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Title

COMPARATIVE BIOSTRATIGRAPHY OF ASMARI FORMATION IN MALEH-KUH AND AMIRAN ANTICLINES, LORESTAN, ZAGROS BASIN, BASED ON BENTHIC FORAMINIFERA

Pages

  191-198

Abstract

 This study aimed to compare ASMARI FORMATION in two sections in Maleh-Kuh and AMIRAN ANTICLINEs based on BENTHONIC FORAMINIFERA. In this study, 26 species and 16 genera of BENTHONIC FORAMINIFERA from the Maleh-Kuh section yielded 2 biozones of Elphidium sp. 14 – Peneroplis farsenensis and Borelis melo curdica – Borelis melo melo were suggesting an age of AQUITANIAN BURDIGALIAN for the formation. In AMIRAN ANTICLINE based on 27 species and 20 genera only the biozone of Borelis melo curdica – Borelis melo melo (Burdigalian) was recorded. Based on this study, the Asmari sequence in Maleh-kuh Section (with a thickness of 310 m) deposited earlier In AQUITANIAN. But in Amiran section (with 162 m thickness) deposition started in BURDIGALIAN and ended synchronously in both sections. In both sections the ASMARI FORMATION overlain Shahbazan Formation disconformably and is in turn under lain by Ghachsaran Formation concordantly-transitionally in Maleh-Kuh and by a sharp contact in Amiran Section.

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    APA: Copy

    MOHAMMADI, M., AMIRI BAKHTIAR, H., & AMRAEE, F.. (2016). COMPARATIVE BIOSTRATIGRAPHY OF ASMARI FORMATION IN MALEH-KUH AND AMIRAN ANTICLINES, LORESTAN, ZAGROS BASIN, BASED ON BENTHIC FORAMINIFERA. GEOSCIENCES, 25(98), 191-198. SID. https://sid.ir/paper/32244/en

    Vancouver: Copy

    MOHAMMADI M., AMIRI BAKHTIAR H., AMRAEE F.. COMPARATIVE BIOSTRATIGRAPHY OF ASMARI FORMATION IN MALEH-KUH AND AMIRAN ANTICLINES, LORESTAN, ZAGROS BASIN, BASED ON BENTHIC FORAMINIFERA. GEOSCIENCES[Internet]. 2016;25(98):191-198. Available from: https://sid.ir/paper/32244/en

    IEEE: Copy

    M. MOHAMMADI, H. AMIRI BAKHTIAR, and F. AMRAEE, “COMPARATIVE BIOSTRATIGRAPHY OF ASMARI FORMATION IN MALEH-KUH AND AMIRAN ANTICLINES, LORESTAN, ZAGROS BASIN, BASED ON BENTHIC FORAMINIFERA,” GEOSCIENCES, vol. 25, no. 98, pp. 191–198, 2016, [Online]. Available: https://sid.ir/paper/32244/en

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