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مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

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Title

STRATIGRAPHY AND MICROPALEONTOLOGY OF THE PERMIAN ROCKS IN NW IRAN

Pages

  98-109

Abstract

 Various stratigraphical sections of the PERMIAN rocks in the northwest of IRAN (Azerbaijan) shows that this sequence consists Of Doroud, Ruteh, and Nesen formations in the southern flanks and Doroud, Surmaq, Julfa and Ali-Bashi formations in Zal And illanlu sections. The analysis and study of forminifera assemblages in the carbonate sequence of the area and the comparison of these Microfossils with other parts of IRAN and neighboring countries indicate that the age of carbonate units is Kubergandian to Dorashamian in Zal and ilIanlu areas and Kubergandian to Djulfian in others sections. Throughout the Azerbaijan, Lower PERMIAN shows a great HIATUS.Field investigation, rock and microfacies studies show many progressive and regressive phases in the PERMIAN sequence of Azerbaaijn.

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  • Cite

    APA: Copy

    SHAABANIAN, R., MOUMENI, I.. (2007). STRATIGRAPHY AND MICROPALEONTOLOGY OF THE PERMIAN ROCKS IN NW IRAN. GEOSCIENCES, 16(63), 98-109. SID. https://sid.ir/paper/31769/en

    Vancouver: Copy

    SHAABANIAN R., MOUMENI I.. STRATIGRAPHY AND MICROPALEONTOLOGY OF THE PERMIAN ROCKS IN NW IRAN. GEOSCIENCES[Internet]. 2007;16(63):98-109. Available from: https://sid.ir/paper/31769/en

    IEEE: Copy

    R. SHAABANIAN, I. MOUMENI, “STRATIGRAPHY AND MICROPALEONTOLOGY OF THE PERMIAN ROCKS IN NW IRAN,” GEOSCIENCES, vol. 16, no. 63, pp. 98–109, 2007, [Online]. Available: https://sid.ir/paper/31769/en

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