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Information Journal Paper

Title

THE NEW EVIDENCE OF ALBIAN-CENOMANIAN BOUNDARY BIOSTRATIGRAPHY FOR FIRST TIME FROM IRAN

Pages

  97-104

Abstract

 The SARVAK FORMATION in Tang -e-Chenarbashi with 712 meters thickness encompasses Albian- Cenomanian planktonic foraminifera. In the studied section, surveying the Albian- Cenomanian boundary is indicated that Rotalipora appeninica Zone not be recognized. Paracostellagerina libyca can be to consider as a marker for ALBIAN-CENOMANIAN BOUNDARY, absence of the Albian marker foraminifera permit us to consider the first occurrence of this species as the bigining of Cenomanian. Also Favosella voloshinae, Paracostellagerina libyca are report for first time from Iran.

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    APA: Copy

    DANESHIAN, J., YOUNESI, K.R., & MOALLEMI, S.A.. (2012). THE NEW EVIDENCE OF ALBIAN-CENOMANIAN BOUNDARY BIOSTRATIGRAPHY FOR FIRST TIME FROM IRAN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, 28(2 (47)), 97-104. SID. https://sid.ir/paper/157108/en

    Vancouver: Copy

    DANESHIAN J., YOUNESI K.R., MOALLEMI S.A.. THE NEW EVIDENCE OF ALBIAN-CENOMANIAN BOUNDARY BIOSTRATIGRAPHY FOR FIRST TIME FROM IRAN. JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES[Internet]. 2012;28(2 (47)):97-104. Available from: https://sid.ir/paper/157108/en

    IEEE: Copy

    J. DANESHIAN, K.R. YOUNESI, and S.A. MOALLEMI, “THE NEW EVIDENCE OF ALBIAN-CENOMANIAN BOUNDARY BIOSTRATIGRAPHY FOR FIRST TIME FROM IRAN,” JOURNAL OF STRATIGRAPHY AND SEDIMENTOLOGY RESEARCHES, vol. 28, no. 2 (47), pp. 97–104, 2012, [Online]. Available: https://sid.ir/paper/157108/en

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