structural well balanced cross-part results counsel that the full fault slip of Hotan fault reaches ca. 358
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with the Tiklik fault. Moreover, the kinematic evolution mentioned above is suitable Using the Call 447
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towards the south with the Tiklik fault and Paleozoic strata (D, C and P) crop out within the core in the 427
The seismic data reveal which the Hotan fold is actually a fault-bend fold managed by the Hotan fault. 333
lowered on the east in the Tiklik thrust zone Using the Tiklik fault plunging for the east (e.g. Jiang 440
Paleogene detachment layer and soak up considerable portion of shortening within the segment (Liang et 72
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between the relatively secure Tarim Basin during the north as well as intensely deformed western Tibetan fifty one
earthquake: seismic dangers of an Energetic blind wedge thrust method within the Western Kunlun tiklik.com selection 600
phase, the hanging wall of Tiklik fault slipped along the fault to uplift AFT samples from the study 421
interpreted the anticline as being a fault-propagation fold. Presented The point that the thrust fault is bounded 426