structural well balanced cross-part success suggest that the entire fault slip of Hotan fault reaches ca. 358shift in northeastern Tibet coincides with expansion from the plateau margin in southeastern Tibet, the onset of typical faulting in central Tibet, and accelerated shortening in northern Tibet. Jointly these phenomena counsel a platea

As famous higher than, in light in the Hotan thrust zone, the interpretation of seismic profile and its 357Benefits from apatite fission keep track of thermochronology together with growth strata and well balanced cross area suggest which the Hotan-Tiklik section underwent two-phase deformation: (1) progress of your Tiklik thrust through the

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