蕉坪铁多金属矿床成矿地质特征及成因探讨

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英文篇名：Discussion on metallogenic geological characteristics and genesis of the Pingping iron polymetallic deposit 作者：黎明 英文作者：LI Ming;292 Brigade of Guangdong Nuclear Industry Geological Bureau; 关键词：蕉坪 ; 铁多金属矿床 ; 成矿地质特征 ; 矿床成因 英文关键词：Jiaoping;;iron polymetallic deposit;;metallogenic geological characteristics;;genesis of the deposit 中文刊名：世界有色金属 英文刊名：World Nonferrous Metals 机构：广东省核工业地质局二九二大队; 出版日期：2019-07-09 16:40 出版单位：世界有色金属 年：2019 期：09 语种：中文; 页：146-147 页数：2 CN：11-2472/TF ISSN：1002-5065 分类号：P618.2

摘要

蕉坪矿床位于华南褶皱系东南部的闽南、粤东铁矿带内,矿床以Fe为主,伴生Cu、Mo等多金属。本文根据近几年来广东省核工业地质局二九二大队在蕉坪铁多金属矿区找矿成果,从区域成矿地质背景入手,研究了蕉坪矿床成矿地质特征和矿体主要特征,对矿床成因作了初步探讨。
        The Jiaoping deposit is located in the southern Fujian and Eastern Guangdong iron ore belts in the southeastern part of the South China fold system. The deposit is dominated by Fe, accompanied by Cu, Mo and other metals. Based on the prospecting results of 292 brigade of Guangdong Nuclear Industry Geological Bureau in Jiaoping Iron Polymetallic Mine in recent years, starting from the regional metallogenic geological background, this paper studies the metallogenic geological characteristics and main ore body characteristics of Jiaoping deposit, and makes a preliminary discussion on the genesis of the deposit.

引文

[1]郑昌能，欧阳玉飞，王涌泉.广东连平大顶铁矿床地质特征及成因探讨[J]，甘肃冶金.2009(1).
    [2]广东省核工业地质局二九二大队，广东省东源县蕉坪铁多金属矿普查阶段性总结报告[R].2017.