| 建水黑甲铁锰矿矿床成因探讨 |
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| 引用本文： | 杜彦强,李琼仙,胡勇,董升普,马大君.建水黑甲铁锰矿矿床成因探讨[J].云南地质,2013(4):491-494. |
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| 作者姓名： | 杜彦强 李琼仙 胡勇 董升普 马大君 |
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| 作者单位： | 云南省地质矿产勘查开发局区调大队,云南玉溪653100 |
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| 摘 要： | 建水县黑甲铁锰矿赋存于第四系残坡积层中,层状、似层状分布于平缓山坡及平坦低凹处,为一套含较多铁锰质结核、残块的第四系堆积矿.
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| 关 键 词： | 残坡积型 铁锰矿 地质特征 成因探讨 云南建水黑甲 |
A PROBE INTO THE GENESIS OF HEIJIA FE-MN DEPOSIT IN JIANSHUI |
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| DU Yan-qiang,LI Qiong-xian,HU Yong,DONG Sheng-pu,MA Da-jun.A PROBE INTO THE GENESIS OF HEIJIA FE-MN DEPOSIT IN JIANSHUI[J].Yunnan Geology,2013(4):491-494. |
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| Authors: | DU Yan-qiang LI Qiong-xian HU Yong DONG Sheng-pu MA Da-jun |
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| Institution: | ( Team of Regional Geological Survey, Yunnan Exploration ＆ Development Bureau of Geology ＆ Mineral Resources, Yuxi 653100) |
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| Abstract: | Heijia Fe- Mn deposit is in Quaternary eluviat- slope wash, which is bedded, stratoid on the gentle slope and in the fiat depression. It is Quaternary accumulation ore deposit of many Fe - Mn concretions andrelict blocks. |
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| Keywords: | Eluvial - Slope Wash Type Fe - Mn Deposit Geological Feature Genesis Probe Heijia Jianshui |
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