缅甸硬玉岩中硬玉矿物的结构水表征
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金资助项目(41272049)


The constitutional water of jadeite minerals in jadeitite from Myanmar
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    本文介绍了名义上无水的辉石族矿物中结构水的研究现状,特别是硬玉矿物的结构水红外表征和含量。且笔者以缅甸硬玉岩为研究对象,使用显微红外光谱、电子探针等测试手段,从微观角度研究其中硬玉矿物的结构水表征。研究结果表明:缅甸硬玉岩中硬玉矿物的结构水在红外光谱中主要表征为3 610~3 620 cm-1和3 540~3 550 cm-1两个区域的吸收峰,且结构疏松的硬玉岩中硬玉矿物的结构水含量呈现外侧多中间少,结构致密的硬玉矿物的结构水含量各部位较为均一。结构水的含量差异和变化趋势可能是硬玉岩形成时板块俯冲和折返过程中的流体参与作用的结果,进一步为缅甸硬玉岩成因提供了的佐证。

    Abstract:

    This paper describes the research status of constitutional water in nominally anhydrous pyroxene group minerals, especially the FTIR characterization and content of constitutional water of jadeite in different rocks. The jadeite minerals from Myanmar were investigated by using micro-FTIR and electron microprobe analysis (EPMA), and the constitutional water characterization of jadeite minerals from Myanmar was studied microcosmically. According to the results achieved, the constitutional water of jadeite minerals from Myanmar is characterized by spectral peaks in the range of 3 610~3 620 cm-1 and 3 540~3 550 cm-1 on the infrared spectra, the content of constitutional water of jadeite minerals in loose structure jade is higher on the outer side and less in the middle, and the constitutional water content in various parts of jadeite minerals with compact structure is fairly homogeneous. Content difference and change trend of constitutional water are not affected by its chemical composition, and probably result from such factors as fluid involvement in diagenesis, jade forming stage and plate subduction and exhumation process. The results achieved by the authors provide a certain basis for the genetic study of Myanmese jade.

    参考文献
    相似文献
    引证文献
引用本文

邢莹莹,2015,缅甸硬玉岩中硬玉矿物的结构水表征[J].岩石矿物学杂志,34(1):87~96. XING Ying-ying,2015,The constitutional water of jadeite minerals in jadeitite from Myanmar[J]. Acta Petrologica et Mineralogica,34(1):87~96.

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
  • 收稿日期:2014-09-02
  • 最后修改日期:2014-12-15
  • 录用日期:
  • 在线发布日期: 2015-01-20
  • 出版日期: