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基于相对密度和X射线粉晶衍射技术测定硬玉岩中硬玉的含量 被引量:3

A Non-destructive Measurement Method of Gem Jadeite Content in Jadeitite Based on Specific Gravity and X-ray Powder Diffraction
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摘要 硬玉岩能否命名为宝石级"翡翠",其硬玉的含量是关键参数,目前测量岩石中矿物质量分数的方法多为有损分析,难以应用于珠宝玉石检测中。本文基于硬玉岩矿物组成及其质量分数的变化,建立了一种通过测量硬玉岩相对密度获得硬玉质量分数的无损分析方法。对186件相对密度在3.30~2.88之间的硬玉岩样品采用静水称重法测试,根据相对密度范围进行分组,利用X射线粉晶衍射、人工重砂分析、电子探针、红外光谱、拉曼光谱等技术确定硬玉岩的主要矿物及其质量分数,进而统计分析硬玉质量分数与硬玉岩相对密度的线性关系。研究表明:硬玉岩的主要矿物为硬玉和杂质矿物钠长石、方沸石。随着硬玉的质量分数(wA)下降,钠长石、方沸石质量分数增加,硬玉岩实测相对密度(SG)发生相应变化,两者的线性方程为wA=1.3454×SG-3.4531(相关系数为0.9814),线性关系良好。由于本方法的硬玉岩实测相对密度近似等于理论相对密度,即可通过测量相对密度获得硬玉的质量分数,这种无损测试方法适用于相对密度在3.3~3.0,硬玉含量在95%~60%,硬玉与钠长石的质量分数之和在90%~97%之间的硬玉岩样品。 The key parameter to determine whether jadeitite can be named gem grade jadeitite ‘jadeite jade’or not is the content( the mass fraction) of jadeite in jadeitite. So far,most methods to determine the mass fraction of mineral in rock are destructive, which is not suitable in gem detection. Based on the changes of mineral composition and mass fraction of mineral in jadeitite,a non-destructive method by measuring the relative density of jadeitite was established in order to get the mass fraction of jadeite. By Static Water Density Method,186 pieces of jadeitite samples with relative densities of 3. 30-2. 88 were divided into groups according to different densities.The main mineral composition and mass fraction of minerals in jadeitite were analyzed by X-ray Powder Diffraction,Manual Heavy-sand Analysis,Electron Probe Microanalysis,Infrared Spectrometry and Raman Spectrometry. The linear relationship between the mass fraction of jadeite and the relative density of jadeitite was statisticstically analyzed. Results show that the main minerals in jadeitite are jadeite,albite,and analcite. As the mass fraction(wA) of jadeite decreases,those of albite and analcime increase,and the measured specific gravities( SG) of jadeitite change accordingly. The relationship between them is wA= 1. 3454 SG-3. 4531( r = 0. 9814),showing a good linear dependence relation. Because the measured specific gravity of jadeitite is approximately equal to the theoretical one,mass fraction of jadeite is obtained by measuring the specific gravity of jadeitite. This nondestructive method applies to jadeitite with a specific gravity of 3. 3-3. 0,jadeite content of 95%-60%,and sum mass fractions of jadeite and albite of 90%-97%.
出处 《岩矿测试》 CAS CSCD 北大核心 2015年第2期207-212,共6页 Rock and Mineral Analysis
关键词 硬玉岩 翡翠 矿物组分 相对密度 X射线粉晶衍射法 电子探针 红外光谱法 拉曼光谱法 jadeitite jadeite jade mineral composition specific gravity X-ray Powder Diffraction Electron Probe Infrared Spectroscopy Raman Spectroscopy
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参考文献25

  • 1Shi G H, Harlow G E,Wang J,et al. Mineralogy ofJadeitite and Related Rocks from Myanmar : A Reviewwith New Data [ J ], European Journal of Mineralogy,2012,24=345 -370.
  • 2Marroni M, Pandolfi L, Principi G, et al. DeformationHistory of the Eclogite- and Jadeitite-bearing Melangefrom North Motagua Fault Zone, Guatemala : Insights inthe Processes of a Fossil Subduction Channel [ J ].Geological Journal, 2009,44 : 167 - 190.
  • 3Harlow G E. Jadeitites,Albitites and Related Rocks fromthe Motagua Fault Zone [ J ]. Journal of MetamorphicGeology,1994,12:49-68.
  • 4Shigeno M,Mori Y,Nishyama T. Reaction Microtexturesin Jadeitites from the Nishisonogi Metamorphic Rock,Kyushu,Japan [ J ]. Journal of Mineralogical andPetrological Sciences ,2005 ,100 :237 - 246.
  • 5Sorensen S, Harlow G E, Rumble D. The Origin ofJadeitite-forming Subduction-zone Fluids : CL-guidedSIMS Oxygen-isotope and Trace-element Evidence [ J ].American Mineralogist ,2006,91:979 -996.
  • 6何为.翡翠及其过渡类型的矿物学特征研究[D].上海:华东理工大学,2011.
  • 7邹泽李,胡林玉,殷小玲.与翡翠伴生钠长石的矿物学特征研究[J].超硬材料工程,2013,25(1):57-62. 被引量:3
  • 8陈秀英,袁心强,林嵩山.危地马拉紫色翡翠的矿物组成特征及意义[J]岩石矿物学杂志,2011.30(Supp):1-7.
  • 9黄德晶,熊威.与翡翠伴生的含钠长石质玉石的鉴别及定名探讨[J].山东国土资源,2011,27(5):17-19. 被引量:5
  • 10周艳,刘嵘,曹姝旻.关于翡翠研究中几个重要问题的思考[J].岩石矿物学杂志,2009,28(1):87-92. 被引量:2

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