The deposit is an example of the oxidized-type skarn related to high-K to shoshonitic igneous suite.
Two to three major stages of scheelite and sulfide deposition occurred.
Fluid evolution included an early high-temperature, high-pressure, and high-salinity homogenous fluid.
At a later stage, fluid boiling contributed to intense scheelite deposition.
Fluids have been sourced from crystallizing magma, with progressing admixture of meteoric water.