摘要
安徽巢湖—肥东一带的铁矿床为中型规模的BIF铁矿床。本文基于已有勘查研究成果,总结归纳矿床地质特征,探讨矿床成因并进行找矿潜力分析。
The iron ore deposits around the Chaohu-Feidong area, Anhui are middle-size deposits of banded iron formation. Based on available exploration and study results, this paper summarized geological features of the deposits, discussed the origin and ore potential.
出处
《安徽地质》
2016年第4期246-250,共5页
Geology of Anhui
关键词
巢湖-肥东地区
沉积变质型铁矿
地质特征
矿床成因
找矿前景
sedimentary metamorphic iron ore deposit
geological features
ore deposit origin
mineral exploration prospective
ChaohuoFeidong area
