In 2008, object samples of natural gas hydrates were obtained for the first time by drilling in the permafrost region of the Qilian Mountains in China. In 2010, an experimental study of natural gas hydrates in the Mull region by the seismic reflection method was carried out. Comprehensive analyses and interpretation of the seismic, well log and geological data suggest that reflections formed by natural gas hydrates on seismic profiles are characterized by low velocity, low amplitude and high frequency. The distribution of natural gas hydrates is associated with fracture zones. On its forming mechanism, the gas moved up along the deep fault, was sealed and accumulated by the permafrost, and formed reservoirs in suitable temperature-pressure conditions.