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Information Journal Paper

Title

Characteristics of the ore-bearing quartz veins using fluid inclusions, Andarian, NW Iran

Pages

  723-738

Abstract

Andarian area is located north of Tabriz city, north west Iran, and tectonically is a part of Ahar-Arasbaran magmatic belt. Geology of the area includes Miocene shallow pluton, Cretaceous flysch-type sediments, metamorphic rocks )hornfels and skarn( and volcanic rocks. Mineralization occurred in two stages: primary and secondary. The primary ore minerals include Au, pyrite and stibnite. Malachite, azurite and iron-hydroxides are the main minerals of the secondary phase. Two phases of liquid-rich and gas-rich inclusions are the most common type of inclusions. The average formation temperature of Quartz-gold vein deposit is 237° C with low salinity (with an average of 8. 7 wt% NaCl equivalent). The pressure of entrapment for fluid inclusions is between 26 to 51 bars, which is equal to the depth of 270-550 m. Based on fluid inclusions studies, the gold bearing Quartz veins formed in epithermal condition.

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  • Cite

    APA: Copy

    Namnabat, E., GHORBANI, M., & Tabatabaee, S.H.. (2019). Characteristics of the ore-bearing quartz veins using fluid inclusions, Andarian, NW Iran. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, 27(3 ), 723-738. SID. https://sid.ir/paper/3964/en

    Vancouver: Copy

    Namnabat E., GHORBANI M., Tabatabaee S.H.. Characteristics of the ore-bearing quartz veins using fluid inclusions, Andarian, NW Iran. IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY[Internet]. 2019;27(3 ):723-738. Available from: https://sid.ir/paper/3964/en

    IEEE: Copy

    E. Namnabat, M. GHORBANI, and S.H. Tabatabaee, “Characteristics of the ore-bearing quartz veins using fluid inclusions, Andarian, NW Iran,” IRANIAN JOURNAL OF CRYSTALLOGRAPHY AND MINERALOGY, vol. 27, no. 3 , pp. 723–738, 2019, [Online]. Available: https://sid.ir/paper/3964/en

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