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大台沟铁矿的成因及找矿标志
引用本文:王志宏,郑娇. 大台沟铁矿的成因及找矿标志[J]. 鞍山科技大学学报, 2010, 0(4)
作者姓名:王志宏  郑娇
作者单位:辽阳县国土资源局国土资源勘测中心;中国冶金矿业鞍山冶金设计院;
摘    要:大台沟铁矿位于本溪市南郊桥头镇,距本溪市约16 km。矿床属前寒武纪硅铁质建造。通过对矿床的成矿作用、矿床地质特征的分析,提出了大台沟铁矿床的成矿机制、矿体形态、矿物共生组合、围岩蚀变等方面的矿化特征,部分揭示了大台沟铁矿床的成矿模式及找矿标志。

关 键 词:铁矿  鞍山式铁矿  成因  找矿标志  

Cause of Dataigou iron ore deposit and prospecting marks
WANG Zhi-hong,ZHENG Jiao. Cause of Dataigou iron ore deposit and prospecting marks[J]. Journal of Anshan University of Science and Technology, 2010, 0(4)
Authors:WANG Zhi-hong  ZHENG Jiao
Affiliation:WANG Zhi-hong1,ZHENG Jiao2(1.Reconnaissance Center of Land Resources Bureau,Liaoyang County,Liaoyang 111200,China,2.Anshan Metallurgical Design and Research Institue,China Metallurgical Mining Corporation,Anshan 114001,China)
Abstract:Dataigou iron ore deposit lies in bridge town of Benxi city,which is about 16 km away from Benxi city.The ore deposit belongs to ferrosilicon geology structure during the precambrian period.By the analysis of the metallogenesis and the geological feature,the mineralization features of ore body shape,mineral symbiotic combination,and wall rock alteration are proposed.It reveals the metallogenic model of Dataigou iron ore deposit and the prospecting marks.
Keywords:iron mine  Anshan iron deposit  cause  prospecting marks  
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