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overlying late Paleozoic strata are actually confirmed by both outcrops and borehole knowledge. In just one hundred twentyOn the other hand, the constrained tectonic rotations from the Keliyang and Sanju sections could be discussed by the dominant thrust faulting within the foreland from the West Kunlun Mountains. Combined with the existing

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overlying late Paleozoic strata have already been confirmed by the two outcrops and borehole facts. In just 120shift in northeastern Tibet coincides with enlargement with the plateau margin in southeastern Tibet, the onset of standard faulting in central Tibet, and accelerated shortening in northern Tibet. Collectively these phenomena recomm

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