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Information Journal Paper

Title

Microfacies, sedimentary environment and diagenesis of the Asmari Formation in Chahar Bisheh Oil Field, south west of Iran

Pages

  86-113

Abstract

 In this research, two subsurface sections consist of well No. 2 and No. 3 from the Asmari Formation with a thickness of 423 and 412 m respectively in Chahar Bisheh oil Field have been studied. The Asmari Formation in this field consists of intermittent layers of limestone and dolomite, very thin shale layers and anhydrite interlayers. Based on petrographic studies and identification of Microfacies, 15 Microfacies and 1 lithofacies in 4 facies belts consist of tidal flats, lagoon, shoal and open marine for the Asmari Formation have been recognized and Sedimentary environment of this formation, is a Homocline ramp carbonate platform. Effective diagenetic processes including cementation, dolomitization, compaction, fracturing, dissolution, micritization, pyritization, geopetal fabric, boring, silicification and neomorphism which has influenced the Asmari Formation by all three marine, meteoric and burial diagenetic environments.

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    APA: Copy

    Yousefi Hajivand, Asiyeh, Adabi, Mohammad Hoseyn, & Sadeghi, Abbas. (2019). Microfacies, sedimentary environment and diagenesis of the Asmari Formation in Chahar Bisheh Oil Field, south west of Iran. RESEARCHES IN EARTH SCIENCES, 9(36 ), 86-113. SID. https://sid.ir/paper/207467/en

    Vancouver: Copy

    Yousefi Hajivand Asiyeh, Adabi Mohammad Hoseyn, Sadeghi Abbas. Microfacies, sedimentary environment and diagenesis of the Asmari Formation in Chahar Bisheh Oil Field, south west of Iran. RESEARCHES IN EARTH SCIENCES[Internet]. 2019;9(36 ):86-113. Available from: https://sid.ir/paper/207467/en

    IEEE: Copy

    Asiyeh Yousefi Hajivand, Mohammad Hoseyn Adabi, and Abbas Sadeghi, “Microfacies, sedimentary environment and diagenesis of the Asmari Formation in Chahar Bisheh Oil Field, south west of Iran,” RESEARCHES IN EARTH SCIENCES, vol. 9, no. 36 , pp. 86–113, 2019, [Online]. Available: https://sid.ir/paper/207467/en

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