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Information Journal Paper

Title

MICROFACIES AND SEDIMENTARY ENVIRONMENT OF TRIASSIC ROCKS IN EGHLID AREA (FARS PROVINCE)

Pages

  27-36

Abstract

 Triassic rocks in Zagros zone, consisting of limestones, dolostones and shale (ca.324 m thick), were examined in Eghlid area (near Nezamabad Village). A lithofacies (shale/marl) and 13 carbonate MICROFACIES, consisting of: 1) paleosol, 2) supratidal mudstone, 3) algal mat boundstone, 4) intertidal mudstone, 5) intertidal breccia, 6) lagoonal mudstone, 7) shale/marl, 8) lagoonal mudstone/wackstone, 9) lagoonal wackstone, 10) lagoonal wackstone/packstone, 11) lagoonal packstone 12) sand shoal packstone, 13) sand shoale grainstone, and 14) open marine mudstone were recognized. All of them have been taken place in the inner part of a ramp. MICROFACIES 1 to 5 belong to intertidal zone; MICROFACIES 6 to 11 (and shale) occurred in the lagoon site; MICROFACIES 12 and 13 referred to the sand shoal and bar; and MICROFACIES 14 was deposited in the open marine belt of the sedimentary basin.

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  • Cite

    APA: Copy

    KANKAZIAN, A., & SERAFAF, S.. (2010). MICROFACIES AND SEDIMENTARY ENVIRONMENT OF TRIASSIC ROCKS IN EGHLID AREA (FARS PROVINCE). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(7), 27-36. SID. https://sid.ir/paper/186827/en

    Vancouver: Copy

    KANKAZIAN A., SERAFAF S.. MICROFACIES AND SEDIMENTARY ENVIRONMENT OF TRIASSIC ROCKS IN EGHLID AREA (FARS PROVINCE). JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2010;2(7):27-36. Available from: https://sid.ir/paper/186827/en

    IEEE: Copy

    A. KANKAZIAN, and S. SERAFAF, “MICROFACIES AND SEDIMENTARY ENVIRONMENT OF TRIASSIC ROCKS IN EGHLID AREA (FARS PROVINCE),” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 7, pp. 27–36, 2010, [Online]. Available: https://sid.ir/paper/186827/en

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