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隆瓦寺院金矿为多期活动的断裂构造和中酸性脉岩双重控矿的蚀变岩型中型金矿床,矿区内的多条矿化蚀变带,具有宽度大、走向延伸较稳定的特征。通过对该成矿特征及成矿条件分析,该矿体形态较简单,总体厚度变化较稳定,品位变化不太均匀。矿体的形成主要受一套浅变质碎屑岩建造、断裂构造及中酸性侵入岩脉的控制。该矿有利的成矿条件和特定的成矿类型对该地区的找矿具有重要指示意义。
The Longwa Temple gold deposit is a multi-phase active fault structure and alteration rock type medium-sized gold deposit with double-controlled ore-vein alteration. Multiple mineralized alteration zones in the mining area have features of large width and more stable extension . Through the analysis of the metallogenic characteristics and metallogenic conditions, the orebody morphology is relatively simple, the overall thickness changes more stable, the grade change is not uniform. The formation of ore bodies is mainly controlled by a set of metamorphic clastic rocks, fault structures and intermediate-acid intrusive dikes. The favorable metallogenic conditions and the specific metallogenic types of this deposit are of great significance to prospecting in this area.