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硅铍石的包裹体及其形成条件研究

高诗佳 白峰

岩石矿物学杂志2013,Vol.32Issue(2):180-188,9.
岩石矿物学杂志2013,Vol.32Issue(2):180-188,9.

硅铍石的包裹体及其形成条件研究

A study of the inclusions in phenakite and the formation conditions of phenakite

高诗佳 1白峰1

作者信息

  • 1. 中国地质大学珠宝学院,北京100083
  • 折叠

摘要

Abstract

The formation conditions of phenakite were studied through investigating its gas-liquid inclusions by means of Laser Raman spectrum analysis and microscopic heating/cooling stage. The observation of phenakite samples revealed numerous randomly-distributed yellow acicular transparent solid inclusions, a few red granular opaque solid inclusions, lots of gas-liquid inclusions and healed cracks. The gas-liquid inclusions in phenakite were divided into two types according to their forms and substances. Type I included rich liquid two-phase H2O-NaCl inclusions (Ⅰa) and pure liquid H2O-NaCl inclusions ( Ⅰ b), whereas Type Ⅱ could be further divided into three-phase H2O-NaCl-CO2) inclusions containing liquid CO2( Ⅱ a) and two-phase H2O-NaCl-CO2 inclusions without liquid CO2 (Ⅱ b). Then some gas-liquid inclusions of different types with clear demarcated gas part and liquid part were chosen to do further test. Using Laser Raman spectrum analysis, the authors affirmed that phenakite is a kind of silicate which contains Be as the matrix for inclusions, and that the gas part of the gas-liquid inclusions contain such components as CO2 and water vapor, whereas the liquid part is NaCl aqueous solution with the dissolution of a little CO2. Two different gas-liquid inclusions were chosen for microscopic heating/ cooling stage test, and the results show that the homogenization temperatures of the inclusions are from 378. 9℃ to 425.5℃ by homogenization method, and their freezing points are about - 12.1 ~-6.3℃ by freezing method. These data were used to figure out the salinities of these inclusions, which are 9.60% ~16.14%. Calculations show that the homogenization pressures range from 234.44 MPa to 428.56 MPa. The formation temperature and the formation pressure of phenakite estimated from homogenization temperature and homogenization pressure are about 378.9~425.5℃ and 234.44~428.56 MPa respectively.

关键词

硅铍石/包裹体/形成温度/形成压力

Key words

phenakite/ inclusions/ formation temperature/ formation pressure

分类

天文与地球科学

引用本文复制引用

高诗佳,白峰..硅铍石的包裹体及其形成条件研究[J].岩石矿物学杂志,2013,32(2):180-188,9.

岩石矿物学杂志

OA北大核心CSCDCSTPCD

1000-6524

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