摘要
清明山铜多金属矿位于闽西北隆起带北东缘,北武夷成矿亚带中,同时又地处北西向宁德~浦城断裂带与北东向武夷山~泰宁断裂带交汇部位。在1:20万江西省上饶地区广丰幅区域地质矿产报告中,把该区划为Ⅰ级找矿远景区。金属及非金属矿产资源十分丰富,是目前矿产勘查中的重点研究区域。针对成矿带中清明山铜多金属矿,对其地质特征从地层、岩浆岩、构造等多方面进行研究,并找出该地区控矿的主要地层因素、构造因素、岩浆岩因素及蚀变因素等,对今后指导该地区铜多金属矿的找矿工作具有重要的意义。
Qingmingshan copper polymetallic deposit is located in the northeast edge of the northwest Fujian uplift belt and the North Wuyi metallogenic sub belt.At the same time,it is also located at the intersection of the northwest Ningde Pucheng fault zone and the Northeast Wuyishan Taining fault zone.In the 1:200000 regional geological and mineral report of Guangfeng range in Shangrao area,Jiangxi Province,this area is divided into class I prospecting prospect.Metallic and non-metallic mineral resources are very rich,which is the key research area in mineral exploration at present.Aiming at the qingmingshan copper polymetallic deposit in the metallogenic belt,this paper studies its geological characteristics from the aspects of stratum,magmatic rock and structure,and finds out the main stratigraphic factors,structural factors,magmatic rock factors and alteration factors,which is of great significance to guide the prospecting of copper polymetallic deposits in this area in the future.
作者
周城
黄璟
饶健
ZHOU Cheng;HUANG Jing;RAO Jian(Jiangxi Nonferrous Geological Exploration Team 4,Jingdezhen 333001)
出处
《世界有色金属》
2021年第23期89-91,共3页
World Nonferrous Metals
关键词
成矿带
铜多金属矿
地质特征
metallogenic belt
Copper polymetallic ore
Geological characteristics
