| 宁陕县南付家河磁铁矿地质特征及成因分析 |
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| 引用本文： | 李革委,王创新,苏会平.宁陕县南付家河磁铁矿地质特征及成因分析[J].陕西地质,2014(1):44-49. |
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| 作者姓名： | 李革委 王创新 苏会平 |
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| 作者单位： | 陕西省地矿局西安地质矿产勘查开发院,西安710100 |
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| 摘 要： | 南付家河磁铁矿地处南秦岭被动陆缘菜子坪—柞水推覆岩片带内,近矿围岩为一套钠长岩,泥盆系发育的同沉积断层控制了矿体的空间位置,矿床成因属热水喷流沉积型。
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| 关 键 词： | 南付家河磁铁矿 同沉积断层 隐爆震碎作用 热水喷流沉积 |
GEOLOGY AND METALLOGENESIS OF THE FUJIAHE MAGNETITE DEPOSIT IN THE SOUTH OF NINGSHAN COUNTY |
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| Li Ge-wei,Wang Chuang-xin,Su Hui-ping.GEOLOGY AND METALLOGENESIS OF THE FUJIAHE MAGNETITE DEPOSIT IN THE SOUTH OF NINGSHAN COUNTY[J].Geology of Shaanxi,2014(1):44-49. |
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| Authors: | Li Ge-wei Wang Chuang-xin Su Hui-ping |
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| Institution: | ( Xi＇ an Exploration and Development Institute of Geology and Mineral Resources, Xi＇ an 710100 ) |
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| Abstract: | The south Fujiahe magnetite deposit occurs in the nappe rock sheet zone from Caiziping to Zhashui at the passive margin of southern Qinling Mountains, in which the near ore wall rock is a set of albitite and the synsedimentary fault controls spatial distribution of ore bodies. The metallogenesis should be of hydrofhermal exhalative sedimentary type. |
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| Keywords: | the south Fujiahe magnetite deposit synsedimentary fault hidden explosive fragments hydrothermal exhalative sedimentation |
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