摘要
安徽铜陵隆起北缘是指铜陵矿集区与繁昌火山岩盆地之间的过渡地段,近年来地质找矿工作取得了明显的进展,在总结该地区的成矿作用特征的基础上,认为铜陵隆起自然向北东延伸,在繁昌火山岩盆地下部存在寻找铜陵式铜金(铁)矿床的可能性,分析了地质找矿潜力。
The north rim of the Tongling uplift refers to the transitional zone between the Tongling ore concentration area and the Fanchang volcanic basin,where remarkable progress has been made in geological and ore prospecting work during recent years.Based on a sum-up of metallogenic features in the area,it is suggested that the Tongling uplift extends northeast naturally and there is possibility for prospecting of the Tongling style copper-gold（iron） ore deposit beneath the Fanchang volcanic basin,and the ore potential is analysed.
出处
《安徽地质》
2011年第2期138-142,共5页
Geology of Anhui
关键词
铜陵隆起北缘
成矿作用
安徽
north rim of the Tongling uplift
metallogeny
Anhui
