赛马—柏林川碱性火山-侵入杂岩体岩浆成因
基金项目:

本文为国家自然科学基金资助项目(编号 49573181)的成果。


On Magma Origin of SaimaBailinchuan Alkaline Volcanic Intrusive Complex
单位:
  • 长春科技大学,130026    
  •    
  •    
  • Changchun University of science and technology,Changchun,130026    
  •    
  •    
  • 摘要
  • | |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • | |
  • 文章评论
    摘要:

    呈岩席产出的赛马—柏林川碱性火山侵入 杂岩体由正长岩类及响岩霞石正长岩类组成。两类岩浆来源于统一的富集地幔源区。源区中镁铁云母、单斜 辉石等的熔融生成了贫镁铁富碱铝的碱性岩浆。地幔富集作用增强生成正长质岩浆,经一个时期的间隔,从更深位的更加富集的地幔产生了响岩霞石正长质岩浆。 岩浆中有上地壳组分的参予。

    Abstract:

    The sheetliked SaimaBailinchuan alkaline vo lcanicintrusive complex consists of syenitesphonolite and nepheline syenite sTwo type s of magmas were produced from the metasomatized mantleThe maficpoor and al kalialuminumrich alkaline magmas were generated by meltng of mafic mica and clinopyroxene in the source regionThe sye nite magma was formed by enrichment in metasomatized mantle ,and the nepheline syenite magma was produced from the more enriched mantle after a period of pause of magma activitySome of the compositions of the uppe r crust joined in the alkaline magmas

    参考文献
    相似文献
    引证文献
引用本文

谭东娟,林景仟,单玄龙.1999.赛马—柏林川碱性火山-侵入杂岩体岩浆成因[J].地质论评,45(7):474-481,[DOI].
Tan Dongjuan, Lin Jingqian, Shan Xuanlong.1999. On Magma Origin of SaimaBailinchuan Alkaline Volcanic Intrusive Complex[J]. Geological Review,45(7):474-481.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史