On the north flank of western Kunlun, the deformation of Sugaite anticline commenced in Pliocene (about four.0 million many years in advance of present). Yingjisha anticline started out during the late Pleistocene. Aketao anticline started out eventually on the late Pleistocene, and Kekeya anticline and Guman anticline started while in the late Pli

structural balanced cross-area success recommend that the full fault slip of Hotan fault reaches ca. 358However, the confined tectonic rotations of your Keliyang and Sanju sections is often discussed with the dominant thrust faulting inside the foreland from the West Kunlun Mountains. Coupled with the present paleomagnetic info round the Pam

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