Around the north flank of western Kunlun, the deformation of Sugaite anticline begun in Pliocene (about 4.0 million yrs right before current). Yingjisha anticline begun within the late Pleistocene. Aketao anticline started off in the end on the late Pleistocene, and Kekeya anticline and Guman anticline begun within the late Pliocene-early Pleistoce

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