摘要
庐枞火山岩盆地位于长江中下游成矿带中部,一直以玢岩型铁硫矿床模型为指导进行矿产勘查,并取得一系列重要找矿成果,但区内铜金矿找矿效果一直不好,近年来庐枞火山岩盆地北部黄屯地区取得了铜金矿找矿突破,矿床类型为爆破角砾岩型,矿床规模可达中型以上。黄屯铜金矿床是该区矿床类型和铜金矿规模的重大突破,对庐枞地区进一步开展铜金矿找矿工作具有重要指导意义。
Located in the middle part of the metallogenic belt along the middle and lower reaches of the Yangtze River, the Lu-Zong volcanic basin has always been dominated by porphyrite pyrite deposit model for mineral exploration, and a series of important prospecting results have been achieved. However, a breakthrough in copper and gold prospecting did not take place until recently an explosion breccia type deposit of potentially above medium size was found in the Huangtun area of the basin. The Huangtun copper and gold deposit is a major discovery in terms of the deposit type and dimension, being significant to further copper and gold exploration in the Lu-Zong area.
作者
谢杰
张冠华
吴文龙
王彪
XIE Jie;ZHANG Guan-hua;WU Wen-long;WANG Biao(No.327 Unit,Bureau of Geology and Mineral Exploration of Anhui Province,Hefei,Anhui 230011,China;Hefei University of Technology,Hefei,Anhui 230009,China)
出处
《安徽地质》
2019年第4期254-256,264,共4页
Geology of Anhui
基金
中国地质调查局“整装勘查区找矿预测与技术应用示范”子项目“安徽黄屯地区深部矿产调查与找矿预测”(121201004000160901-10)资助。
关键词
黄屯
铜金矿床
地质特征
成因探讨
Huangtun
copper and gold deposit
geological features
genetic discussion
