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J4 ›› 2014, Vol. 20 ›› Issue (2): 177-.

• 特约稿 • 上一篇    下一篇

流体包裹体岩相学的一些问题探讨

卢焕章   

  • 出版日期:2014-06-20 发布日期:2014-07-19

Fluid Inclusion Petrography:A Discussion

LU Huanzhang   

  • Online:2014-06-20 Published:2014-07-19

摘要:

流体包裹体岩相学是流体包裹体研究的基础和前提。在流体包裹体研究过程中,我们十分重视和强调选择什么样的 流体包裹体去做测温和分析。在流体色裹体岩相学中区分原生和次生包裹体十分重要。只有选择了原生流体包裹体后才能 进行显微测温学和流体包裹体成分分析。这种选择包裹体的过程(或步骤),确定流体包裹体的分类以及在显微镜下观察流 体包裹体捕获后的変化,是流体包裹体岩相学(Fluid inclusion petrography)最主要的内容。本文叙述流体包裹体岩相学的内容 和区分原生和次生流体包裹体的一些实例和方法,阐述了流体包裹体与主矿物之关系。

关键词: 流体包裹体岩相学;原生和次生流体包裹体;主矿物

Abstract:

Petrographic microscopy of a rock and mineral sample is the first and at same time essential step of any fluid inclusion study. Fluid inclusion is a paleogeofluid trapped in minerals. To distinguish the primary and secondary fluid inclusions is an essential step, then a proper interpretation of fluid inclusions can be made only when textural relationship between fluid inclusion and the host mineral and rock are considered. This is the major subject for fluid inclusion petrography. A few methods to describe the essential part of fluid inclusion petrography are included.

Key words: fluid inclusion, petrography, primary and secondary fluid inclusion, host mineral.