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The general formula for nambulite is (Li,Na)Mn4Si5O14(OH).〔 It is named after the mineralogist, Professor Matsuo Nambu (born 1917) of Tohoko University, Japan, who is known for his research in manganese minerals.〔M. Yoshii, Y. Aoki, K. Maeda. 1972. Nambulite, a new lithium- and sodium-bearing manganese silicate from the Funakozawa mine, northeastern Japan. 2001 Mineral Data Publishing, version 1.2. ()〕 The mineral was first discovered in the Funakozawa Mine, northeastern Japan, a metasedimentary manganese ore.〔 Nambulite is formed from the reaction between a hydrothermal solution and rhodonite, and commonly creates veins in the host rock.〔(Nambulite, (Li,Na)Mn4Si5O14(OH), in the Sausar Group of rocks in Central India Journal of Mineralogical and Petrological Sciences, Volume 100, pp. 26–30, 2005 )〕 Other than a collector’s gem, however, it has little economic value. It belongs to the crystal system Triclinic-Pinacoidal (or Triclinic-Normal),〔 meaning that it has three axes of unequal length (a, b, c), all intersecting at oblique angles with each other (none of the angles are equal to 90°). It belongs to the crystal class , meaning that any point on the crystal that is rotated 360° and then completely inverted will meet with an equal (but opposite) point on the crystal (see centrosymmetry).〔Dyar,M.D., Gunter, M.E., and Tasa, D.(2008) Mineralogy and Optical Mineralogy. Mineralogical Society of America, 77-78.〕 It’s space group is P . The three axes (a, b, c) have different indices of refraction, na=1.707, nb=1.710, nc=1.730.〔〔 The index of refraction (RI) can be defined as n = cair/cmineral, where “n” is the index of refraction and “c” is the speed of light. The maximum birefringence is .023, the difference between the highest (nc=1.730) and lowest (na=1.707) indices of refraction within the mineral. In a medium with an index of refraction equaling 1.53, Nambulite has a calculated relief of 1.71-1.73, giving it a moderate to high relief. Relief is a measure of the difference between the index of refraction of the mineral and that of the medium (often Canada balsam or other epoxy with an RI of around 1.53-1.54).〔Klein, C., and Barbara D. (2002) The Manual of Mineral Science. 23rd edition. 289-296 p. John Wiley and Sons, Inc. Hoboken, New Jersey, U.S.A.〕 Nambulite is an ''anisotropic'' crystal, where the velocity of light that passes through the crystal varies depending on the crystallographic direction. In contrast, an ''isotropic'' crystal includes all isometric crystals, and the velocity of light is equal in all directions.〔 The mineral exhibits slight pleochroism.〔(Hanfbook of Mineralogy )〕 Pleochroism is an optical property observed when the mineral is viewed under the microscope in plane polarized light, and when it the stage of the microscope is rotated the observed colors change. The color change is due to different wavelengths being absorbed in different directions, and the color of the mineral depends on the crystallographic orientation.〔 ==References== 抄文引用元・出典: フリー百科事典『 ウィキペディア（Wikipedia）』 ■ウィキペディアで「Nambulite」の詳細全文を読む スポンサード リンク
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