摘要
非洲刚果(金)加丹加铜钴成矿带是世界上著名的刚果(金)—赞比亚铜钴成矿带的西延部分,加丹加岩系中的罗安群是主要的含矿地层;由于褶皱和推覆构造运动,使深埋的含矿地层被推覆至地表,从而形成了沿卢菲利弧形褶皱展布的富而浅的铜钴成矿带。
Katanga copper-cobalt metallogenic belt inCongo （DRC） is western extension part of the world＇s famous Congo （DRC）-Zambia＇s copper-cobalt metallogenic belt. Roan Group of Katanga rocks is the main ore-bearing strata. Due to folds and nappe tectonics, so deeply buried ore-bearing strata were pushed to the surface cover, thus forming rich-shallow copper-cobalt metallogenic belt along fold distribution in Lufilian arch.
出处
《资源环境与工程》
2010年第2期137-140,共4页
Resources Environment & Engineering
关键词
刚果(金)加丹加
铜钴成矿带
构造特征
Katanga in Congo （DRC）
copper-cobalt metallogenic belt
structure characteristics
