摘要
著名的中南部非洲新元古代卢富里安沉积型铜-钴矿带中,不仅蕴含巨量的沉积型铜-钴矿资源,而且还发育有受沉积地层控制的变质热液型铅锌矿。这类铅锌矿化产出在碳酸盐岩中,矿床中矿化元素较复杂;矿体通常受地层和断层构造带的控制,呈筒状或块状,这与沉积型铜-钴矿完全不同。刚果(金)的Kipushi锌-(铜)-铅矿床是典型的代表。
In the world famous Lufilian sedimentary Cu-Co belt in Central African,there are not only a huge amount of sedimentary Cu-Co deposits,but also many metamorphic hydrothermal Pb-Zn deposits controlled by the sedimentary strata.This type of lead-zinc mineralization is hosted in the carbonate rock layer,the ore-forming elements are complex in the deposit.The Pb-Zn orebodies are commonly controlled by the strata and fault structures and are in tubular or massive shape,which are completely different from the sedimentary Cu-Co deposits.Kipushi Zn-(Cu)-Pb deposit is a typical representative in Congo(DRC).
作者
肖波
覃鹏
XIAO Bo;QIN Peng(NFC Africa Mining PLC,Kitwe Pox.22592,Zambia;China Nonferrous Metals(Guilin)Geology and Mining Co.,Ltd.,Guilin 541004,Guangxi,China)
出处
《矿产与地质》
2019年第4期623-627,共5页
Mineral Resources and Geology
基金
中国有色矿业集团有限公司科技项目（编号：2017KJJH11）专项经费资助
