安徽地质2024，Vol.34Issue(1)：13-15,24,4.
安徽芜湖赵村-刘村铁矿床地质特征及成因分析
Geological characteristics and genesis of the Zhaocun-Liucun iron deposit in Wuhu,Anhui
汪锦1
作者信息
- 1. 安徽省地质矿产勘查局327地质队,安徽合肥 230011
- 折叠
摘要
Abstract
As a part of the Yongzhen iron ore field,the Zhaocun-Liucun iron deposit was discovered through geomagnetic anomaly verification and was found to be a medium-sized one by followup mineral exploration.The iron ore bodies,lens-like to stratoid,occur near the"rock concave"of the contact zone,in the marlstone and calcareous mudstone of the Xujiashan Formation in the middle Triassic,belonging to a typical porphyritic iron deposit.The ore bodies are shallow and dominated by magnetic iron,which is easy to develop.The"rock concave"structure is the most important ore-controlling structure in this area.The magnetic anomaly plays an irreplaceable role in the discovery of iron ore and the arrangement of exploration workings.It is expected to make new progress in the peripheral and deep exploration around the deposit.关键词
赵村-刘村铁矿/地质特征/岩凹/磁异常Key words
Zhaocun-Liucun iron deposit/geological characteristics/rock concave/magnetic anomaly分类
天文与地球科学引用本文复制引用
汪锦..安徽芜湖赵村-刘村铁矿床地质特征及成因分析[J].安徽地质,2024,34(1):13-15,24,4.
