文章摘要
王伟中,李怀乾,贾兴杰,王夏.河南舞阳铁矿田含矿岩系原岩及古环境恢复[J].矿产勘查,2015,6(4):413-419
河南舞阳铁矿田含矿岩系原岩及古环境恢复
Protolith of iron-bearing strata and restoration of plaeo environments of Wuyang iron ore deposit, Henan
  
DOI:
中文关键词: 含矿岩系  原岩恢复  沉积变质铁矿  河南舞阳
英文关键词: ore-bearing strata, restoration of protolith, metamorphosed sedimentary iron deposit, Wuyang county, Henan Province
基金项目:中国地质调查局调查评价项目(编号:1212011120777)和河南省整装勘查项目(编号:11-24)联合资助。
作者单位
王伟中 河南省有色金属地质矿产局第四地质大队,郑州 450016 
李怀乾 河南省有色金属地质矿产局第四地质大队,郑州 450016 
贾兴杰 河南省有色金属地质矿产局第四地质大队,郑州 450016 
王夏 河南省有色金属地质矿产局第四地质大队,郑州 450016 
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中文摘要:
      河南舞阳铁矿田地处河南舞阳—新蔡铁矿集区的重要区段上,已探明铁矿石资源储量超过10亿t,且仍有较大的找矿潜力。为在钻探施工过程中准确地确定所在层位,预测矿层,矿体连接时保障其准确性,根据矿物组成及其退化变质规律和沉积过程中碎屑颗粒大小及其比重差异,对含矿岩系原岩及古环境进行了恢复。笔者认为,主要含矿地层物质来源,赵案庄组为喜庄组风化剥蚀物、超基性海底火山喷发物、海洋物质的混合物;铁山庙组为喜庄组、赵案庄组风化剥蚀物、基性海底火山喷发物、海洋物质的混合物。基性、超基性火山喷发物质首先在陆地上沉积,后经搬运、分选,在潮坪环境下形成磁铁矿矿体。
英文摘要:
      The Wuyang iron ore deposit is located in the Wuyang-Xincai iron mineralization concentration area in Henan Province, and the proven iron ore reserve is more than 1 billion tons, and still there is huge potential for iron prospecting. In order to accurately determine the drilling positions, to predict the iron-bearing layer and outline the orebody precisely, the protolith of iron-bearing strata and paleo-environment were conducted according to the mineral composition, degeneration regulation, and the particle size of clasts and gravity difference of the deposition process. Based on the study, it is concluded that the main material sources of ore-bearing layers are as followings:Zhaoanzhang group material sources result from the weathered materials of Xizhuang group, subfloor ultra-basic volcanic eruption and marine substances. Tieshanmiao group source materials results from weathered materials of Xizhuang group and Zhaoanzhuang group, subfloor ultra-basic volcanic eruption and mixture of marine substances. The ultrabasic and basic volcanic eruption materials were first deposited on the land, then by transportation and differentiation, the magnetite ore deposit was formed in the flat tidal environment. 
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