The geological features suggested that the deposit could be derived from metasomatism of fluids which are highly enriched in volatiles and REEs. 地质特征表明牦牛坪矿床派生于高度富集挥发分和稀土元素的气成热液流体的交代作用。
The wallrock alteration is weak, with characteristics of medium-low T hydrothermal ore deposit. 围岩蚀变微弱，具中低温热液矿床的特征。
As a whole, the deposit belongs to middle-low temperature postmagmatic hydrothermal deposit. 总的来说，矿床属于中低温岩浆期后热液矿床，形成于燕山期。
