摘要
本文简述了前人关于永平铜矿控矿构造、成矿流体、物质来源、矿床成因及成矿规律等方面的研究成果;针对其边深部找矿,笔者提出了验证Ⅳ矿带往深部呈"L型"沿深及探索深部含矿斑岩体存在的两个方向。
This paper describes the results of previous studies on Yongping copper ore controlling structure and metallogenic fluid, material source, ore genesis and metallogenic regularity and so on; the edge of the deep prospecting, the author puts forward the verification to the Deep Ore Zone IV showed a "L" and the two directions along the deep exploration of deep ore the existence of porphyry.
作者
郑忠超
ZHENG Zhong-chao(Jiangxi provincial geological and mineral exploration and Development Bureau, Northeastern Jiangxi Province,Shangrao 334000,Chin)
出处
《世界有色金属》
2018年第3期178-179,共2页
World Nonferrous Metals
关键词
控矿构造
成矿流体
物质来源
“L型”矿体
含矿斑岩体
ore controlling structure
ore-forming fluid
material source
"L type" ore body
ore bearing pluton