摘要
本文在野外地质详查工作及室内综合研究整理的基础上,对横峰县焦岭铅锌矿成矿地质背景、矿体地质特征等进行了阐述,认为本矿体属燕山期花岗岩侵入后期热液成因。
On the basis of detailed field geological investigation and indoor comprehensive research,this paper expounds the metallogenic geological background and geological characteristics of Jiaoling lead-zinc mine in Hengfeng County,and holds that this ore body belongs to hydrothermal origin in late Yanshanian granite intrusion.
作者
朱炜民
罗振辉
林海辉
ZHU Wei-min;LUO Zhen-hui;LIN Hai-hui(Jiangxi Nonferrous Geological Exploration team 1,Yingtan 335003,China)
出处
《世界有色金属》
2020年第17期67-69,共3页
World Nonferrous Metals
关键词
地质特征
铅锌矿
矿床成因
geological characteristics
Lead-zinc mine
Genesis of deposit