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the early levels of the India–Asia continental collision are also lacking. The western Tarim Basin with the northeastern margin from the Pamir presents a perfect prospect to investigate their development and evolution.

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in the Tiklik fault. Additionally, the kinematic evolution pointed out higher than is suitable Using the Make contact with 447

insights into your design, timing and kinematics of deformation throughout this segment of your Western seventy eight

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with the structural and apatite fission-keep track of results in this study. See the textual content for comprehensive discussions. 823

Throughout the Paleocene, alluvial supporter conglomerates were deposited alongside the northeastern margin in the Pamir, in addition to a thick gypsum unit began to be deposited from the Tarim Basin. Each one of these traces of proof indicate the north-verging thrusting, foreland basin subsidence, uplift, and northward indentation with the Pamir began inside the Paleocene (sixty two–fifty eight Ma).

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3 main stages tiklik.com for kinematic evolution of the Hotan-Tiklik traverse. The first phase previous to late 411

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