structural well balanced cross-section final results propose that the overall fault slip of Hotan fault reaches ca. 358
deposited with the east stop in the Tiklik thrust zone, and Buya syncline forming on the hanging wall 446
fault plus the cooling of samples from your hanging wall of the Tiklik fault in the analyze. The function is 469
layers played an productive job in propagating deformation from western Tibetan Plateau into Tarim 38
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the fault underwent considerable activity at late Oligocene to early Miocene, resulting in the 344
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The India-Eurasian collision has created a broad zone of intracontinental deformation that extends forty six
Irrespective of whether there have been volcanic tuff beds while in the area described by Zheng et al. (2015a) was beneath 134
occasion may well mark the underthrusting of the Tarim block beneath the western Tibetan Plateau, although 494
concerning the rather secure Tarim Basin during the north as well as intensely deformed western Tibetan fifty one
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the mineral focus underneath a binocular microscope. AFT analyses in the samples had been carried 172
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