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Information Journal Paper

Title

GEOLOGICAL AND MINERALOGICAL STUDIES OF HYDROTHERMAL ALTERATIONS (ALUNITIZATION AND KAOLINITIZATION) IN NORTH OF ISFAHAN (KESHEH AREA)

Pages

  1-10

Abstract

 Northern parts of Isfahan province are included into well known Cenozoic Magmatic Belt of Central Iran. There are extensive Eocene volcanic events. Field observation indicated that, the late intrusion bodies which are belonged to Oligo – Miocene are caused some dispersed HYDROTHERMAL ALTERATION in area. On the base of XRD, XRF and SEM data mineralogy and chemical composition of fresh and altered volcanics are determined. Volcanic rocks with chemical composition andesite to trachy- andesite have more extensive in this area. KAOLINITE, ALUNITE and jarosite are major minerals in altered pyroclastic rocks. Mineral assemblages of these alterations are characteristic of acid – sulfate or advanced argilic type alterations. With attention to the geochemistry of major and trace element the KAOLINITE - ALUNITE association are likely from hypogene source in Kesheh area.

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    APA: Copy

    TAGHIPOUR, B., NOURBEHESHT, I., & KHALILI, MAHMOUD. (2007). GEOLOGICAL AND MINERALOGICAL STUDIES OF HYDROTHERMAL ALTERATIONS (ALUNITIZATION AND KAOLINITIZATION) IN NORTH OF ISFAHAN (KESHEH AREA). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", 27(1), 1-10. SID. https://sid.ir/paper/56009/en

    Vancouver: Copy

    TAGHIPOUR B., NOURBEHESHT I., KHALILI MAHMOUD. GEOLOGICAL AND MINERALOGICAL STUDIES OF HYDROTHERMAL ALTERATIONS (ALUNITIZATION AND KAOLINITIZATION) IN NORTH OF ISFAHAN (KESHEH AREA). RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE"[Internet]. 2007;27(1):1-10. Available from: https://sid.ir/paper/56009/en

    IEEE: Copy

    B. TAGHIPOUR, I. NOURBEHESHT, and MAHMOUD KHALILI, “GEOLOGICAL AND MINERALOGICAL STUDIES OF HYDROTHERMAL ALTERATIONS (ALUNITIZATION AND KAOLINITIZATION) IN NORTH OF ISFAHAN (KESHEH AREA),” RESEARCH JOURNAL OF UNIVERSITY OF ISFAHAN "SCIENCE", vol. 27, no. 1, pp. 1–10, 2007, [Online]. Available: https://sid.ir/paper/56009/en

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