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金竹坑铁矿矿床地质特征及成矿地质因素研究
引用本文:王金和.金竹坑铁矿矿床地质特征及成矿地质因素研究[J].有色金属(矿山部分),2011,63(1):30-35.
作者姓名:王金和
作者单位:福建省196地质大队,福建沙县,365500
摘    要:金竹坑铁矿具有一定的赋存层位性,在长期的构造活动背景下,含矿岩浆侵入含铁质岩层和灰岩岩层,发生接触交代作用,使成矿元素得以富集成矿。因此本区矿床类型为接触交代型铁矿床。

关 键 词:金竹坑铁矿  地质特征  地质因素  成矿元素

Study on Metallogenic Geological Factor and Geological Characteristics of Jinzhukeng Iron Deposit
Authors:WANG Jinhe
Affiliation:Fujian Provincial No.196 Geology Team, Shaxian 365500, Fujian, China
Abstract:Jinzhukeng Iron deposit have a layer of Existing, at the background of the long-term structure activity, While the magma of containing mineral invade to the strata of containing iron rock and ash rock strata, occurring on contacting explanation function, making into a mine by riching the mineral chemical element, therefore the deposit type is a Iron deposit of contacting and explaining.
Keywords:Jinzhukeng iron deposit  geological characteristic  geological factor  ore-forming element
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