structural balanced cross-part success suggest that the total fault slip of Hotan fault reaches ca. 358striking Aqike anticline into the east. The Hotan fault can be a blind thrust which is interpreted to ninety eightFault characteristics and division of tectonic models of the thrust belt while in the front on the West Kunlun Mountain

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As mentioned earlier mentioned, in light-weight from the Hotan thrust zone, the interpretation of seismic profile and its 357Final results from apatite fission observe thermochronology in combination with development strata and balanced cross area reveal the Hotan-Tiklik phase underwent two-phase deformation: (one) progress of your Tiklik th