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Information Journal Paper

Title

PETROGRAPHY AND SEDIMENTARY ENVIRONMENTAL DEPOSITS OF THE ASMARI FORMATION IN NORTHERN FLANK OF BANGESTAN ANTICLINE

Pages

  107-116

Abstract

 The ASMARI FORMATION of OLIGOMIOCENE age is the main reservoir in Dezful Embayment. The ASMARI FORMATION was studied around the northern flank of BANGESTAN ANTICLINE and at the north west of Bonjileh village. The thickness of  the ASMARI FORMATION in  the studied region is 198.5 meters. The formation is overlain and underlain with disconformable contacts, by the Pabdeh and Gachsaran formations respectively. Field studies led to recognition of three lithofacies: limestone, shale and marly limestone. Derived results from microscopic studies of thin sections led to recognition of 14 microfacies that in comparison with standard microfacies were precipitated in 4 DEPOSITIONAL ENVIRONMENTs, including supratidal, lagoon, barrier and open marine. Based on these results, the ASMARI FORMATION deposited in different parts of a homoclinal carbonate ramp. Several parameters such as: environmental condition, surface water penetration in to the reservoir, diagenetic processes, and the rate of fracture development are responsible for the quality of this reservoir.

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  • Cite

    APA: Copy

    KOHANSAL GHADIMVAND, NADER, HAMDI, BAHAODIN, & ALIPOUR, MARYAM. (2009). PETROGRAPHY AND SEDIMENTARY ENVIRONMENTAL DEPOSITS OF THE ASMARI FORMATION IN NORTHERN FLANK OF BANGESTAN ANTICLINE. JOURNAL OF THE EARTH, 4(1), 107-116. SID. https://sid.ir/paper/192970/en

    Vancouver: Copy

    KOHANSAL GHADIMVAND NADER, HAMDI BAHAODIN, ALIPOUR MARYAM. PETROGRAPHY AND SEDIMENTARY ENVIRONMENTAL DEPOSITS OF THE ASMARI FORMATION IN NORTHERN FLANK OF BANGESTAN ANTICLINE. JOURNAL OF THE EARTH[Internet]. 2009;4(1):107-116. Available from: https://sid.ir/paper/192970/en

    IEEE: Copy

    NADER KOHANSAL GHADIMVAND, BAHAODIN HAMDI, and MARYAM ALIPOUR, “PETROGRAPHY AND SEDIMENTARY ENVIRONMENTAL DEPOSITS OF THE ASMARI FORMATION IN NORTHERN FLANK OF BANGESTAN ANTICLINE,” JOURNAL OF THE EARTH, vol. 4, no. 1, pp. 107–116, 2009, [Online]. Available: https://sid.ir/paper/192970/en

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