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Information Journal Paper

Title

OPTICAL CHARACTERS, CHEMICAL COMPOSITION AND FORMATION MECHANISM OF COLORLESS SODIC AND SODIC-CALCIC AMPHIBOLES IN PIEMONTITE-QUARTZ SCHISTS FROM HIGH P-LOW T SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU, JAPAN

Pages

  135-154

Abstract

 Colorless SODIC AND SODIC-CALCIC AMPHIBOLES occur in PIEMONTITE-QUARTZ SCHISTs in the Asemi-gawa (garnet zone) and Besshi (albite-biotite zone) areas of high P-low T SANBAGAWA METAMORPHIC BELT in central Shikoku, Japan. Colorless sodic amphiboles in the Asemi-gawa area are glaucophane while colorless sodic-calcic amphiboles from the Besshi area are barroisite and magnesiokatophorite. Colorless SODIC AND SODIC-CALCIC AMPHIBOLES are richer in Mg and poorer in Fe in comparison with the colored SODIC AND SODIC-CALCIC AMPHIBOLES from the epidote-quartz schists of the same metamorphic grade. Optical characters of the glaucophanes from the Asemi-gawa area are identified by their colorless and lack of pleochroism in the a, b and g directions; ng ^ Z = 13, 2V(a) = 20 and b = Y. Optical characters of magnesiokatophorite from the Besshi area are: colorless and without pleochroism in the a, b and γ directions; ng ^ Z =17, 2V(a) = 25 and b=Y. Chemical composition of the coexisting minerals with colorless SODIC AND SODIC-CALCIC AMPHIBOLES have shown a very high oxygen fugacity condition in which iron exists only as Fe3+ and occurs mostly in hematite.  Therefore, such condition was responsible for formation of SODIC AND SODIC-CALCIC AMPHIBOLES which are very rich in Mg.

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    APA: Copy

    IZADYAR, J.. (2005). OPTICAL CHARACTERS, CHEMICAL COMPOSITION AND FORMATION MECHANISM OF COLORLESS SODIC AND SODIC-CALCIC AMPHIBOLES IN PIEMONTITE-QUARTZ SCHISTS FROM HIGH P-LOW T SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU, JAPAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 13(1), 135-154. SID. https://sid.ir/paper/3785/en

    Vancouver: Copy

    IZADYAR J.. OPTICAL CHARACTERS, CHEMICAL COMPOSITION AND FORMATION MECHANISM OF COLORLESS SODIC AND SODIC-CALCIC AMPHIBOLES IN PIEMONTITE-QUARTZ SCHISTS FROM HIGH P-LOW T SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU, JAPAN. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2005;13(1):135-154. Available from: https://sid.ir/paper/3785/en

    IEEE: Copy

    J. IZADYAR, “OPTICAL CHARACTERS, CHEMICAL COMPOSITION AND FORMATION MECHANISM OF COLORLESS SODIC AND SODIC-CALCIC AMPHIBOLES IN PIEMONTITE-QUARTZ SCHISTS FROM HIGH P-LOW T SANBAGAWA METAMORPHIC BELT IN CENTRAL SHIKOKU, JAPAN,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 13, no. 1, pp. 135–154, 2005, [Online]. Available: https://sid.ir/paper/3785/en

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