浅谈永平铜矿边深部找矿方向  

Discussion on the direction of prospecting in the deep side of Yongping Copper Mine

作　　者：郑忠超 ZHENG Zhong-chao(Jiangxi provincial geological and mineral exploration and Development Bureau, Northeastern Jiangxi Province,Shangrao 334000,Chin)

机构地区：[1]江西省地质矿产勘查开发局赣东北大队,江西上饶334000

出　　处：《世界有色金属》2018年第3期178-179,共2页World Nonferrous Metals

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.

关 键 词：控矿构造 成矿流体 物质来源 “L型”矿体 含矿斑岩体 

分 类 号：P694[天文地球—地质学]