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Information Journal Paper

Title

HYDROTHERMAL FLUID EVOLUTION IN THE DALLI PORPHYRY CU-AU DEPOSIT: FLUID INCLUSION MICRO THERMOMETRY STUDIES

Pages

  277-306

Abstract

 IntroductionA wide variety of world-class porphyry Cu deposits occur in the Urumieh-Dohktar MAGMATIC ARC (UDMA) of Iran.The arc is composed of calcalkaline granitoid rocks, and the ore-hosting porphyry intrusions are dominantly granodiorite to quartz-monzonite (Zarasvandi et al., 2015). It is believed that faults played an important role in the emplacement of intrusions and subsequent porphyry-copper type mineralization (Shahabpour, 1999). Three main centers host the porphyry copper mineralization in the UDMA: (1) Ardestan-SarCheshmeh-Kharestan zone, (2) Saveh-Ardestan district; in the central parts of the UDMA, hosting the DALLI PORPHYRY CU-AU deposit, and (3) Takab-Mianeh-Qharahdagh- Sabalan zone.

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    APA: Copy

    ZARASVANDI, ALIREZA, ASADI, FATEME, POURKASEB, HOUSHANG, AHMADNEJAD, FARHAD, & ZAMANIAN, HASAN. (2016). HYDROTHERMAL FLUID EVOLUTION IN THE DALLI PORPHYRY CU-AU DEPOSIT: FLUID INCLUSION MICRO THERMOMETRY STUDIES. JOURNAL OF ECONOMIC GEOLOGY, 7(2), 277-306. SID. https://sid.ir/paper/180538/en

    Vancouver: Copy

    ZARASVANDI ALIREZA, ASADI FATEME, POURKASEB HOUSHANG, AHMADNEJAD FARHAD, ZAMANIAN HASAN. HYDROTHERMAL FLUID EVOLUTION IN THE DALLI PORPHYRY CU-AU DEPOSIT: FLUID INCLUSION MICRO THERMOMETRY STUDIES. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2016;7(2):277-306. Available from: https://sid.ir/paper/180538/en

    IEEE: Copy

    ALIREZA ZARASVANDI, FATEME ASADI, HOUSHANG POURKASEB, FARHAD AHMADNEJAD, and HASAN ZAMANIAN, “HYDROTHERMAL FLUID EVOLUTION IN THE DALLI PORPHYRY CU-AU DEPOSIT: FLUID INCLUSION MICRO THERMOMETRY STUDIES,” JOURNAL OF ECONOMIC GEOLOGY, vol. 7, no. 2, pp. 277–306, 2016, [Online]. Available: https://sid.ir/paper/180538/en

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