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Information Journal Paper

Title

THE STUDY OF LIMESTONE DEPOSITS OF KANGAN FORMATION: APPLICATION FOR ORIGINAL MINERALOGY AND PALEOCLIMATOLOGY, SOUTH PARS FIELD, PERSIAN GULF

Pages

  87-102

Abstract

 The reservoir part of KANGAN FORMATION with thickness of 115 m is a carbonate-evaporate sequence that is considered as a part of the largest carbonate reservoir in the South Pars Field in the PERSIAN GULF. Based on the facies studies the KANGAN FORMATION consists of 12 microfacies and 4 facies belts, such as tidal flat, lagoon, shoal and open marine. The elemental studies and oxygen carbon isotopic trends in limestone samples indicate that these sediments were deposited in a tropical shallow environment and aragonite was original carbonate mineralogy. KANGAN FORMATION has undergone a meteoric diagenesis in a closed diagenetic system. Variation of minor elements and their ratios along the stratigraphic column, and particularly between Dalan-Kangan Formations, clearly determined the boundary between these two formations. This variation is related to diagenetic and facies variations.

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    APA: Copy

    ADABI, MOHAMMAD HOSSEIN, & KHODAEI, NAVAB. (2009). THE STUDY OF LIMESTONE DEPOSITS OF KANGAN FORMATION: APPLICATION FOR ORIGINAL MINERALOGY AND PALEOCLIMATOLOGY, SOUTH PARS FIELD, PERSIAN GULF. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), 34(4 (SECTION: GEOLOGY)), 87-102. SID. https://sid.ir/paper/2282/en

    Vancouver: Copy

    ADABI MOHAMMAD HOSSEIN, KHODAEI NAVAB. THE STUDY OF LIMESTONE DEPOSITS OF KANGAN FORMATION: APPLICATION FOR ORIGINAL MINERALOGY AND PALEOCLIMATOLOGY, SOUTH PARS FIELD, PERSIAN GULF. JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT)[Internet]. 2009;34(4 (SECTION: GEOLOGY)):87-102. Available from: https://sid.ir/paper/2282/en

    IEEE: Copy

    MOHAMMAD HOSSEIN ADABI, and NAVAB KHODAEI, “THE STUDY OF LIMESTONE DEPOSITS OF KANGAN FORMATION: APPLICATION FOR ORIGINAL MINERALOGY AND PALEOCLIMATOLOGY, SOUTH PARS FIELD, PERSIAN GULF,” JOURNAL OF SCIENCE (UNIVERSITY OF TEHRAN) (JSUT), vol. 34, no. 4 (SECTION: GEOLOGY), pp. 87–102, 2009, [Online]. Available: https://sid.ir/paper/2282/en

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