山东省济宁强磁异常区深部铁矿初步验证及其意义
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国家自然科学基金项目(面上项目),40672139


Deep Iron Deposit of The Jining Magnetic Anomaly Area elementary was tested and its Significance in Shandong Province
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    摘要:

    山东省济宁磁异常是一个重、磁同源体,面积大于100 km2,磁异常峰值为3800nT。钻探验证在孔深1041.57~1796.54m位置发现铁矿体,矿体总厚度74.04~220m,磁性铁平均品位15.89~25.19%。矿石类型有条带状方解磁铁石英岩和条带状磁铁石英大理岩,矿石的主要组成矿物为石英、方解石、磁铁矿、磁赤铁矿、菱铁矿。矿体产于济宁岩群浅变质岩系中,矿床特征与条带状铁建造(BIF)铁矿或鞍山式铁矿有明显区别,铁矿成因类型属与千枚岩、变质中酸性火山岩、大理岩有关的沉积变质型铁矿床。该区铁矿资源潜力巨大。

    Abstract:

    Jining magnetic anomaly in Shandong province is a consanguineous association of gravity anomaly and magnetic anomaly. The area of magnetic anomaly is greater than 100km2and the peak of anomaly is 3800 nT. Through bore test ,iron orebodies are discovered in the bore deep 1041.57~1796.54m.The orebodies thickness is 74.04~220m.Average grades of magnetic iron in the ore are 15.89~25.19%.Ore types consist of banded calcite magnetite quartzite and banded magnetite quartz marble.Mainly mineral assemblage of the ore comprise quartz,calcite,magnetite,maghemite and siderite.The orebodies indwell in epizonal metamorphic rocks of Jining group .The deposit characteristices are differ from banded iron formation(BIF) and “Anshan” type iron obviously. Genetic type of the iron belongs to metamorphosed sedimentary iron deposit,which is relevant with phyllit,metamorphic intermediate-acidic volcanic rock and marble. Potential resources of the iron deposit are huge.

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宋明春.2008.山东省济宁强磁异常区深部铁矿初步验证及其意义[J].地质学报,82(9):1285-1292.
songmingchun.2008. Deep Iron Deposit of The Jining Magnetic Anomaly Area elementary was tested and its Significance in Shandong Province[J]. Acta Geologica Sinica,82(9):1285-1292.

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  • 收稿日期:2008-07-01
  • 最后修改日期:2008-07-03
  • 录用日期:2008-07-01
  • 在线发布日期: 2008-09-17
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