摘要
通过对皖南东至-宁国一带燕山期侵入岩的岩石学、微量元素地球化学、侵位时代的分析,探讨了其岩浆来源及演化规律。结果表明:研究区燕山期侵入岩轻、重稀土分馏程度高,铕负异常不明显,岩浆为地壳熔融作用的产物,部分岩体分离结晶作用明显。区内找矿方向宜以中、小型矽卡岩型、钨-钼矿床为主,金矿与前寒武纪地层的相对高背景有关。
Based on the analysis of petrology,trace element geochemistry and emplacement age of Yanshanian intrusive rocks from east to Ningguo in southern Anhui,the magma source and evolution law are discussed.The results show that the Yanshanian intrusive rocks in the study area have high fractionation of light and heavy rare earth elements,and the negative Eu anomaly is not obvious.The magma is the product of crustal melting,and the fractional crystallization of some rock masses is obvious.The main prospecting directions in this area are medium and small skarn and W-Mo deposits.The gold deposits are related to the relative background of Precambrian strata.
作者
侯克斌
安永梅
吴正方
HOU Ke-bin;AN Yong-mei;WU Zheng-fang(Geological Survey of Anhui Province,Hefei 230001,China;Anhui Geological Survey and Mapping Institute,Hefei 230001,China;Anhui Geological and Mineral Bureau 324 Geological Team,Chizhou 247100,China)
出处
《世界有色金属》
2019年第14期179-179,181,共2页
World Nonferrous Metals
关键词
东至-宁国地区
燕山期侵入岩
岩浆来源及演化
找矿意义
East to Ningguo area
Yanshanian intrusive rocks
magma source and evolution
prospecting significance