缅甸莫西西玉——一种特殊的动力变质与交代玉石

亓利剑, 吕晓瑜, 刘卫东, 欧阳秋眉

亓利剑, 吕晓瑜, 刘卫东, 欧阳秋眉. 缅甸莫西西玉——一种特殊的动力变质与交代玉石[J]. 宝石和宝石学杂志, 2003, 5(4): 1-6.
引用本文: 亓利剑, 吕晓瑜, 刘卫东, 欧阳秋眉. 缅甸莫西西玉——一种特殊的动力变质与交代玉石[J]. 宝石和宝石学杂志, 2003, 5(4): 1-6.
QI Li-jian, LÜ Xiao-yu, LIU Wei-dong, OUYANG Qiu-mei. Maw-Sit-Sit Jade from Burma: A Particular Jade Formed by Dynamic Metamorphism and Metasomatism[J]. Journal of Gems & Gemmology, 2003, 5(4): 1-6.
Citation: QI Li-jian, LÜ Xiao-yu, LIU Wei-dong, OUYANG Qiu-mei. Maw-Sit-Sit Jade from Burma: A Particular Jade Formed by Dynamic Metamorphism and Metasomatism[J]. Journal of Gems & Gemmology, 2003, 5(4): 1-6.

缅甸莫西西玉——一种特殊的动力变质与交代玉石

详细信息
    作者简介:

    亓利剑(1956—),男,教授,地球化学专业,主要从事宝石学研究与教学工作。

  • 中图分类号: P619.28

Maw-Sit-Sit Jade from Burma: A Particular Jade Formed by Dynamic Metamorphism and Metasomatism

  • 摘要: 以缅甸莫西西玉为研究对象, 采用镜下分析、X射线粉晶衍射、电子探针、拉曼光谱、红外吸收光谱等分析测试方法, 重点对该玉石的成分、玉相和振动光谱特征进行了研究。研究表明, 莫西西玉主要由一组分布不均的富铬矿物组成, 即铬硬玉[x(Kch) 为15%~18%]、富铬氟镁钠闪石[w(Cr2O3)为4%左右]、钠长石、含铬钠长石[w(Cr2O3) 为1%左右]、钠铬辉石[x((Kch) 为62%~65%]及铬铁矿。玉石具典型的糜棱、交代网脉状及交代假象结构。在300~580cm-1拉曼位移范围内, 钠铬辉石和铬硬玉中由Cr—O和Al—O弯曲振动致拉曼谱峰, 其峰形、峰位、半高宽及振动频率均存在较明显的差异。研究结果初步证实, 莫西西玉属一种典型的由不同期次动力变质与低温热液交代作用形成的玉石。
    Abstract: Mineralogical composition, texture and vibrational spectrum and origin of Maw-sit-sit jade from Burma are studied. The testing methods of optical microscope, EPMA, X-ray powder diffraction analysis, infrared absorption spectrum and Raman spectrum are employed in the research. The results show that mineralogical composition of Maw-sit-sit jade mainly consists of chrome-jadeite[x(Kch) =15%~18%], chromian eckermannite[w(Cr2O3) =4% or so], albite, chromiferous-albite[w(Cr2O3) 1% or so], kosmochlor[w(Kch) =62%~65%], chromite, etc. The jade is formed by the dynamic metamorphism and metasomatism characterized by mylonitic, metasomatic network and metasomatic pseudomorphous textures. The shape, the location and the semi-height breadth of Raman spectra of the chrome-jadeite and kosmochlor in the range 300~580 cm-1 are closely associated with the Cr3+ concentration, and at the same time are restrained by the bend vibration of Cr-O and Al-O. The research indicates that Maw-sit-sit jade are formed by the superimposition and reformation of multistage dynamic metamorphism and low-temperature hydrothermal metasomatism.
  • [1]

    Gübelin E. Maw-sit-sit: a new decorative gemstone from Burma[J].Gems & Gemology, 1965, 11(8): 227-238.

    [2] 张蓓莉.系统宝石学[M].北京:地质出版社, 1997.257-264.
    [3] 崔文元, 王时麒, 杨富绪, 等.缅甸翡翠(辉石玉)的矿物学及其分类的研究[J].云南地质, 1998, 17(3, 4): 356-380.
    [4] 赵明开.缅甸翡翠矿物与自然类型[J].云南地质, 1998, 17(3, 4): 320-337.
    [5]

    Colombo E, Rinaudo C, Trossarelli C. The mineralogical composition of Maw-sit-sit from Myanmar[J].The Journal of Gemmology, 2000, 27(2): 87-92.

    [6] 邹天人, 於晓晋, 夏风荣, 等.翡翠的单斜辉石类矿物研究[J].宝石和宝石学杂志, 1999, 1(1): 27-32.
    [7] 欧阳秋眉.翡翠的矿物组成[J].宝石和宝石学杂志, 1999, 1(1): 18-24.
    [8] 亓利剑, 郑曙, 谭振宇.缅甸辉玉常见的种属及宝石学特征[J].珠宝科技, 1998, (10) 1:51-56.
    [9] 徐培苍, 李如壁.地学中的拉曼光谱[M].西安:陕西科学技术出版社, 1996.64-66.
    [10] 张位及.缅甸北部帕敢地区翡翠矿床地质[J].云南地质, 2002, 21(4): 378-390.
计量
  • 文章访问数:  16
  • HTML全文浏览量:  0
  • PDF下载量:  1
  • 被引次数: 0
出版历程
  • 收稿日期:  2003-10-24

目录

    /

    返回文章
    返回