The geological features suggested that the deposit could be derived from metasomatism of fluids which are highly enriched in volatiles and REEs. 地質(zhì)特征表明牦牛坪礦床派生于高度富集揮發(fā)分和稀土元素的氣成熱液流體的交代作用。
The wallrock alteration is weak, with characteristics of medium-low T hydrothermal ore deposit. 圍巖蝕變微弱，具中低溫熱液礦床的特征。
As a whole, the deposit belongs to middle-low temperature postmagmatic hydrothermal deposit. 總的來(lái)說(shuō)，礦床屬于中低溫巖漿期后熱液礦床，形成于燕山期。
