Research Lab. Report 2004.04.25
Ruby in Fuchsite
Gemmological Association of All Japan Research Laboratory
Ahmadjan ABDURIYIM (Ph.D.-Min), Hiroshi KITAWAKI (FGA, CGJ)
  Ruby in zoisite is commonly known as an ornamental material of a rock containing ruby. Other materials such as ruby in anorthite-pargasite-picotite from Myanmar (Karl Schmetzer, 2003), ruby in feldspar-mica from Siberia (Grygoriev, 2000) and ruby in kyanite (Elisabeth, Strack, 1993) are also reported.
Recently we had a chance to examine ruby in a translucent to opaque rock shown in the photo.
Our analysis showed that the object was ruby in muscovite (fuchsite) containing high concentration of chromium(Cr). This study describes its detail.

Photo-1: Ruby in fuchsite.

œ Sample and Analysis
  Two pieces of the material, one bead (47.57g) and one cabochon (7.079ct) were examined in this study. According to Mr. Minoru KAMEYAMA of Miyuki Co.Ltd., who contributed the samples, these were newly discovered in Mysory district in the south India.
The samples were analysed by an X-ray analytical microscope (JSX-3600), an X-ray powder diffraction system (XRD-6000) and a Raman spectroscope (RENISHAW 1000) to distinguish each mineral phases. With the X-ray analytical microscope, the samples were measured on 90, 200, 50 and 10 points, i.e., 350 points in total, on the surface in white, green, red and brown parts of matrix respectively, using an X-ray beam converged in 50 ƒΚm which was selected by a micro collimator. Three-dimensional chemical composition mapping that can be observed from any direction was also figured out by making the two-dimensional composition mapping in wide area of 7~7 mm. Each part of different colour was powdered to be analysed on an X-ray powder diffraction system and each variety was searched by the data obtained. Also each part of different colour in appearance was analysed by a Raman spectroscope using an Ar-ion laser of 488nm.

œ Results of Analysis

X-ray fluorescence analysis and X-ray powder diffraction analysis
  The area of differently coloured mineral phases in appearance that were analysed by an X-ray analytical microscope was shown in Photo-2.

ž gray-green to green, transparent to translucent matrix: Cr-containing muscovite (fuchsite)
ž colourless transparent to white translucent matrix: muscovite and quartz
ž red transparent to translucent inclusion: ruby
ž brown transparent to translucent inclusion: rutile
The area analysed by an X-ray analytical microscope and the area of chemical composition mapping.

  As you can see in the analysis results in Table-1, the matrix of aggregated crystal was composed of different mineral phases, one is gray-green to green and the other is colourless to white. Large part of the matrix is gray-green to green, transparent to translucent muscovite (fuchsite) containing high concentration of Cr, and has composition of Al2O3F35.59`42.73wt%ASiO2F47.4`54.0wt%AK2OF 8.89`11.12wt%ANa2OF0.09`2.02wt% within the all measurement value. It contains trace elements such as Fe, Ti, Cr, Rb and Sr, and the content of Cr2O3 reaches to 0.22`0.29wt%. It also shows high concentration of TiO2 (0.28`2.55wt%) because large amount of minute brown rutile inclusions are contained in the matrix. In green area, Cr content tends to rise and Ti content tends to reduce as the colour hue becomes brighter. From the results of compositional analysis in Table-1, its chemical formula is expressed as K0.9Na0.1(Al,Cr)3Si3O10(OH)2. This muscovite variety with high concentration of Cr is called fuchsite, among which high quality material from Minas Gerais mine in south east Brazil and Wolfefs Neck metamorphic belt in Maine, USA, can be a simulant of jadeite.
  White area composing a part of matrix consists of Si-rich muscovite, in which SiO2 value shows wide range of 51.89`80.89wt%. Microcrystalline quartz crystals are mixed in this matrix, which can be confirmed by data obtained by X-ray powder diffraction system. Contents of Al and K tend to reduce as Si content becomes rich. Fe and Ti of under 1wt% are contained as impurities, but Cr content is almost too low to be detected. Very few amount of Ba was detected.
  Red part is corundum, that is, ruby, and has wide range of Cr2O3 content 0.25`0.6wt% and low contents of Fe2O3F0.15wt% and Ga2O3F0.002wt% or lower. Other trace transition metal elements such as Ti, V and Mn were not detected.
  Brown crystal was rutile, containing small amount of V and Fe as impurities.
  Each matrix and inclusion described above can be confirmed on a microscopic Raman spectroscope. Green matrix consisted of minute crystal aggregation, which made the Raman spectrum rather weak and the identification of muscovite was difficult.
Examples of composition measurement in areas of different colour by X-ray fluorescence analysis. (-):undetected

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