticline and Guman anticline began within the late Pliocene-early

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