辽宁宽甸万宝村铜金钼矿地质特征及找矿方向  

GEOLOGICAL CHARACTERISTICS AND PROSPECTING DIRECTION OF THE WANBAOCUN CU-AU-MO DEPOSIT IN KUANDIAN, LIAONING PROVINCE

作　　者：孙武国[1] 刘冰[1] 廉涛[1] 

机构地区：[1]辽宁省第七地质大队,辽宁丹东118003

出　　处：《地质与资源》2014年第5期446-449,共4页Geology and Resources

摘　　要：辽宁宽甸万宝村铜金钼矿位于燕山期石柱子花岗闪长岩体与寒武纪碳酸盐岩地层的接触带内,受北东向与北西向构造共同控制.矿体赋存于北西向构造带内,呈雁行式排列.北西向构造控制了石柱子花岗闪长岩的侵位,同时控制了夕卡岩矿体的形成与分布.恢复夕卡岩矿区的构造形迹,特别是早期控制岩浆侵位的隐伏构造带,对夕卡岩地区找矿具有指导意义.The Wanbaocun Cu-Au-Mo deposit in Kuandian County, Liaoning Province, located in the contact zone between the Yanshanian Shizhuzi granodiorite and Cambrian carbonate rock, is jointly controlled by NE-and NW-trending faults. The ore bodies lie in the NW-trending structural belt in en echelon arrangement. The NW structure controls the emplacement of Shizhuzi granodiorite, as well as the formation and distribution of skarn orebodies. It is significant for further prospecting to recover the structural features in the skarn area, especially the buried early structural belts that controlled the magma intrusion.

关 键 词：铜金钼矿 夕卡岩 找矿方向 辽宁宽甸 万宝村 

分 类 号：P618.51[天文地球—矿床学] P618.41[天文地球—地质学]