Journal of The Gemmological Society of Japan
Online ISSN : 2189-8413
Print ISSN : 0385-5090
ISSN-L : 0385-5090
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Displaying 1-13 of 13 articles from this issue
Articles
  • Takahiro Sato, Kazuhiro Miyagawa, Teruo Sano, Naoko Ariizumi, Shigeki ...
    2023 Volume 37 Issue 1-4 Pages 3-10
    Published: December 25, 2023
    Released on J-STAGE: January 25, 2024
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    We applied fluorescence fingerprint to various rubies, and analyzed the data by principal component analysis. As a result, it was found that three features mainly affect fluorescence fingerprint of ruby. The first is the red fluorescence around at λem=694 nm. The second is longer-wavelength fluorescence of Cr clusters around at λem=774 nm. The third is direction of optic axis. On the score plots, Myanmar and synthetic ruby stones were separated from the others. Especially fluorescence fingerprint of the Myanmar ruby was characteristically different from the others because of fluorescence of Cr clusters. It is suggested that fluorescence fingerprint of ruby is partially available to geographic origin determination.

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  • Masahiko Hayashi, Atsushi Yamazaki
    2023 Volume 37 Issue 1-4 Pages 11-12
    Published: December 25, 2023
    Released on J-STAGE: January 25, 2024
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Articles
  • Shoko Odake
    2023 Volume 37 Issue 1-4 Pages 13-19
    Published: December 25, 2023
    Released on J-STAGE: January 25, 2024
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    Raman spectroscopy is an analytical technique with many advantages such as non-destructive, quick analysis, no sample preparation, and high spatial resolution, and is routinely used by gemological laboratories for the identification of gemstones and their inclusions. This paper reviews the principle of Raman spectroscopy, details of the equipment and examples of its use in gemology.

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  • Hisao Kanda
    2023 Volume 37 Issue 1-4 Pages 20-30
    Published: December 25, 2023
    Released on J-STAGE: January 25, 2024
    JOURNAL RESTRICTED ACCESS

    This paper reviews rare types of diamond growth. It is quite popular that diamond grows from molten metal under high pressure and temperature conditions. The diamond is usually grown at a fixed temperature, but there are only a few reports that show growth morphology of diamond formed while the temperature is decreased. This paper presents growth pattens formed on diamond surfaces when the growth temperature is rapidly decreased, and diamond dendrite formed with temperature decrease at slow rates.

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