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Around the north flank of western Kunlun, the deformation of Sugaite anticline started off in Pliocene (about four.0 million yrs just before existing). Yingjisha anticline started off inside the late Pleistocene. Aketao anticline started in the long run of the late Pleistocene, and Kekeya anticline and Guman anticline commenced during the late Plio

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