摘要
大横路钴铜矿床主要产于老岭群大栗子组第二岩性段内。其控矿因素主要有地层、褶皱和断裂、变质作用及岩浆活动。找矿标志主要为老岭群大栗子组含炭岩系、矿化蚀变(硅化、孔雀石化、褐铁矿化、黄铜矿化)、区域化探及土壤异常(Co、Cu、N、iPb、Zn、A g等组合异常)、老岭群大栗子组中的中基性脉岩等。
The orebody of the Dahenglu Co, Cu deposit mainly occurs m tne second lithozone of Dalizi Formation, I.aoling Group. The ore--control factor shows strata, fold, fracture, metamorphism and magmatic activities. The criteria for ore prospecting are mainly carbon- bearing rock series of the Dalizi Formation of Laoling Group, mineralization (silication, malachiteize, limoniteize and pyriteize;), regional geochemical exploration and soil anomalies ( assemblage anomalies of Co, Cu, Ni, pb, Zn and Ag), and intermediate basic vein rock.
出处
《吉林地质》
2005年第4期26-31,共6页
Jilin Geology
关键词
钴铜矿床
找矿标志
控矿因素
矿体特征
Co, Cu deposit
criteria for ore prospecting
ore- control factor
characteristics of ore body