摘要
杨六圪卜铁矿赋存于新太古界色尔腾山(岩)群东五分子组的斜长角闪片麻岩中,矿体由磁铁石英岩组成。斜长角闪片麻岩及磁异常为直接的找矿标志。本区铁矿具有较强的磁性,可做为间接找矿标志。
The Yangliugebu Iron Ore occurs in the amphibolite gneiss of Eastern pentamolecular formation of Seltengshan(rock)group in Neoarchean and the ore body is composed of magnetite quartzite.The amphibolite gneiss and magnetic anomaly are direct indicators for deposit.The iron ore in this area is with stronger magnetic properties,so it can be as an indirect indicator for deposit.
作者
王武
赵利兵
郭延涛
Wang Wu;Zhao Li-bing;Guo Yan-tao(Baotou Steel Survey and Mapping Institute,Baotou 014010,Inner Mongolia Autonomous Region,China)
出处
《包钢科技》
2022年第1期11-13,38,共4页
Science & Technology of Baotou Steel
关键词
铁矿
矿床特征
找矿标志
iron ore
deposit characteristics
indicator for deposit
