Biostratigraphy of the Gurpi Formation based on planktonic foraminifera in Bishe-deraz section, South of Ilam

Q: How can I download an article?

To download an article from SID, first log in to the site, search for the article title, and click on the 'Download Article' option.

Q: How can I download an ISI article?

To download an ISI article on SID, enter the keyword or article title in the search bar, view the relevant results, click on the desired article, and select the 'Download Article' option.

Q: How can I access the SID database?

To access the SID database, visit SID.ir, create an account, and log in to access scientific resources.

Q: Is downloading articles from SID free?

Some articles on SID are available for free, while others require payment. Details are specified on the article's page.

AMIRI F.; ZAREI E.

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

Journal Paper

Paper Information

Journal: GEOSCIENCES Year:2020 | Volume:29 | Issue:115 Page(s): 17-26

Download Full-Text

Persian Verion

View:

429

Download:

Cites:

Information Journal Paper

Title

Biostratigraphy of the Gurpi Formation based on planktonic foraminifera in Bishe-deraz section, South of Ilam

Author(s)

AMIRI F. | ZAREI E. | Issue Writer Certificate

Keywords

BiostratigraphyQ1

Gurpi FormationQ1

Planktonic foraminiferalQ1

ZagrosQ1

Abstract

The Gurpi Formation in Bishe-deraz Section, south of Ilam, consists of 201m marl with intercalations of limy marl with two formal members of Seymareh (Lopha) and Emam-Hasan. The formation overlies the Ilam Formation and is gradationally overlain by the purple shales of the basal part of the Pabdeh Formation. The Gurpi Formation was divided to 9 biozone on the basis of planktonic foraminifera which almost are cosmopolitan and consist of: 1-Radotruncana calcarata Taxon-Range Zone. 2-Globotruncanita stuartiformis Partial-Range Zone. 3-Globotruncana aegyptiaca Interval Zone. 4-Gansserina gansseri Interval Zone. 5-Contusotruncana contusa Interval Zone. 6-Abathomphalus mayaroensis Interval Zone. 7-Praemurica uncinata Interval Zone. 8-Morozovella angulata Interval Zone. 9-Globanomalina pseudomenardii Interval Zone. The formation was deposited from upper Campanian through late Paleocene (Selandian-Thanetian? ) according to the planktonic foraminifera recorded. A distinct hiatus was confirmed at the Cretaceous-Paleogene boundary according to microbiostratigraphic and sedimentologic studies and also field work observation.

Cites

No record.

References

No record.

Cite

APA: Copy

AMIRI, F., & ZAREI, E.. (2020). Biostratigraphy of the Gurpi Formation based on planktonic foraminifera in Bishe-deraz section, South of Ilam. GEOSCIENCES, 29(115 ), 17-26. SID. https://sid.ir/paper/378187/en

Vancouver: Copy

AMIRI F., ZAREI E.. Biostratigraphy of the Gurpi Formation based on planktonic foraminifera in Bishe-deraz section, South of Ilam. GEOSCIENCES[Internet]. 2020;29(115 ):17-26. Available from: https://sid.ir/paper/378187/en

IEEE: Copy

F. AMIRI, and E. ZAREI, “Biostratigraphy of the Gurpi Formation based on planktonic foraminifera in Bishe-deraz section, South of Ilam,” GEOSCIENCES, vol. 29, no. 115 , pp. 17–26, 2020, [Online]. Available: https://sid.ir/paper/378187/en

Related Journal Papers