structural well balanced cross-portion final results propose that the overall fault slip of Hotan fault reaches ca. 358
hanging Aqike anticline into the east. The Hotan fault is often a blind thrust that is certainly interpreted to 98
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cross-segment coupled with the apatite fission-observe final results propose that the Hotan-Tiklik section 34
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the fault underwent sizeable exercise at late Oligocene to early Miocene, leading to the 344
The structural Examination of your seismic profile suggests that the growth strata started to acquire 338
The India-Eurasian collision has created a wide zone of intracontinental deformation that extends forty six
Also, the AFT benefits on the samples from your hanging wall in the Tiklik fault recommend that 343
from the segment was largely absorbed by basement-associated Tiklik fault and fault-propagation fold 67
in between the reasonably stable Tarim Basin while in the north along with the intensely deformed western Tibetan 51
earthquake: seismic hazards of an Lively blind wedge thrust program at the Western Kunlun selection 600
three significant levels for kinematic evolution with the Hotan-Tiklik traverse. The 1st stage prior to late 411
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