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by common density and magnetic separation with the crushed samples, with closing hand selecting from 171
linked floor geology, particularly while in the Aqike and Buya areas, continue to be unclear and need 396
layers performed an economical position in propagating deformation from western Tibetan Plateau into Tarim 38
Tiklik fault underwent two stages of exhumation, an earlier phase during late Oligocene to early 399
Hotan fault produced along the higher fault-flat (detachment layer alongside lowermost Pz1 strata) of 418
The structural Investigation in the seismic profile suggests that The expansion strata began to acquire 338
The India-Eurasian collision has developed a large zone of intracontinental deformation that extends 46
In addition, the AFT results of your samples from your hanging wall in the Tiklik fault recommend that 343
from the phase was primarily absorbed by basement-concerned Tiklik fault and fault-propagation fold sixty seven
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The West Kunlun vary, together the northwest margin on the Tibetan Plateau includes a crucial file of plateau formation and its northwards enlargement. Having said that, besides the properly-documented Miocene tiklik.com tectonism, its extended-phrase background of exhumation/uplift stays enigmatic. Right here we report an integrated low-temperature thermochronology study (apatite fission track and corresponding zircon (U-Th)/He) across a N-S transect through the West Kunlun range that reveals a protracted very low-temperature thermochronological file, characterized by a complex mosaic of thermal histories from the person terrane things for the duration of amalgamation to sort the Tibetan Plateau. Our new knowledge reveal two popular cooling episodes over the Cretaceous along with the Neogene, along with several other additional subdued and/or localized cooling episodes.
stage, the hanging wall of Tiklik fault slipped together the fault to uplift AFT samples while in the study 421
interpreted the anticline like a fault-propagation fold. Supplied the fact that the thrust fault is bounded 426