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Information Journal Paper

Title

STUDY OF REE BEHAVIORS, FLUID INCLUSIONS, AND O, S STABLE ISOTOPES IN ZAFAR-ABAD IRON SKARN DEPOSIT, NW DIVANDARREH, KORDESTAN PROVINCE

Pages

  235-257

Abstract

 The Zafar-abad iron ore deposit, situated in the NW part of Divandarreh (lat. 36°01' 14" and long. 46°58' 22"). The ore body is located on the northern margin of the Sanandaj-Sirjan igneous metamorphic zone. The Zafar-abad Fe-skarn deposit is one of the important, medium-size mineral deposits in western Iran.REE patterns of skarn MAGNETITE were among others studied in Skarn deposit by (Taylor, 1979) Hydrothermal alteration and fluid-rock interaction significantly affect total contents of REE and their patterns in fluids. Moreover, fractionation of REE by chemical complication, adsorption effects and redox reactions are characteristic processes determining REE behavior during crystallization. Stable isotope data for oxygen and sulfur have been widely used with great success to trace the origin and evolution history of paleo-hydrothermal fluids of meteoric, magmatic, and metamorphic.

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    APA: Copy

    BARATI, MEHRDAD, & GHOLIPOOR, MEISAM. (2015). STUDY OF REE BEHAVIORS, FLUID INCLUSIONS, AND O, S STABLE ISOTOPES IN ZAFAR-ABAD IRON SKARN DEPOSIT, NW DIVANDARREH, KORDESTAN PROVINCE. JOURNAL OF ECONOMIC GEOLOGY, 6(2), 235-257. SID. https://sid.ir/paper/180519/en

    Vancouver: Copy

    BARATI MEHRDAD, GHOLIPOOR MEISAM. STUDY OF REE BEHAVIORS, FLUID INCLUSIONS, AND O, S STABLE ISOTOPES IN ZAFAR-ABAD IRON SKARN DEPOSIT, NW DIVANDARREH, KORDESTAN PROVINCE. JOURNAL OF ECONOMIC GEOLOGY[Internet]. 2015;6(2):235-257. Available from: https://sid.ir/paper/180519/en

    IEEE: Copy

    MEHRDAD BARATI, and MEISAM GHOLIPOOR, “STUDY OF REE BEHAVIORS, FLUID INCLUSIONS, AND O, S STABLE ISOTOPES IN ZAFAR-ABAD IRON SKARN DEPOSIT, NW DIVANDARREH, KORDESTAN PROVINCE,” JOURNAL OF ECONOMIC GEOLOGY, vol. 6, no. 2, pp. 235–257, 2015, [Online]. Available: https://sid.ir/paper/180519/en

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