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About the north flank of western Kunlun, the deformation of Sugaite anticline started in Pliocene (about 4.0 million decades just before existing). Yingjisha anticline started while in the late Pleistocene. Aketao anticline begun ultimately of the late Pleistocene, and Kekeya anticline and Guman anticline commenced during the late Pliocene-early Pleistocene https://tiklik.com/

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