The active Altyn Tagh fault system defines the northern fringe of the Tibetan Plateau, absorbs up to one-third to 1-fifth in the India – Siberia convergence by means of left-lateral slip , and functions as a very important tectonic boundary in various geodynamic products relating to rise and northward growth of the Tibetan Plateau.
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insights in the style, timing and kinematics of deformation across this section of the Western 78
unconformities, While N1 sits higher than C in the north of Buya and N2 overlies previously mentioned Pt to farther 437
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Maigaiti slope is almost 200 km in size, but it really has not noticeable deformation, and taper wedge angle of the fold and thrust belt is fewer than those active orogenies, it's indicates the gypsum-mudstone of Aertashi Formation and The form of Cenozoic deposition are vital things, the gypsum-mudstone controls α of taper wedge, the styles of basement and dispositive wedge Regulate β of taper wedge.
As a result, The expansion strata made above the Hotan fold present constraints tiklik.com To judge the 334
interpreted to mark thrusting and exhumation of the surrounding orogens throughout the Tarim Basin 461
Moreover, the AFT final results in the samples in the hanging wall from the Tiklik fault suggest that 343
interpreted the anticline like a fault-propagation fold. Supplied the fact that the thrust fault is bounded 426
of Buya managed the deformation in the Buya region. These aspects or their integration would 444
to your south by the Tiklik fault and Paleozoic strata (D, C and P) crop out with the Main of your 427
portion lengths, fault slip and shortening magnitudes in unique phase. The strata symbols tend to be the 813