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Title

GEOCHEMISTRY AND FLUID INCLUSIONS STUDIES OF LOW-SULFIDATION EPITHERMAL GOLD MINERALIZATION IN THE MIRKUH ALI MIRZA AREA, SARAB, NW IRAN

Pages

  9-14

Abstract

 The MIRKUH ALI MIRZA gold mineralization is located in north SARAB in the Western Alborz–Azerbaijan structural zone. Mineralization was formed in the form of a vein occurring in Neogene dacitic and rhyodacitic tuff along a series of NW–SE trending fault; Mineralization associated with quartz-sericite-adularia-calcite and pyrite (<1%) assemblages is a typical of LOW-SULFIDATION EPITHERMAL GOLD mineralization. The fluid inclusion data from quartz minerals indicate homogenization temperature of 161-260oC and salinities of 0.5 to 6.5 wt% NaCl equiv. The variation in gold grade in quartz vein is 270-3240 ppb. The highest gold content is in lattice and breccias quartz that can indicate direct relationship between boiling to gold deposition. The idea is supported by coexistence of vapor-dominant and liquid-dominant fluid inclusions.

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    APA: Copy

    MAGHSOUDI, A., YAZDI, M., MEHR PARTOU, M., & VOSOUGHI ABEDINI, M.. (2012). GEOCHEMISTRY AND FLUID INCLUSIONS STUDIES OF LOW-SULFIDATION EPITHERMAL GOLD MINERALIZATION IN THE MIRKUH ALI MIRZA AREA, SARAB, NW IRAN. GEOSCIENCES, 22(85), 9-14. SID. https://sid.ir/paper/31795/en

    Vancouver: Copy

    MAGHSOUDI A., YAZDI M., MEHR PARTOU M., VOSOUGHI ABEDINI M.. GEOCHEMISTRY AND FLUID INCLUSIONS STUDIES OF LOW-SULFIDATION EPITHERMAL GOLD MINERALIZATION IN THE MIRKUH ALI MIRZA AREA, SARAB, NW IRAN. GEOSCIENCES[Internet]. 2012;22(85):9-14. Available from: https://sid.ir/paper/31795/en

    IEEE: Copy

    A. MAGHSOUDI, M. YAZDI, M. MEHR PARTOU, and M. VOSOUGHI ABEDINI, “GEOCHEMISTRY AND FLUID INCLUSIONS STUDIES OF LOW-SULFIDATION EPITHERMAL GOLD MINERALIZATION IN THE MIRKUH ALI MIRZA AREA, SARAB, NW IRAN,” GEOSCIENCES, vol. 22, no. 85, pp. 9–14, 2012, [Online]. Available: https://sid.ir/paper/31795/en

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