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Information Journal Paper

Title

MICROBIOSTRATIGRAPHY, FACIES AND SEDIMENTARY ENVIRONMENT OF THE JAHRUM FORMATION, NORTHWEST OF SHIRAZ

Pages

  43-53

Abstract

 The JAHRUM FORMATION with 192 m thickness at the studied area consists of carbonate sequence which overlies Pabdeh Formation sharply and underlies the Asmari Formation gradually. The aim of this paper is to describe the micro biostratigraphy, biological facies and sedimentary environment interpretation of JAHRUM FORMATION at the section studied. Based on biostratigraphic studies 19 genera and 27 species of BENTHIC FORAMINIFERA were identified which are located in two assemblage zones. Biozone no.1 (Nummulites-Alveolina assemblage subzone) belonging to the Middle EOCENE age and biozone no.2 (Nummulites fabiani taxon range zone) belong to the Late EOCENE age. According to the diagnosed biozones, the age of JAHRUM FORMATION at the studied section is Middle EOCENE - Late EOCENE. Studies led to the identification of eight biofacies of lagoon, shoal and open sea. The absence of turbidite deposits and reef facies indicate sediments deposition of JAHRUM FORMATION has occurred in a carbonate platform of hemoclinal ramp type (including inner, middle and outer ramp).

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    APA: Copy

    PARVANEHNEZHAD SHIRAZI, M., & BALOOD, S.. (2015). MICROBIOSTRATIGRAPHY, FACIES AND SEDIMENTARY ENVIRONMENT OF THE JAHRUM FORMATION, NORTHWEST OF SHIRAZ. APPLIED SEDIMENTOLOGY, 3(5), 43-53. SID. https://sid.ir/paper/260607/en

    Vancouver: Copy

    PARVANEHNEZHAD SHIRAZI M., BALOOD S.. MICROBIOSTRATIGRAPHY, FACIES AND SEDIMENTARY ENVIRONMENT OF THE JAHRUM FORMATION, NORTHWEST OF SHIRAZ. APPLIED SEDIMENTOLOGY[Internet]. 2015;3(5):43-53. Available from: https://sid.ir/paper/260607/en

    IEEE: Copy

    M. PARVANEHNEZHAD SHIRAZI, and S. BALOOD, “MICROBIOSTRATIGRAPHY, FACIES AND SEDIMENTARY ENVIRONMENT OF THE JAHRUM FORMATION, NORTHWEST OF SHIRAZ,” APPLIED SEDIMENTOLOGY, vol. 3, no. 5, pp. 43–53, 2015, [Online]. Available: https://sid.ir/paper/260607/en

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