摘要
库布苏北金矿由北、中、南3个金矿化带构成,矿化带受区域韧性剪切带库布苏大断裂两侧的韧脆性次级断裂控制。库布苏大断裂以北为野马泉地块南缘的泥盆纪火山岩浆弧带,断裂以南为老鸦泉一黄羊山弧前沉积带。库布苏北金矿化带位于野马泉火山岩浆弧中。
The kub subei gold mine is composed of three gold mineralization belts in north, middle and south, and the mineralization belt is controlled by the tough brittle secondary fracture on both sides of the kubsu fault zone. In the north of kubsu, the magma arc belt of the devonian volcano is the southern margin of the field, and the south of the fault is the prearc sedimentary belt of the old crow's spring. The kubusu north gold mineralization belt is located in the magmatic arc of the wild horse spring.
出处
《世界有色金属》
2017年第21期154-155,共2页
World Nonferrous Metals
关键词
青河县库布
苏北金矿矿区
地质特征
qinghe county kubu
Subei gold mine
Geological characteristics of
