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As pointed out previously mentioned, in light-weight in the Hotan thrust zone, the interpretation of seismic profile and its 357The West Kunlun vary, alongside the northwest margin in the Tibetan Plateau consists of an important document of plateau development and its northwards enlargement. Having said that, in addition to the well-document

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The active Altyn Tagh fault system defines the northern fringe of the Tibetan Plateau, absorbs up to at least one-3rd to 1-fifth in the India – Siberia convergence by means of left-lateral slip , and functions as a very important tectonic boundary in several geodynamic types regarding rise and northward development in the Tibetan Plateau.La

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