摘要
Shenglitun molybdenum deposit was a concealed deposit related to skarn 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.16 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-nickel polymetallic metallogenic belt of Yantongshan-Heishi Town.