首页 | 本学科首页   官方微博 | 高级检索  
     检索      

徐州峒山铁(铜)矿的成矿特征及找矿方向
引用本文:陈小华.徐州峒山铁(铜)矿的成矿特征及找矿方向[J].地质学刊,2001,25(1):17-22.
作者姓名:陈小华
作者单位:华东有色地质勘查局矿产勘查开发院!江苏南京210007
摘    要:铜山铁(铜)矿床属接触交代-高温热液型矿床,主要受闪长夺和碳酸盐地层的接触带构造控制,成矿物质来源于岩浆岩,具有典型的地面磁异常、围岩蚀变和矿化分期分期带特征,分析了矿床西部的地层、构造、岩浆岩和磁异常特点,探讨了该区的找矿方向。

关 键 词:接触带  控矿构造  磁异常  找矿方向  江苏  铜矿床  铁矿床  成矿物质  岩浆岩
文章编号:1003-6474(2001)01-0017-06
修稿时间:2001年1月19日

The Ore-forming properties and Prospect of the Iron (Copper)Deposit in Dongshan, Xuzhou
CHEN Xiao,hua.The Ore-forming properties and Prospect of the Iron (Copper)Deposit in Dongshan, Xuzhou[J].Jiangsu Geology,2001,25(1):17-22.
Authors:CHEN Xiao  hua
Abstract:Dongshan iron (copper)deposit is deemed to be a type of contact metasomatic to hydrothermal which is mainly controlled by the structures around the contact zone of dioritic porphyrite and carbonate beds with ore forming materials derived from magmatites and typical zoning features of ground magnetic anomaly, country rock alteration and mineralization phases. The characteristics of the strata, structure, magmatic rocks and magnetic anomaly in the west of the deposit are reviewed and its ore prospect is also discussed.
Keywords:Contact zone  Ore  controlling structure  Magnetic anomaly  Ore prospect  Xuzhou  Jiangsu
本文献已被 CNKI 维普 等数据库收录!
点击此处可从《地质学刊》浏览原始摘要信息
点击此处可从《地质学刊》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号