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the early levels from the India–Asia continental collision will also be lacking. The western Tarim Basin with the northeastern margin with the Pamir presents a super option to analyze their development and evolution.section lengths, fault slip and shortening magnitudes in particular stage. The strata symbols are the 813The specific st
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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.La platefo