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Information Journal Paper

Title

FLUID INCLUSION AND SULFUR STABLE ISOTOPE EVIDENCE FOR THE ORIGIN OF THE AHANGRAN PB-AG DEPOSIT

Pages

  343-367

Abstract

 IntroductionThe Ahangaran PB-AG deposit is located in the Hamedan province, west Iran, 25 km southeast of the city of Malayer. The deposit lies in the strongly folded Sanandaj-Sirjan tectonic zone, in which the ore bodies occur as thin lenses and layers. The host rocks of the deposit are Early Cretaceous carbonates and sandstones that are unconformably underlain by Jurassic rocks. Ore minerals include galena, pyrite, chalcopyrite, pyrrhotite and supergene iron oxide minerals. Gangue minerals consist of barite, dolomite, chlorite, calcite and quartz. The mineralization occurs as open-space fillings, veins, veinlets, disseminations, and massive replacements. Alteration consists of silicification, sericitization, and dolomitization. In this study, we carried out studies of mineralogy, micro thermometry of FLUID INCLUSIONs and sulfur isotopes to determine the source of sulfur and the physico-chemical conditions of formation.

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    APA: Copy

    MAANIJOU, MOHAMMAD, VAFAEI ZAD, MASOUMEH, & ALIANI, FARHAD. (2016). FLUID INCLUSION AND SULFUR STABLE ISOTOPE EVIDENCE FOR THE ORIGIN OF THE AHANGRAN PB-AG DEPOSIT. JOURNAL OF ECONOMIC GEOLOGY, 7(2), 343-367. SID. https://sid.ir/paper/180547/en

    Vancouver: Copy

    MAANIJOU MOHAMMAD, VAFAEI ZAD MASOUMEH, ALIANI FARHAD. FLUID INCLUSION AND SULFUR STABLE ISOTOPE EVIDENCE FOR THE ORIGIN OF THE AHANGRAN PB-AG DEPOSIT. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2016;7(2):343-367. Available from: https://sid.ir/paper/180547/en

    IEEE: Copy

    MOHAMMAD MAANIJOU, MASOUMEH VAFAEI ZAD, and FARHAD ALIANI, “FLUID INCLUSION AND SULFUR STABLE ISOTOPE EVIDENCE FOR THE ORIGIN OF THE AHANGRAN PB-AG DEPOSIT,” JOURNAL OF ECONOMIC GEOLOGY, vol. 7, no. 2, pp. 343–367, 2016, [Online]. Available: https://sid.ir/paper/180547/en

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