广东省罗定市朝罗洞金多金属矿区地质特征及成矿规律

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英文篇名：Geological characteristics and metallogenic regularity of Jinduo metal deposit in Chaoluodong, Luoding City, Guangdong Province 作者：邓英健 英文作者：DENG Ying-jian;Guangdong Nuclear Industry Geological Exploration Institute; 关键词：罗定 ; 金属矿区 ; 地质特征 ; 成矿规律 英文关键词：Luoding;;metal mining area;;geological characteristics;;metallogenic regularity 中文刊名：COLO 英文刊名：World Nonferrous Metals 机构：广东省核工业地质调查院; 出版日期：2019-04-26 09:47 出版单位：世界有色金属 年：2019 期：No.519 语种：中文; 页：COLO201903050 页数：2 CN：03 ISSN：11-2472/TF 分类号：98-99

摘要

广东省罗定市朝罗洞金多金属矿区位于罗定盆地西北部,广宁～罗定断裂的南端,贵子弧形断裂的北部,区域岩浆活动频繁,构造发育,分布有大面积的云开群地层,岩性主要以片岩,片麻岩为主,区域上金矿点众多,金成矿条件优越。
        Chaoluodong gold polymetallic mining area in Luoding City, Guangdong Province is located in the northwest part of Luoding Basin, the southern end of Guangning-Luoding fault and the northern part of Guizi arc fault. The regional magmatic activity is frequent, the structure is developed, and there are large areas of Yunkai Group strata. The lithology is dominated by schist and gneiss. There are many gold deposits in the region, and the gold metallogenic conditions are superior.

引文

[1]广东省区域地质志(M).北京:地质出版社,1988.
    [2]广东省罗定市朝罗洞金多金属矿区预查成果报告.广东省核工业地质调查院.