地质找矿论丛2012，Vol.27Issue(2)：180-185,6.DOI:10.6053/j.issn.1001-1412.2012.02.007
河南省舞阳铁矿田岗庙刘铁矿床的地质特征及构造控矿分析
Geological features and ore-controlling structural analysis of Gangmiaoliu iron deposit in Wuyang iron ore field, Henan
摘要
Abstract
This article summarizes the geological features of Gangmiaoliu iron deposit, such as stratigraphy, structure, orebodies and ore, and analyses the ore-controlling structure. The deposit is a sedimentary metamorphic iron ore deposit. The ore-bearing rock series is located between the upper and lower mig-matite member of Neo-archean Tieshanmiao formation. Spatially, the deposit is strictly controlled by the graben and horst fault blocks. The ancient erosion surface, the unconformity caused only complete oxidation of ore in the central ore block and has no major impact on the eastern and western blocks. This article can be used to the integrated exploration of the southeast Wuyang iron ore field.关键词
岗庙刘铁矿床/地质特征/控矿构造/地垒/地堑/舞阳铁矿田/河南省Key words
Geological features/ ore-controlling factors/ horst/ graben/ Wuyang iron ore field/ Henan province分类
天文与地球科学引用本文复制引用
刘昭宜..河南省舞阳铁矿田岗庙刘铁矿床的地质特征及构造控矿分析[J].地质找矿论丛,2012,27(2):180-185,6.基金项目
中国地质调查局地质调查评价项目(编号:1212011120777)和河南省整装勘查项目(编号:11-Z24). （编号:1212011120777）
