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The structural Assessment with the seismic profile indicates that The expansion strata began to develop 338
The India-Eurasian collision has made a wide zone of intracontinental deformation that extends forty six
indicate the structural portion crosses two main thrust zones: the Tiklik zone while in the hinterland 25
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Hotan fault slips along the detachment layer within the lowermost Paleogene strata and many of the slip 365
the fault underwent major exercise at late Oligocene to early Miocene, resulting in the 344
Cette nouvelle économie à donner naissance à plusieurs acteurs dans ce secteur et notamment des nouvelles plateformes en ligne permettant de moderniser le secteur.
interpreted to mark thrusting and exhumation with the bordering orogens across the Tarim Basin 461
This modification in thrust-fault orientation refl ects a Middle Miocene transform inside the kinematic style of plateau expansion, from lengthy-standing NNE-SSW contraction that mimicked the plate convergence way for the inclusion of recent tiklik.com structures accommodating east-west movement. This kinematic
The results of the Examination provide new insights right into a kinematic model for triangle zones and advise that these two distinct models shaped because of two-stage syntectonic sedimentation. We further more go over the kinematic product of tectonic deformation provided the existence of two-stage syntectonic sediments and propose 4 distinctive sedimentary superposition patterns. Every one of these sequences suggest that deformation is controlled by full syntectonic sediment geometry and imply that early sediment form exerts the best influence. The presence of early prograding sediment encourages the event from the spaced thrust belt, when an early aggrading bundle boosts the structure on the limited thrust adjacent towards the hinterland.
expressed by activity of Tiklik fault which has been indicated by the sooner cooling stage recorded 348
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