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熔体包裹体在镁铁质火山岩成因研究中的应用
Melt Inclusions and Their Applications on the Origin of Mafic Volcanic Rocks

查看参考文献142篇

任钟元 1   张乐 1,2   吴亚东 1,2   徐晓波 1,2   张磊 1,2   梅盛旺 1,2   于亚锋 1,2   罗清晨 1,2   张庆霖 1,2  
文摘 熔体包裹体是矿物在生长或结晶过程中捕获的小的硅酸盐熔体,它保存了原生岩浆、岩浆演化以及源区性质等方面的重要信息。然而,全岩成分只保留了经历复杂地质过程(如分离结晶、岩浆混合、地壳混染和后期蚀变等)之后的“混合”成分,有关岩石起源方面的重要信息部分或全部消失。本文系统总结了熔体包裹体的研究方法,包括岩相学观察、挑选寄主矿物、加热均一化、镶嵌和磨制样品靶、成分分析等,介绍了熔体包裹体方法在镁铁质火山岩成因研究中一些应用实例。
其他语种文摘 Melt inclusions are small silicate melts trapped in minerals during growth or crystallization,which may preserve important information of the primary magma,process of magmatic evolution and nature of the source. In contrast,whole rock compositions only retain the "mixed" compositions after complicated geological processes,including fractional crystallization, magma mixing, crustal assimilation and alteration,during which some or all of the important information about the origin of rocks may have disappeared. This paper presents the method of melt inclusion study,including petrological observation,selection of host minerals,rehomogenization of melt inclusions,mounting and polishing melt inclusions and compositional analyses of melt inclusions. Finally,this paper also introduces some examples on the application of melt inclusions in the study of the genesis of mafic volcanic rocks.
来源 矿物岩石地球化学通报 ,2018,37(3):395-413 【核心库】
DOI 10.19658/j.issn.1007-2802.2018.37.090
关键词 熔体包裹体 ; 微区原位分析 ; 镁铁质火山岩
地址

1. 中国科学院广州地球化学研究所, 广州, 510640  

2. 中国科学院大学, 北京, 100049

语种 中文
文献类型 研究性论文
ISSN 1007-2802
学科 地质学
基金 国家自然科学基金项目
文献收藏号 CSCD:6319933

参考文献 共 142 共8页

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引证文献 7

1 丁一 熔体包裹体挥发分应用的研究进展 岩石矿物学杂志,2019,38(6):897-913
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2 周斌 四川木里混杂带海山玄武岩辉石斑晶中的熔体包裹体:甘孜-理塘古特提斯洋内热点与洋中脊相互作用的记录 岩石学报,2020,36(3):925-947
被引 5

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