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复兴屯金矿床位于吉南—辽东成矿带白山—老岭成矿亚带上,区域“S”型断裂带为金矿的重要控矿容矿构造,矿体赋存于老岭群珍珠门组大理岩、大理岩与大栗子组片岩接触带附近,产出形态主要受北东向、北西向断层及闪长岩脉产状控制。在总结复兴屯金矿床地质条件、地质特征、成矿规律及找矿标志的基础上,进一步指出了区域上和矿区内的找矿方向。
The Fuxingantun gold deposit is located on the Baishan-Laoling metallogenic belt in the Ji Nan-Liaodong metallogenic belt. The regional “S” -type fault zone is an important ore-controlling ore-bearing structure of the gold deposit. The ore body is hosted in the Laoling Group Near the contact zone of the pearlite, marble and big chestnut assemblage in the Pearl Gate Group, the output patterns are mainly controlled by the NE-trending, NW-trending faults and diorite veins. On the basis of summarizing the geological conditions, geological characteristics, metallogenic regularity and prospecting signs of Fuxingantun gold deposit, the prospecting direction in the area and in the mining area is further pointed out.