Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)

In order to determine stratigraphy and the introduction of biozonationes in the Pabdeh Formation based on the new planktonic foraminifera biozonationes in the Thethys strict, one stratigraphic sections in the Izeh zone at Gurpi anticline are selected and sampled. The thickness of the Pabdeh Formatio...

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Main Authors: Nasrin Hadavandkhani, Abbas Sadeghi, Mohammad Hossein Adabi, Alireza Tahmasbi Sarvestani
Format: Article in Journal/Newspaper
Language:Persian
Published: University of Isfahan 2017
Subjects:
Online Access:https://doi.org/10.22108/jssr.2017.21620
https://doaj.org/article/6bc38be48d6046a49ee027e9e78cf840
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spelling ftdoajarticles:oai:doaj.org/article:6bc38be48d6046a49ee027e9e78cf840 2023-05-15T18:00:32+02:00 Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan) Nasrin Hadavandkhani Abbas Sadeghi Mohammad Hossein Adabi Alireza Tahmasbi Sarvestani 2017-06-01T00:00:00Z https://doi.org/10.22108/jssr.2017.21620 https://doaj.org/article/6bc38be48d6046a49ee027e9e78cf840 FA per University of Isfahan http://jssr.ui.ac.ir/article_21620_0e61809919238747ae9477d8352fc38b.pdf https://doaj.org/toc/2008-7888 https://doaj.org/toc/2423-8007 2008-7888 2423-8007 doi:10.22108/jssr.2017.21620 https://doaj.org/article/6bc38be48d6046a49ee027e9e78cf840 Journal of Stratigraphy and Sedimentology Researches, Vol 33, Iss 2, Pp 1-18 (2017) Pabdeh Formation Biostratigraphy Lithostratigraphy Izeh Tange Hatti Stratigraphy QE640-699 article 2017 ftdoajarticles https://doi.org/10.22108/jssr.2017.21620 2022-12-31T08:47:38Z In order to determine stratigraphy and the introduction of biozonationes in the Pabdeh Formation based on the new planktonic foraminifera biozonationes in the Thethys strict, one stratigraphic sections in the Izeh zone at Gurpi anticline are selected and sampled. The thickness of the Pabdeh Formation in this section is 672 m., and 4 lithological units (Purple shale (106.25 m. thickness), Lower limestone and marl (50/75 m. thickness), Limestone (295 m. thickness) and Upper limestone and marl (220 m. thickness)) in Chahardeh stratigraphic section at Izeh zone. Biostratigraphic studies led to recognition of 30 genera and 141 species of planktonic foraminifera and then 21 biozones in realm (Wade et al. (2011) were identified. These identified biozones (P3-P5 (Paleocene),E1-E16 (Eocene), O1(Oligocene)) in the studied section in Izeh zone are in well correlated with biozones of Tethys region. Based on the indicated biozones and fossil contents, the age of the Pabdeh Formation is Middle Paleocene (Selandian) - Late Oligocene (Chattian). Article in Journal/Newspaper Planktonic foraminifera Directory of Open Access Journals: DOAJ Articles
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language Persian
topic Pabdeh Formation
Biostratigraphy
Lithostratigraphy
Izeh
Tange Hatti
Stratigraphy
QE640-699
spellingShingle Pabdeh Formation
Biostratigraphy
Lithostratigraphy
Izeh
Tange Hatti
Stratigraphy
QE640-699
Nasrin Hadavandkhani
Abbas Sadeghi
Mohammad Hossein Adabi
Alireza Tahmasbi Sarvestani
Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
topic_facet Pabdeh Formation
Biostratigraphy
Lithostratigraphy
Izeh
Tange Hatti
Stratigraphy
QE640-699
description In order to determine stratigraphy and the introduction of biozonationes in the Pabdeh Formation based on the new planktonic foraminifera biozonationes in the Thethys strict, one stratigraphic sections in the Izeh zone at Gurpi anticline are selected and sampled. The thickness of the Pabdeh Formation in this section is 672 m., and 4 lithological units (Purple shale (106.25 m. thickness), Lower limestone and marl (50/75 m. thickness), Limestone (295 m. thickness) and Upper limestone and marl (220 m. thickness)) in Chahardeh stratigraphic section at Izeh zone. Biostratigraphic studies led to recognition of 30 genera and 141 species of planktonic foraminifera and then 21 biozones in realm (Wade et al. (2011) were identified. These identified biozones (P3-P5 (Paleocene),E1-E16 (Eocene), O1(Oligocene)) in the studied section in Izeh zone are in well correlated with biozones of Tethys region. Based on the indicated biozones and fossil contents, the age of the Pabdeh Formation is Middle Paleocene (Selandian) - Late Oligocene (Chattian).
format Article in Journal/Newspaper
author Nasrin Hadavandkhani
Abbas Sadeghi
Mohammad Hossein Adabi
Alireza Tahmasbi Sarvestani
author_facet Nasrin Hadavandkhani
Abbas Sadeghi
Mohammad Hossein Adabi
Alireza Tahmasbi Sarvestani
author_sort Nasrin Hadavandkhani
title Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
title_short Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
title_full Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
title_fullStr Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
title_full_unstemmed Stratigraphy and the introduction of new biozonationes in the Pabdeh Formation (Tange Hatti section, Izeh zone, Khuzestan)
title_sort stratigraphy and the introduction of new biozonationes in the pabdeh formation (tange hatti section, izeh zone, khuzestan)
publisher University of Isfahan
publishDate 2017
url https://doi.org/10.22108/jssr.2017.21620
https://doaj.org/article/6bc38be48d6046a49ee027e9e78cf840
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_source Journal of Stratigraphy and Sedimentology Researches, Vol 33, Iss 2, Pp 1-18 (2017)
op_relation http://jssr.ui.ac.ir/article_21620_0e61809919238747ae9477d8352fc38b.pdf
https://doaj.org/toc/2008-7888
https://doaj.org/toc/2423-8007
2008-7888
2423-8007
doi:10.22108/jssr.2017.21620
https://doaj.org/article/6bc38be48d6046a49ee027e9e78cf840
op_doi https://doi.org/10.22108/jssr.2017.21620
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