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Information Journal Paper

Title

APPLICATION OF GARNET CHEMISTRY IN THERMODYNAMIC STUDIES OF DEHNOW TONALITE (NORTHWEST OF MASHHAD)

Pages

  253-264

Abstract

 Hornblende biotite bearing TONALITE from the west of DEHNOW comprises of quartz, calcic plagioclase (andesine-labradorite), GARNET (mostly almandine), biotite (annite to siderophyllite), calcic amphibole (mainly ferrohornblende) and accessory minerals of chlorite, epidote, calcite and ilmenite. According to thermo barometry of amphibole, plagioclase as well as the chemistry of GARNET that shows CaO content of about 4.91-5.48 wt% and MnO content of about 1.89-2.40 wt%, the GARNET in TONALITE has crystallized in the TEMPERATURE and PRESSURE range of 696 to 950°C and 6.4 to 12 kbar, respectively, and which is in a greater depth than that of amphibole and plagioclase.

Cites

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  • Cite

    APA: Copy

    SAMADI, R., MIRNEJAD, H., SHIRDASHTZADEH, N., & KAWABATA, H.. (2012). APPLICATION OF GARNET CHEMISTRY IN THERMODYNAMIC STUDIES OF DEHNOW TONALITE (NORTHWEST OF MASHHAD). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 20(2), 253-264. SID. https://sid.ir/paper/4118/en

    Vancouver: Copy

    SAMADI R., MIRNEJAD H., SHIRDASHTZADEH N., KAWABATA H.. APPLICATION OF GARNET CHEMISTRY IN THERMODYNAMIC STUDIES OF DEHNOW TONALITE (NORTHWEST OF MASHHAD). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2012;20(2):253-264. Available from: https://sid.ir/paper/4118/en

    IEEE: Copy

    R. SAMADI, H. MIRNEJAD, N. SHIRDASHTZADEH, and H. KAWABATA, “APPLICATION OF GARNET CHEMISTRY IN THERMODYNAMIC STUDIES OF DEHNOW TONALITE (NORTHWEST OF MASHHAD),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 20, no. 2, pp. 253–264, 2012, [Online]. Available: https://sid.ir/paper/4118/en

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