摘要
北山铅锌矿位于丹池成矿带中段北东边缘,是南岭地区典型的大型铅锌矿床之一。矿体赋存于中泥盆统东岗岭组顶部的白云岩中,受NNE走向断裂构造控制。通过与MVT矿床特征进行对比,综合分析认为,北山铅锌矿属于MVT矿床。
Beishan Pb-Zn deposit is located in the northeast margin of the middle Danchi metallogenic belt,which is one of the typical large-scale Pb-Zn deposits in Nanling area.The orebodies are hosted in dolomite at the top of Donggangling formation of Middle Devonian and controlled by NNE trending fault structure.By comparing with the characteristics of MVT deposit,Beishan Pb-Zn deposit belongs to MVT deposit.
作者
马鹏
MA Peng(School of Earth Sciences,Guilin University of technology,Guilin 541006,China)
出处
《世界有色金属》
2020年第24期93-94,共2页
World Nonferrous Metals
关键词
北山
铅锌矿床
地质特征
矿床成因
Beishan
Pb-Zn deposit
geological features
deposit genesis
