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Information Journal Paper

Title

NANNOSTRATIGRAPHY OF GURPI FORMATION IN DARE- SHAHR SECTION (SE ILAM)

Pages

  299-308

Abstract

NANNOFOSSILS are good for biostratigraphy, since they are abundant, planktonic, rapidly evolving and largely cosmopolitan especially in the late Cretaceous. With respect to this reality and due to the lack of any precise paleontological study, the NANNOFOSSILS of GURPI FORMATION were investigated in the DARE-SHAHR. This formation consists of marl and shale and two members (Lopha and Emam Hassan limestones). In this study, for the first time, 24 genera and 48 species of NANNOFOSSILS were identified. According to the stratigraphic distribution of calcareous NANNOPLANKTONS the study section is Late Santonian to Early Danian age corresponding to CC16-CC26 (Sissingh 1977) and NP1-NP2 (Martini 1971). The presence of Biantolithus sparsus, Cruciplacolithus primus, Micula prinsii, indicate that the K/T boundary is continues and within GURPI FORMATION in DARE-SHAHR section.

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References

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APA: Copy

HADAVI, F., & RASA EZADI, M.M.. (2009). NANNOSTRATIGRAPHY OF GURPI FORMATION IN DARE- SHAHR SECTION (SE ILAM). JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), 4(4), 299-308. SID. https://sid.ir/paper/127105/en

Vancouver: Copy

HADAVI F., RASA EZADI M.M.. NANNOSTRATIGRAPHY OF GURPI FORMATION IN DARE- SHAHR SECTION (SE ILAM). JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY)[Internet]. 2009;4(4):299-308. Available from: https://sid.ir/paper/127105/en

IEEE: Copy

F. HADAVI, and M.M. RASA EZADI, “NANNOSTRATIGRAPHY OF GURPI FORMATION IN DARE- SHAHR SECTION (SE ILAM),” JOURNAL OF GEOTECHNICAL GEOLOGY (APPLIED GEOLOGY), vol. 4, no. 4, pp. 299–308, 2009, [Online]. Available: https://sid.ir/paper/127105/en

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