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Information Journal Paper

Title

BIOSTRATIGRAPHY AND PALAEOECOLOGY OF TARBUR FORMATION IN SEMIROM AREA, SOUTHWEST OF ISFAHAN

Pages

  85-108

Abstract

 Introduction: The TARBUR FORMATION is located in the interior of Fars region (east of Zagros Mountains) and is known as a carbonate unit with abundant larger benthic FORAMINIFERA, RUDIST and coral. This formation is exposed in the interior part of Fars and high Zagros zones and southwestward it laterally changes to thin limestone beds. The facies of this formation eventually changes into the Gurpi shale Formation. The purpose of this study is to assess the paleoecology and BIOSTRATIGRAPHY of the TARBUR FORMATION based on present fauna (foraminifera) in SEMIROM area (SW of Isfahan). The study area with geographical coordinate of N: 31o 22' 48" and E: 51o 32' 01" is located at about 5kms southwest of SEMIROM area. The thickness of the TARBUR FORMATION in the study area is 462 meters. The formation mainly consists of carbonate and terrigenous rocks and has a gradual and conformable contact with underlying red shale unit (S2) while is overlaid by the Kashkan Formation which is marked by an erosional surface...

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    APA: Copy

    AZIZI, R., SAFARI, A., & VAZIRI MOGHADDAM, H.. (2015). BIOSTRATIGRAPHY AND PALAEOECOLOGY OF TARBUR FORMATION IN SEMIROM AREA, SOUTHWEST OF ISFAHAN. SEDIMENTARY FACIES, 8(1), 85-108. SID. https://sid.ir/paper/199816/en

    Vancouver: Copy

    AZIZI R., SAFARI A., VAZIRI MOGHADDAM H.. BIOSTRATIGRAPHY AND PALAEOECOLOGY OF TARBUR FORMATION IN SEMIROM AREA, SOUTHWEST OF ISFAHAN. SEDIMENTARY FACIES[Internet]. 2015;8(1):85-108. Available from: https://sid.ir/paper/199816/en

    IEEE: Copy

    R. AZIZI, A. SAFARI, and H. VAZIRI MOGHADDAM, “BIOSTRATIGRAPHY AND PALAEOECOLOGY OF TARBUR FORMATION IN SEMIROM AREA, SOUTHWEST OF ISFAHAN,” SEDIMENTARY FACIES, vol. 8, no. 1, pp. 85–108, 2015, [Online]. Available: https://sid.ir/paper/199816/en

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