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伊春-延寿成矿带处于华北板块、西伯利亚板块和古太平洋板块之间的构造叠加部位,是中国东北地区松辽地块的重要组成部分,翠宏山矿床位于伊春-延寿成矿带北段的五星-关松镇中间隆起带,是该成矿带上重要的矽卡岩型Fe-Mo-W多金属矿床,主要分为翠宏山、翠南和翠中三个矿段。区内出露的地层主要为下寒武统铅山组(?1q),局部出露少量上二叠统五道岭组(P3w)。矿区花岗质侵入岩发育,其中,白岗质碎裂花岗岩和花岗闪长岩在地表和近地表分布,呈岩株或岩枝状产出的黑云母花岗
The Yichun-Yanshou metallogenic belt is located at the superimposed position between the North China Plate, the Siberia Plate and the Paleo-Pacific Plate and is an important part of the Songliao block in northeastern China. The Cuihongshan deposit is located in the north of Yichun-Yanshou metallogenic belt The five-star section of Guanghong, the middle uplift belt, is an important skarn-type Fe-Mo-W polymetallic deposit on the metallogenic belt. It is mainly divided into three ore sections of Cuihongshan, Cui Nan and Cui Zhong. The strata exposed in this area are mainly the Lower Cambrian Qianshan Formation (~ 1q) and a small amount of Upper Permian Wudaoling Formation (P3w). The granitic intrusive rocks in the mining area are developed. Among them, the Baigang Fragmentation Granite and the Granodiorite are distributed on the surface and near the surface, with biotite granite