the early levels of your India–Asia continental collision may also be missing. The western Tarim Basin for the northeastern margin with the Pamir supplies an excellent possibility to investigate their development and evolution.
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U-Pb and Hf isotopic through the east section of Tiekelike tectonic belt: constrains within the timing 682
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the fault underwent sizeable exercise at late Oligocene to early Miocene, causing the 344
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The India-Eurasian collision has produced a wide zone of intracontinental deformation that extends 46
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reflections into the stratigraphic models within the seismic profile. The structural and progress strata model 156
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the mineral concentrate below a binocular microscope. AFT analyses from the samples had been carried 172
Maigaiti slope is sort of 200 km in size, but it hasn't clear deformation, and taper wedge angle of the fold and thrust belt is lower than All those Lively orogenies, It is suggests the gypsum-mudstone of Aertashi Development and the shape of Cenozoic deposition are crucial things, the gypsum-mudstone controls α of taper wedge, the shapes of basement and dispositive wedge Handle β of taper wedge.