期刊文献+

辽宁宽甸绿色云母玉的宝石学特征及颜色成因探讨 被引量:6

Gemmological Characteristics and Colour Causes of Green Muscovite Jade from Kuandian,Liaoning Province
下载PDF
导出
摘要 近期,笔者获得来自辽宁东部宽甸地区的绿色玉石,为研究该样品的宝玉石学特征及其颜色成因,采用常规的宝石学鉴定方法及偏光显微镜、红外光谱仪、激光拉曼光谱仪、X射线粉末衍射仪、X射线荧光光谱仪、光纤光谱仪等测试仪器,对其进行了宝石学、矿物学、光谱学特征及主要化学成分和微量元素的研究。结果表明,该玉石的主要矿物组成为白云母,质量分数达98%以上,具鳞片变晶结构,少量的红色矿物为金红石;Cr3+类质同象替代白云母中的Al3+是该样品产生绿色的主要原因,依据国家珠宝玉石名称的标准,应将该样品定名为云母玉。 A new kind of green jade was found recently in Kuandian,Liaoning Province.In order to find out the gemmological characteristics and colour causes of the green jade,this paper investigates the gemmological characteristics,mineralogical characteristics,spectrographic characteristics,chemical compositions and trace elements of the sample by using the conventional gemmological identification methods,polarizing microscope,infrared spectrometer(FTIR),laser Raman microspectrometer,X-ray powder diffraction spectrometer(XRD),X-ray fluorescence spectrometer(XRF) and fiber optic spectrometer.The results show that the main mineral component of the sample is muscovite,with minor auxiliary mineral of rutile.The cause of its green colour is the isomorphic replacement of Cr3+ to Al3+.According to the national standard,the sample is named as muscovite jade.
出处 《宝石和宝石学杂志》 CAS 2012年第1期46-50,共5页 Journal of Gems & Gemmology
关键词 云母玉 微量元素 颜色 类质同象 宽甸 muscovite jade trace element colour isomorphism Kuandian
  • 相关文献

参考文献5

二级参考文献19

  • 1杨银成,沈刚刚,张芬英,蔡岩萍.青海省祁连绿东陵玉石矿及地质特征[J].矿产与地质,2007,21(6):662-664. 被引量:3
  • 2Brown M.2001.From microscope to mountain belt:150 year of petrology and its contribution to understanding geodynamics,particularly the tectonics of orogens[J].Journal of Geodynamies,32:115~64.
  • 3Chaplin T D,Ross N L and Reynard B.2000.A high-temperature and high-pressure Raman spectroscopic study of CaGeO3 garnet [J].Phys.Chem.Minerals,27:213~219.
  • 4Chopelas A and Serghiou G.2002.Spectroscopic evidence for pressureinduced phase transitions in diopside[J].Phys.Chem.Minerals,29:403~408.
  • 5Cliff T,Johnston and Wang S.2002.Novel pressure-induce phase transformation in hydrous layered materials [J].Geophysical Research Letters,29,NO.0,10.1029.
  • 6Domanik K D and Holloway J R.1996.The stability and composition of phengitic muscovite and associated phases from 5.5 to 11 GPa:Implication for deeply subducted sediments [J].Geochimica et Cosmochimica Acta,60(21):4 133~4 150.
  • 7Holtzet M,Solin S A and Pinnavaia T J.1993.Effect of pressure on the Raman vibrational modes of layered aluminosilicate compounds[J].Physical review,48:312~317.
  • 8Kirby S,Engdahl E R and Denlinger R.1996.Intermediate-depth intraslab earthquakes and arc volcanism as physical expressions of crustal and uppermost mantle metamorphism in subducting slabs[J].American Geophysical Union,195 ~ 214.
  • 9Lin C C.2001.High-pressure Raman spectroscopic study of Co- and Niolivines[J].Phys.Chem.Minerals,28:249~257.
  • 10Mckeown D A,Bell M I and Edgar S E.1999.Vibrational analysis of the dioctahedral mica:2M1 muscovite[J].American Mineralogist,84:1041~1048.

共引文献31

同被引文献35

引证文献6

二级引证文献15

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部