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Information Journal Paper

Title

FACIES AND DEPOSITIONAL ENVIRONMENTS OF TERRIGENOUS DEPOSITS OF THE ASMARI FORMATION, IN THE AGHAJARI WELL NO. 61

Pages

  1-18

Abstract

 The ASMARI FORMATION (Oligo-Miocene) consists of carbonate and terrigenous deposits (Ahwaz Member) in the AGHAJARI OIL FIELD. In the Aghajari Well No.61, the Ahwaz Sandstone Member is unconformably bounded by underlain Pabdeh Formation and the overlying upper Asmari Member. Petrograpgic studies of the terrigenous deposits of the Ahwaz Member led to recognition of open marine, incised valley, barrier, lagoon, tidal flat, elongate and lobate deltas and fluvial FACIES deposits. These FACIES were formed after Late Ruplian tectonic activity. Based on this study, the lower unit of the Ahwaz Sandstone Member was formed in a mixed carbonate-terrigenous distally steepened ramp, but its upper unit, on the other hand, was formed on a homoclinal ramp. FACIES variations within the Ahwas Member can be related to tectonic activity, sea level fluctuations and depositional processes.

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    Cite

    APA: Copy

    AMIN RASOULI, H., LASEMI, Y., & ZAHRI, SH.. (2011). FACIES AND DEPOSITIONAL ENVIRONMENTS OF TERRIGENOUS DEPOSITS OF THE ASMARI FORMATION, IN THE AGHAJARI WELL NO. 61. SEDIMENTARY FACIES, 3(2), 1-18. SID. https://sid.ir/paper/199862/en

    Vancouver: Copy

    AMIN RASOULI H., LASEMI Y., ZAHRI SH.. FACIES AND DEPOSITIONAL ENVIRONMENTS OF TERRIGENOUS DEPOSITS OF THE ASMARI FORMATION, IN THE AGHAJARI WELL NO. 61. SEDIMENTARY FACIES[Internet]. 2011;3(2):1-18. Available from: https://sid.ir/paper/199862/en

    IEEE: Copy

    H. AMIN RASOULI, Y. LASEMI, and SH. ZAHRI, “FACIES AND DEPOSITIONAL ENVIRONMENTS OF TERRIGENOUS DEPOSITS OF THE ASMARI FORMATION, IN THE AGHAJARI WELL NO. 61,” SEDIMENTARY FACIES, vol. 3, no. 2, pp. 1–18, 2011, [Online]. Available: https://sid.ir/paper/199862/en

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