Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province

In order to study biostratigraphy of the Pabdeh Formation in southwest of Ilam, Marbera section was selected. In this section, Pabdeh Formation is mainly consists of marls, shale and marly limestones. The study of calcareous nannofossils led to the recognition of 72 species and 26 genera. According...

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Main Authors: saeideh senemari, Afsaneh Deh Bozrgi
Format: Article
Language:fas
Published: University of Isfahan 2017-11-01
Series:Journal of Stratigraphy and Sedimentology Researches
Subjects:
Online Access:http://jssr.ui.ac.ir/article_22227_6e321f359b0eb36089ba4e1fdf626768.pdf
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spelling doaj-b7525d2571c44784b0d8b257db016fb72020-11-24T22:11:45ZfasUniversity of IsfahanJournal of Stratigraphy and Sedimentology Researches 2008-78882423-80072017-11-01333799410.22108/jssr.2017.100648.100022227Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam provincesaeideh senemari0Afsaneh Deh Bozrgi1University ofاستادیار گروه زمین‌شناسی دانشگاه بین‌المللی امام خمینی (ره) قزوینIn order to study biostratigraphy of the Pabdeh Formation in southwest of Ilam, Marbera section was selected. In this section, Pabdeh Formation is mainly consists of marls, shale and marly limestones. The study of calcareous nannofossils led to the recognition of 72 species and 26 genera. According to the first and last occurrence of index species and based on Martini (1971) zonation, the following biozones are identified:, Tribrachiatus contortus Zone (NP10), Discoaster binodosus Zone (NP11), Tribrachiatus orthostylus Zone (NP12), Discoaster lodoensis Zone (NP13), Discoaster sunlodoensis Zone (NP14), Nannotetrina fulgens zone (NP15), Discoaster tanii nodifer Zone (NP16), Discoaster saipanensis Zone (NP17), Chiasmolithus oamaruensis Zone (NP18), Isthmolithus recurvus Zone (NP19), Sphenolithus pseudoradians Zone (NP20), Ericsonia Subdisticha zone (NP21), Helicosphaera reticulate Zone (NP22), Sphenolithus predistintus Zone (NP23), Sphenolithus distentus Zone (NP24), Sphenolithus ciperoensis Zone (NP25). As a result of this study and based on the obtained biozones, the age of Pabdeh Formation in southwest of Ilam, is Early Eocene (Ypresian) to Late Oligocene (Chattian).http://jssr.ui.ac.ir/article_22227_6e321f359b0eb36089ba4e1fdf626768.pdfIlamBiostratigraphyPaleogeneZagros BasinPabdeh Formation
collection DOAJ
language fas
format Article
sources DOAJ
author saeideh senemari
Afsaneh Deh Bozrgi
spellingShingle saeideh senemari
Afsaneh Deh Bozrgi
Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
Journal of Stratigraphy and Sedimentology Researches
Ilam
Biostratigraphy
Paleogene
Zagros Basin
Pabdeh Formation
author_facet saeideh senemari
Afsaneh Deh Bozrgi
author_sort saeideh senemari
title Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
title_short Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
title_full Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
title_fullStr Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
title_full_unstemmed Biostratigraphy of Pabdeh Formation based on calcareous nannofossils, southwest of Ilam, Ilam province
title_sort biostratigraphy of pabdeh formation based on calcareous nannofossils, southwest of ilam, ilam province
publisher University of Isfahan
series Journal of Stratigraphy and Sedimentology Researches
issn 2008-7888
2423-8007
publishDate 2017-11-01
description In order to study biostratigraphy of the Pabdeh Formation in southwest of Ilam, Marbera section was selected. In this section, Pabdeh Formation is mainly consists of marls, shale and marly limestones. The study of calcareous nannofossils led to the recognition of 72 species and 26 genera. According to the first and last occurrence of index species and based on Martini (1971) zonation, the following biozones are identified:, Tribrachiatus contortus Zone (NP10), Discoaster binodosus Zone (NP11), Tribrachiatus orthostylus Zone (NP12), Discoaster lodoensis Zone (NP13), Discoaster sunlodoensis Zone (NP14), Nannotetrina fulgens zone (NP15), Discoaster tanii nodifer Zone (NP16), Discoaster saipanensis Zone (NP17), Chiasmolithus oamaruensis Zone (NP18), Isthmolithus recurvus Zone (NP19), Sphenolithus pseudoradians Zone (NP20), Ericsonia Subdisticha zone (NP21), Helicosphaera reticulate Zone (NP22), Sphenolithus predistintus Zone (NP23), Sphenolithus distentus Zone (NP24), Sphenolithus ciperoensis Zone (NP25). As a result of this study and based on the obtained biozones, the age of Pabdeh Formation in southwest of Ilam, is Early Eocene (Ypresian) to Late Oligocene (Chattian).
topic Ilam
Biostratigraphy
Paleogene
Zagros Basin
Pabdeh Formation
url http://jssr.ui.ac.ir/article_22227_6e321f359b0eb36089ba4e1fdf626768.pdf
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