| 岩浆-流体过渡和阿尔泰三号伟晶岩脉之成因 |
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| 引用本文： | 卢焕章,王中刚,李院生.岩浆-流体过渡和阿尔泰三号伟晶岩脉之成因[J].矿物学报,1996,16(1):1-7,T002. |
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| 作者姓名： | 卢焕章 王中刚 李院生 |
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| 作者单位： | 中国科学院广州地球化学研究所!贵阳，550002，中国科学院广州地球化学研究所!贵阳，550002，中国科学院广州地球化学研究所!贵阳，550002 |
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| 摘 要： | 本文对新疆阿尔泰可可托海的三号伟晶岩形成的物理化学条件、特别是流体-熔融包裹体进行了研究，证明岩浆的确可以分出热液，对于三号伟晶岩脉来说，这种热液组分主要是NaCl－CO2－H2O流体。
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| 关 键 词： | 伟晶岩 流体-熔融包裹体 岩浆-流体过渡 |
MAGMA/FLUID TRANSITION AND GENESIS OF PEGMATITE DIKE No. 3 AT ALTAY, XINJIANG |
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| Lu Huanzhang, Wang Zhonggang, Li Yuansheng.MAGMA/FLUID TRANSITION AND GENESIS OF PEGMATITE DIKE No. 3 AT ALTAY, XINJIANG[J].Acta Mineralogica Sinica,1996,16(1):1-7,T002. |
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| Authors: | Lu Huanzhang Wang Zhonggang Li Yuansheng |
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| Abstract: | This paper deals with the physico-chemical conditions under which pegmatite dike No. 3at Koktokay, Altay, Xinjiang was formed in terms of fluid-melt inclusions. The results indicatethat hydrothermal solutions can be really fractionated from magmas. As for pegmatite dike No. 3,this kind of hydrotherpal solutions is dominated by NaCl+CO2+H2O fluid. |
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| Keywords: | magma/fluid transition pegmatite fluid-melt inclusions |
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