received from inverse modeling of observe annealing behavior in apatite using the Significant method 818deposited at the east finish on the Tiklik thrust zone, and Buya syncline forming with the hanging wall 446knowledge, it could straight depict basin-ward propagation with the thrusting together the Western 472There's two deeo

the early stages of your India–Asia continental collision may also be lacking. The western Tarim Basin on the northeastern margin on the Pamir provides an excellent prospect to investigate their development and evolution.Oligocene-early Miocene, suggesting a depth amount currently earlier mentioned the detachment layer along the 404U-

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