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Information Journal Paper

Title

PETROGRAPHY AND GEOCHEMISTRY OF JAROSITE IN RANGAN (SOUTHWEST OF ARDESTAN)

Pages

  203-214

Abstract

 The study area is a part of central Iranian Cenozoic magmatic belt. The dominant rock type in the area is rhyodacite with Eocene in age. These rocks have been effected by Qum-Zefreh fault as well as alteration by HYDROTHERMAL SOLUTIONS. Due to sulfate - acid alteration, the following minerals are formed: pyrite + alkali feldspar + sericite + pyrophyllite + barite + JAROSITE + hematite + quartz. The presence of abundant JAROSITE mineral and the high heavy elemental content, as well as the high K/Na ratio, we suggest that the RANGAN JAROSITE may have a magmatic - hydrothermal ongm.

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    APA: Copy

    PARSAPOUR, A., KHALILI, M., NOGHREHEIAN, M., & MAKIZADEH, M.. (2004). PETROGRAPHY AND GEOCHEMISTRY OF JAROSITE IN RANGAN (SOUTHWEST OF ARDESTAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 12(2), 203-214. SID. https://sid.ir/paper/3871/en

    Vancouver: Copy

    PARSAPOUR A., KHALILI M., NOGHREHEIAN M., MAKIZADEH M.. PETROGRAPHY AND GEOCHEMISTRY OF JAROSITE IN RANGAN (SOUTHWEST OF ARDESTAN). IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2004;12(2):203-214. Available from: https://sid.ir/paper/3871/en

    IEEE: Copy

    A. PARSAPOUR, M. KHALILI, M. NOGHREHEIAN, and M. MAKIZADEH, “PETROGRAPHY AND GEOCHEMISTRY OF JAROSITE IN RANGAN (SOUTHWEST OF ARDESTAN),” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 12, no. 2, pp. 203–214, 2004, [Online]. Available: https://sid.ir/paper/3871/en

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