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Information Journal Paper

Title

FACIES AND SEDIMENTARY ENVIRONMENTS OF EOCENE NUMMULITIC LIMESTONE IN SOUTHERN KHALKHAL

Pages

  53-62

Abstract

ZIARAT FORMATION in KHALKHAL region is disconformably located on creataceours limes and is covered by acidic tuffs and andesite lithic unites of EOCENE Age which is equal to the lower part of Karaj Formation and this is the indicator of a unit of Nummulitic limestone with the age of middle EOCENE.The thickness of the studied section is 36 meter and its dominant lithology includes limestone, sandy limestone, nummulitic limestone and marl. According to field studies and microscopic sections, the identified microfacies belong to six environments, namely, tidal flat, lagoon, back bar, bioclassic bar, forebar and open marine. The sedimentation model of a shallow sea is in the epicontinental platform which has never found the conditions of a deep marine.This carbonate platform which is the type of homoclinal ramp is comparable withsouthern parts of Persian Gulf (Troutial Coast) in the present age environment.

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    Cite

    APA: Copy

    MAHARI, R., KANGI, A., & AFTAB NAVASHNGH, S.. (2009). FACIES AND SEDIMENTARY ENVIRONMENTS OF EOCENE NUMMULITIC LIMESTONE IN SOUTHERN KHALKHAL. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, 2(5), 53-62. SID. https://sid.ir/paper/186818/en

    Vancouver: Copy

    MAHARI R., KANGI A., AFTAB NAVASHNGH S.. FACIES AND SEDIMENTARY ENVIRONMENTS OF EOCENE NUMMULITIC LIMESTONE IN SOUTHERN KHALKHAL. JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK[Internet]. 2009;2(5):53-62. Available from: https://sid.ir/paper/186818/en

    IEEE: Copy

    R. MAHARI, A. KANGI, and S. AFTAB NAVASHNGH, “FACIES AND SEDIMENTARY ENVIRONMENTS OF EOCENE NUMMULITIC LIMESTONE IN SOUTHERN KHALKHAL,” JOURNAL OF SEDIMENT AND SEDIMENTARY ROCK, vol. 2, no. 5, pp. 53–62, 2009, [Online]. Available: https://sid.ir/paper/186818/en

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