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Information Journal Paper

Title

MICROBIOSTRATIGRAPHY OF THE CENOMANIAN-TURONIAN BOUNDARY IN EAST OF THE KOPEH-DAGH (HAMAM QALE) SECTION

Pages

  31-44

Abstract

 The Upper Cenomanian–Lower Turonian deposits of Hamam-Qal’eh section (east Kopeh- Dagh) were studied based on foraminifera from biostratigraphic point of view. Based on the standard biozonation, three biozones for Upper Cenomanian–Lower Turonian deposits were differentiated in a 1m interval sampling (R. cushmani, W. archaeocretacea, H.helvetica). Whiteinela archaeocretacea zone was divided into three subzones. This recorded zonation confirms that the sedimentation was continuous at the Cenomanian-Turonian boundary.

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    APA: Copy

    GHOURCHAEI, SH., VAHIDINIA, M., MAHMUDIE GHARAEI, M.H., & POURMOAFI, S.M.. (2011). MICROBIOSTRATIGRAPHY OF THE CENOMANIAN-TURONIAN BOUNDARY IN EAST OF THE KOPEH-DAGH (HAMAM QALE) SECTION. IRANIAN JOURNAL OF GEOLOGY, 5(19), 31-44. SID. https://sid.ir/paper/129429/en

    Vancouver: Copy

    GHOURCHAEI SH., VAHIDINIA M., MAHMUDIE GHARAEI M.H., POURMOAFI S.M.. MICROBIOSTRATIGRAPHY OF THE CENOMANIAN-TURONIAN BOUNDARY IN EAST OF THE KOPEH-DAGH (HAMAM QALE) SECTION. IRANIAN JOURNAL OF GEOLOGY[Internet]. 2011;5(19):31-44. Available from: https://sid.ir/paper/129429/en

    IEEE: Copy

    SH. GHOURCHAEI, M. VAHIDINIA, M.H. MAHMUDIE GHARAEI, and S.M. POURMOAFI, “MICROBIOSTRATIGRAPHY OF THE CENOMANIAN-TURONIAN BOUNDARY IN EAST OF THE KOPEH-DAGH (HAMAM QALE) SECTION,” IRANIAN JOURNAL OF GEOLOGY, vol. 5, no. 19, pp. 31–44, 2011, [Online]. Available: https://sid.ir/paper/129429/en

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