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Information Journal Paper

Title

Mineralization and fluid evolution during mineralization of Sefidkouh Fluorite deposit, north west of Torbate Jam

Pages

  209-218

Abstract

 KuhSefid Flourite deposit is located about 110 km south east of Mashhad. Geological units of the region related to Kashafroud Formation with Jurassic age. Most of Fluorite mineralization can be seen along the faults with direction of north west-south east. Fluorite veins are differente in diameter of 2 to 2. 5 m and length of 50 m. Hydrothermal solutions with maximum and minimum temperatures of 181⁰ C and 125⁰ C with the average temperature of 152⁰ C in protraction of faults, cracks and fragments, have created mineral substance. Geological evidences, petrography, mineralization and homogeneous temperature of fluids inclusion, are the evidences that concluded the Fluorite mineralization as Epithermal.

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    APA: Copy

    Pazhkhzade, leila, Ebrahimi Nasrabadi, Khosroo, Vatanpour, hamidreza, GHAEMI, FARZIN, & DARVISHI KHATOONI, JAVAD. (2018). Mineralization and fluid evolution during mineralization of Sefidkouh Fluorite deposit, north west of Torbate Jam. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 26(1 ), 209-218. SID. https://sid.ir/paper/389580/en

    Vancouver: Copy

    Pazhkhzade leila, Ebrahimi Nasrabadi Khosroo, Vatanpour hamidreza, GHAEMI FARZIN, DARVISHI KHATOONI JAVAD. Mineralization and fluid evolution during mineralization of Sefidkouh Fluorite deposit, north west of Torbate Jam. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2018;26(1 ):209-218. Available from: https://sid.ir/paper/389580/en

    IEEE: Copy

    leila Pazhkhzade, Khosroo Ebrahimi Nasrabadi, hamidreza Vatanpour, FARZIN GHAEMI, and JAVAD DARVISHI KHATOONI, “Mineralization and fluid evolution during mineralization of Sefidkouh Fluorite deposit, north west of Torbate Jam,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 26, no. 1 , pp. 209–218, 2018, [Online]. Available: https://sid.ir/paper/389580/en

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