Mineralization process includes K-feldspar–quartz–pyrite, quartz–molybdenite, quartz–sulfide, and quartz–calcite stages.

The ore-forming fluids are high temperature, moderate salinity and relatively reduced condition.

The ore-forming fluids were evolved from magmatic to meteoric in origin, and materials came from the lower continental crust.

The decrease in temperature and remarkable transition of redox condition were critical for the formation of the Mo deposit.