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Information Journal Paper

Title

INTRODUCING THE OSTRACODS IN MARLS UNITS 1 AND 3 (K1 AND K3) OF TARBUR FORMATION IN CHEHEL CHESHMEH KHERAMEH MOUNTAIN (SOUTHEAST OF SHIRAZ)

Pages

  139-148

Abstract

 As OSTRACODS are excellent index in determining the paleoenvironment, age and paleoecology of sediments, the OSTRACODS in marls units 1 and 3 of TARBUR FORMATION have been studied. TARBUR FORMATION with 712 m thickness is divided into 6 units. In this study, 60 samples of marls units 1 and 3 have been washed, and studied and totally 21 species identified. The OSTRACODS indicate a MAESTRICHTIAN age and warm, oxygen-rich and shallow depositional environment for the studied units.

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    APA: Copy

    PARVANEH NEJAD SHIRAZI, M., AMIRI BAKHTIAR, H., & ABDOLLAHI, P.. (2011). INTRODUCING THE OSTRACODS IN MARLS UNITS 1 AND 3 (K1 AND K3) OF TARBUR FORMATION IN CHEHEL CHESHMEH KHERAMEH MOUNTAIN (SOUTHEAST OF SHIRAZ). JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 27(3 (44)), 139-148. SID. https://sid.ir/paper/157089/en

    Vancouver: Copy

    PARVANEH NEJAD SHIRAZI M., AMIRI BAKHTIAR H., ABDOLLAHI P.. INTRODUCING THE OSTRACODS IN MARLS UNITS 1 AND 3 (K1 AND K3) OF TARBUR FORMATION IN CHEHEL CHESHMEH KHERAMEH MOUNTAIN (SOUTHEAST OF SHIRAZ). JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2011;27(3 (44)):139-148. Available from: https://sid.ir/paper/157089/en

    IEEE: Copy

    M. PARVANEH NEJAD SHIRAZI, H. AMIRI BAKHTIAR, and P. ABDOLLAHI, “INTRODUCING THE OSTRACODS IN MARLS UNITS 1 AND 3 (K1 AND K3) OF TARBUR FORMATION IN CHEHEL CHESHMEH KHERAMEH MOUNTAIN (SOUTHEAST OF SHIRAZ),” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 27, no. 3 (44), pp. 139–148, 2011, [Online]. Available: https://sid.ir/paper/157089/en

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