| 福建省仙游县东湖伟晶岩矿床地质特征及成因分析 |
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| 引用本文： | 陈向东. 福建省仙游县东湖伟晶岩矿床地质特征及成因分析[J]. 华南地质与矿产, 2008, 18(1): 59-64 |
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| 作者姓名： | 陈向东 |
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| 作者单位： | 仙游县国土资源局矿产资源管理站,福建,仙游,351200 |
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| 摘 要： | 东湖伟晶岩矿床为花岗质完全分异式伟晶岩类型；该矿床是由深部岩浆经多期多阶段演化分异形成的伟晶岩浆热液，在区域NE向张性构造应力的作用下，再次侵位到早期侵入岩体后经缓慢结晶而成的。
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| 关 键 词： | 东湖伟晶岩矿床 地质特征 矿床成因 福建省 |
| 文章编号： | 1007-3701(2008)01-0059-06 |
| 修稿时间： | 2007-09-06 |
Geological characteristics of Donghu pegmatite deposit of Xianyou county in Fujian province and genetic analysis |
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| CHEN Xiang-dong. Geological characteristics of Donghu pegmatite deposit of Xianyou county in Fujian province and genetic analysis[J]. Geology and Mineral Resources of South China, 2008, 18(1): 59-64 |
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| Authors: | CHEN Xiang-dong |
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| Affiliation: | CHEN Xiang - dong ( Mineral Resource Management Office of Territorial Resource Department Jn Xianyou County, 351200 Xianyou Fujian) |
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| Abstract: | Donghu pegmatite deposit is characterized by granitic and completely differential pegmatite. Under the tectonic stress with direction of NE, the pegmatite magma hydrotherm was formed with the multi - periodic evolution of the deep - seated magma, crystallized slowly to have become the pegmatite deposit. |
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| Keywords: | Donghu pegmatite deposit geological characteristics genesis of deposit Fujian Province |
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