吉林磐石胜利屯钼矿床地质特征及其找矿前景

胜利屯钼矿是近年来在吉林磐石红旗岭地区发现的一个与矽卡岩、石英脉及花岗岩成矿作用有关的隐伏钼矿床，该矿床产于辉发河深大断裂北侧，烟筒山～红旗岭一黑石镇北西向铜镍多金属成矿带上。1-6号矿体受燕山期花岗岩和大理岩之间的接触带所控制，7—22号矿体赋存于斜长角闪片岩、斜长角闪片麻岩中，23—24号矿体赋存于花岗岩、花岗斑岩中。该矿床的发现和评价对于烟筒山～黑石镇北西向铜镍多金属成矿带的区域找矿评价具有重要意义。

Geological features and exploration prospects of Shenglitun molybdenum deposit, Panshi of Jilin Province

Shenglitun molybdenum deposit was a concealed deposit related to skam quartz vein and granite mineralization, which was found in the Jilin Panshi Hongqiling area in recent years. The deposit occurs in the NW trend copper-nickel polymetallic metallogenic belt of Yantongshan-Hongqiling-Heishi Town, on the north side of Huifa River deep fault. No. 1- 6 orebody were controlled by contact zone between Yanshanian granite and griotte, No.7-22 orebody occurs in plagioclase hornblende schist and plagioclase hornblende gneiss, No.23-24 orebody occurs in granite, granite porphyry. Discovery and evaluation of the deposit have important significance for regional prospecting evaluation of NW trend copper-ickel polymetallic metallogenic belt of Yantongshan-Heishi Town.