structural well balanced cross-portion results recommend that the whole fault slip of Hotan fault reaches ca. 358With its central place between the Tibetan Plateau and the Tian Shan Array, the Tarim Basin is a essential ingredient with the Cenozoic Asian orogenic method. Even so, an extensive regional research, and a lot more significantly t

To the north flank of western Kunlun, the deformation of Sugaite anticline started in Pliocene (about four.0 million years ahead of existing). Yingjisha anticline started out during the late Pleistocene. Aketao anticline started out eventually from the late Pleistocene, and Kekeya anticline and Guman anticline commenced in the late Pliocene-early P

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