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黑龙江关鸟河铜钨矿床是近几年来老点新评有经济价值的矿床,矿床位于大兴安岭地槽褶皱系,罕达气优地槽褶皱带,罕达气断褶束内的兴隆-罕达气成矿带。矿床的成因类型是中高温热液矿床,矿床的工业类型是矽卡岩型。通过对矿床区域她质、成矿条件、矿区地质特征及矿床成因研究,认为该区找矿前景非常乐观。
Guan Tong He Heilongjiang copper-tungsten deposit is a new point in recent years, there are new economic value of the deposit, the deposit is located in the Greater Xing’an Mountains geosynclinal fold system, the Qaidam gas gut fold belt, Qaeda gas fold folds Xinglong - Qaeda Gas metallogenic belt. The genetic type of the deposit is high-temperature hydrothermal deposit, and the industrial type of the deposit is skarn type. Through the study of her qualities, metallogenic conditions, geological features and genesis of the deposit in the deposit area, the prospect of prospecting in the area is very optimistic.