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Information Journal Paper

Title

MINERALOGICAL PROPERTIES OF HYDROTHERMAL ANALCIME IN VOLCANIC ROCKS OF SOUTH KAHRIZAK

Pages

  113-120

Abstract

 Analcime along with other ZEOLITE group minerals such as: TETRANATROLITE, NATROLITE, MESOLITE, SCOLCITE, HEULANDITE, STILBITEs and, LEVYNE occur as vein and cavity filling minerals in the intermediate to basic volcanic rocks in South KAHRIZAK. Scanning Electron Microscopy (SEM) of microcrystaline ANALCIME reveal pseudo-cubic prismatic faces of [211] containing laminations perpendicular to the elongation of the crystals. These laminations are due to crystal growth mechanism and are characteristics of hydrothermally formed ANALCIME (H-type). X-ray diffraction study has revealed a pseudocubic symmetry for ANALCIME with unit-cell parameters of: a = 13.6974(51) Å, b = 13.6874(124) Å, C = 13.6637(311) Å, V = 2561.695 Å3.Raman spectrum of the sample shows vibrational mode frequency for H2O molecules in ANALCIME at about 3500 cm-1.

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    Cite

    APA: Copy

    TUTTI, F., YAZDANI, S., & BAZARGANI GUILANI, K.. (2011). MINERALOGICAL PROPERTIES OF HYDROTHERMAL ANALCIME IN VOLCANIC ROCKS OF SOUTH KAHRIZAK. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 19(1), 113-120. SID. https://sid.ir/paper/4020/en

    Vancouver: Copy

    TUTTI F., YAZDANI S., BAZARGANI GUILANI K.. MINERALOGICAL PROPERTIES OF HYDROTHERMAL ANALCIME IN VOLCANIC ROCKS OF SOUTH KAHRIZAK. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2011;19(1):113-120. Available from: https://sid.ir/paper/4020/en

    IEEE: Copy

    F. TUTTI, S. YAZDANI, and K. BAZARGANI GUILANI, “MINERALOGICAL PROPERTIES OF HYDROTHERMAL ANALCIME IN VOLCANIC ROCKS OF SOUTH KAHRIZAK,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 19, no. 1, pp. 113–120, 2011, [Online]. Available: https://sid.ir/paper/4020/en

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