摘要
马滴达北山金铜矿床产于下古生界五道沟群地层与燕山期英云闪长岩(斑)岩接触带岩体一侧,矿化类型为硅化蚀变岩型,主矿体产在岩体的NW向断裂及裂隙构造中,矿床成因为次火山类型。
Madida north hill gold-copper deposit originated in the one side of contact zone between Lower Paleozoic Wudaogou Group stratum and Yanshanian tonalite.The mineralization type belongs to Silicified alteration rock type.Main orebody was located in the NW strike fracture and fissure structure,the deposit is subvolcanic.type in genesis.
出处
《吉林地质》
2012年第4期41-44,共4页
Jilin Geology
关键词
马滴达金铜矿
地质特征
次火山类型
Madida gold-copper deposit
geological features
subvolcanic type
