| 安徽蚌埠—凤阳地区铁矿床成因类型探讨 |
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| 引用本文： | 陈令财,魏士书.安徽蚌埠—凤阳地区铁矿床成因类型探讨[J].云南地质,2013(4):402-405. |
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| 作者姓名： | 陈令财 魏士书 |
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| 作者单位： | 安徽省地质矿产勘查局312地质队,安徽蚌埠233040 |
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| 摘 要： | 矿体均赋存于太古界五河群中.沉积变质型磁铁矿,含矿岩系为角闪斜长片麻岩、斜长角闪岩等.似层状透镜状产出,层控明显,航磁异常显示有较好找矿远景.
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| 关 键 词： | 磁铁矿 沉积变质型 五河群 新太古界 安徽蚌埠凤阳 |
A PROBE INTO THE GENESIS TYPE OF FE DEPOSIT IN BENGBU-FENGYANG AREA,ANHUI |
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| CHEN Ling-cai,WEI Shi-shu.A PROBE INTO THE GENESIS TYPE OF FE DEPOSIT IN BENGBU-FENGYANG AREA,ANHUI[J].Yunnan Geology,2013(4):402-405. |
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| Authors: | CHEN Ling-cai WEI Shi-shu |
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| Institution: | (Geological Team 312, Anhui Exploration Bureau of Geology ＆ Mineral Resources, Bengbu 233040) |
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| Abstract: | The ore body is in Archaeozoic Wuhe Group. It is a sedimentary metamorphic magnetite deposit. The ore - bearing rock series are composed of amphibole plagioclase gneiss, amphibolite, etc. in stratoid occur- rence, clear stratabound. The prospecting perspective is good according to the aeromagnetic anomaly. |
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| Keywords: | Magnetite Sedimentary Metamorphic Type Wuhe Group Neo - Archaeozoic Fengyang Bengbu Anhui |
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