| 山西省灵丘小青沟-流砂沟银锰多金属矿床特征及矿床成因研究 |
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| 引用本文： | 高昊.山西省灵丘小青沟-流砂沟银锰多金属矿床特征及矿床成因研究[J].地质找矿论丛,2004,19(2):87-91. |
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| 作者姓名： | 高昊 |
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| 作者单位： | 山西省地勘局,二一七地质队,山西,大同,037008 |
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| 摘 要： | 小青沟-流砂沟银锰矿床为中低温热液矿床,其锰矿经氧化淋滤富集成氧化锰矿床.燕山期火山作用为其提供了热源.五台群变质岩和长城系高于庄组作为银锰多金属矿源层.
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| 关 键 词： | 成因 次火山岩-热液 长城系含锰建造 小青沟-流砂沟银锰矿 山西省 |
| 文章编号： | 1001-1412(2004)02-0087-05 |
| 收稿时间： | 2003/9/8 0:00:00 |
| 修稿时间： | 2003年9月8日 |
CHARACTERISTICS OF XIAOQINGGOU Ag, Mn POLYMETAL ORE DEPOSIT, LINGQIU COUNTY, SHANXI PROVINCE AND STUDY ON ITS GENESIS |
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| GAO Hao.CHARACTERISTICS OF XIAOQINGGOU Ag, Mn POLYMETAL ORE DEPOSIT, LINGQIU COUNTY, SHANXI PROVINCE AND STUDY ON ITS GENESIS[J].Contributions to Geology and Mineral Resources Research,2004,19(2):87-91. |
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| Authors: | GAO Hao |
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| Institution: | 217 Geological Team, Shanxi Geological and exploration Bureau, Datong 037008, China |
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| Abstract: | Xiaoqinggou-Liushagou Ag, Mn polymetal ore deposit is primarily a meso-epithermal deposit which was exposed to leaching and oxidation and turned into the precent Mn oxide deposit. The ore-forming heat source is Yanshanian volcanism and Gaoyuzhuang formation of precambrian group, the source bed suppied ore materials. |
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| Keywords: | genesis subvolcanic hydrothermal fluid Mn-bearing formation of Changcheng series Xiaoqinggou-Liushagou Ag-Mn polymetal ore Shanxi province |
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