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Information Journal Paper

Title

STUDY OF LITHOFACIES, MICROFACIES AND DEPOSITIONAL ENVIRONMENT OF ASMARI FORMATION IN PARSI OIL FIELD

Pages

  73-82

Abstract

 The OLIGO-MIOCENE ASMARI FORMATION is one of the most important reservoir units of the Parsi Oil Field that is located in North Dezful Embayment in SW of Iran.This formation is laid over the shales of Pabdeh Formation concordantly and is overlaid concordantly by evaporates of Gachsaran Formation. ASMARI FORMATION (with 419m thickness) is composed of anhydrite, carbonate rocks (limestone & dolomite) associated with thin shale interlayers.In this study LITHOFACIES, MICROFACIES, and their associated facies of studied formation have been investigated based on core samples and thin sections. Study of ASMARI FORMATION led to recognition of 8 LITHOFACIES and 18 MICROFACIES that are related to open marine, barrier, shallow subtidal facies, reef, lagoon, supratidal and intertidal environments. The Correlation of mentioned micofacies with standard model of carbonate from ramp environment (Buxton & Pedley, 1989), show that ASMARI FORMATION was deposited in a CARBONATE RAMP which some local reef or patch reef.

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  • Cite

    APA: Copy

    HASAN VAND, A., & AL ALI, S.M.. (2009). STUDY OF LITHOFACIES, MICROFACIES AND DEPOSITIONAL ENVIRONMENT OF ASMARI FORMATION IN PARSI OIL FIELD. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(5), 73-82. SID. https://sid.ir/paper/186819/en

    Vancouver: Copy

    HASAN VAND A., AL ALI S.M.. STUDY OF LITHOFACIES, MICROFACIES AND DEPOSITIONAL ENVIRONMENT OF ASMARI FORMATION IN PARSI OIL FIELD. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(5):73-82. Available from: https://sid.ir/paper/186819/en

    IEEE: Copy

    A. HASAN VAND, and S.M. AL ALI, “STUDY OF LITHOFACIES, MICROFACIES AND DEPOSITIONAL ENVIRONMENT OF ASMARI FORMATION IN PARSI OIL FIELD,” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 5, pp. 73–82, 2009, [Online]. Available: https://sid.ir/paper/186819/en

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