安徽地质2024，Vol.34Issue(1)：9-12,4.
安徽当涂后钟山铁矿成矿地质特征及矿床成因分析
Metallogenic geological characteristics and genesis of the Houzhongshan iron deposit in Dangtu,Anhui
操龙健 1洪涛涛 2费振正2
作者信息
- 1. 安徽省核工业勘查技术总院,安徽芜湖 241000
- 2. 安徽省地质矿产勘查局322地质队,安徽马鞍山 243000
- 折叠
摘要
Abstract
The Houzhongshan iron deposit is located in the northern part of the Zhonggu ore field in the south section of the Ningwu volcanic rock basin in the middle and lower reaches of the Yangtze River metallogenic belt,which is an iron deposit of hydrothermal metasomatism and filling origin.The ore bodies occur near the contact zone between dioritic porphyrite and the Huangmaqing Formation and Zhouchongcun Formation in the middle Triassic.The basement fault,intrusive contact zone and anticline structure jointly control the occurrences of the ore bodies.This paper analyzes the ore-forming geological conditions,mineralization characteristics and genesis of the deposit and discusses the prospecting direction for guiding exploration in the depth of the area.关键词
后钟山铁矿/钟姑矿田/地质特征/矿床成因Key words
Houzhongshan iron deposit/Zhonggu ore field/geological characteristics/ore genesis分类
天文与地球科学引用本文复制引用
操龙健,洪涛涛,费振正..安徽当涂后钟山铁矿成矿地质特征及矿床成因分析[J].安徽地质,2024,34(1):9-12,4.
