Volume 32 (2022)
Volume 31 (2021)
Volume 30 (2020)
Volume 29 (2020)
Volume 28 (2019)
Volume 27 (2018)
Volume 26 (2017)
Volume 25 (2016)
Volume 24 (2015)
Volume 23 (2014)
Volume 22 (2013)
Volume 21 (2012)
Volume 20 (2011)
Volume 19 (2010)
Volume 18 (2009)
Volume 17 (2008)
Volume 16 (2007)
Stratigraphy and Palaeontology
Calcareous nannofossil biostratigraphy of Paleocene ‒ middle Eocene interval at NE Kazeroon

A. Mahanipour; Reza Afrooz

Volume 29, Issue 113 , November 2019, , Pages 25-34


  In the present study, calcareous nannofossil biostratigraphy was investigated at the Paleocene ‒ middle Eocene interval at northeast Kazerun (Shahneshin anticline). A thickness of 50 m from the upper part of Gurpi ‒ lower part of Pabdeh formations is investigated and mainly consists of marly limestone, ...  Read More

Stratigraphy and Palaeontology
Structural evolution of Zoophycos group trace fossils from the Pabdeh Formation (Paleocene–Oligocene), SE of Ilam province, SW Iran

Zahra Hosseini Asgarabadi; Nasrollah Abbassi; Hassan Mohseni; Saeed Khodabakhsh

Volume 29, Issue 113 , November 2019, , Pages 211-220


  The Pabdeh Formation (Paleocene to Oligocene in age) comprises alternation of marl and limestone with the Purple Shale at the base is well exposed on the flanks of the Kabir-Kuh. Thalassinoides, Rhizocorallium, Planolites, Chondrites, cf. Rosselia, Spirophyton and Zoophycos were found in the limestone ...  Read More

Lithostratigraphy and biostratigraphy of the Pabdeh Formation at Chahardeh village section (Izeh zone, Khuzestan province)

N. Hadavandkhani; A. Sadeghi; M. H. Adabi; A. R. Tahmasbi

Volume 27, Issue 107 , June 2018, , Pages 137-150


  The Pabdeh Formation with a thickness of 797.2 m. and 4 lithological units (purple shale (144.25 m.), lower limestone and marl (221.75 m.), limestone (73.5 m.) and upper limestone and marl (357.7 m.) is stretched at Chahardeh village stratigraphic section in Izeh zone.. Biostratigraphic studies led to ...  Read More

Determining microfacies of phosphate bearing Pabdeh Formation in paleogene carbonate ramp of Lar anticline (Northeast of Gachsaran)

Sh. Shariati

Volume 27, Issue 105 , December 2017, , Pages 97-104


  Pabdeh Formation comprised carbonate-siliciclastic succession of Zagros fold-thrust belt in south west of Iran. The studied area is located in Lar Mountains (North East of Khami anticline) which extend in a northwest-southeast direction Parallel to the Zagros sedimentary basin trend. Microfacies analysis ...  Read More

Biostratigraphy of Oligocene and Lower Miocene Strata along a Transect from Well "A" in Persian Gulf to Semirum Section in High Zagros

M Joudaki; D Baghbani; S.A Aghanabati; B Soleimani; H Asilian; B Ariafar

Volume 24, Issue 96 , September 2015, , Pages 151-158


  In order to biostratighraphy and to discover relationships between biozones of  the Oligocene and lower Miocene strata in Zagros foreland basin, Zagros simply folded belt and High Zagros area, 10 stratigraphic sections along a transect from well "A" in Persian Gulf to Semirum section in High Zagros ...  Read More

Calcareous Nannofossil Biostratigraphy of Pabdeh Formation at Gurpi Anticline

A Ahifar; A Kani; H Amiri Bakhtiar

Volume 24, Issue 95 , June 2015, , Pages 107-120


  Pabdeh Formation has been investigated in three sections viz. the Type Section, Tang-e Hatti and the northern limb of Gurpi Anticline within the ZagrosSedimentaryBasin with emphasis on calcareous nannofossils. Study of microscope slides prepared from the 1508 collected samples resulted in determination ...  Read More

Paleoecology and Paleoenvironment of the Basal Purple Shales of the Pabdeh Formation at Bisheh-Deraz Section, Southwest of Iran

J Rabbani; E Ghasemi-Nejad; A.R Ashouri; M Vahidinia

Volume 24, Issue 94 , March 2015, , Pages 165-172


  The basal unit of the Pabdeh Formation at Bisheh-Deraz section composes of 47m purple to green to grey shale and marl. These beds gradually change to shale and argillaceous limestone in the top of the section. In order to study paleoecology and paleoenvironment of these beds, palynological evidences ...  Read More

Calcareous Nannofossils Biostratigraphy of the Upper Part of Gurpi Formation- Lower Part of Pabdeh Formation (Purple shale) at the North-East of Gurpi Anticline

Mohammad Parandavar; A Mahanipur; S. A Aghanabati; S. A. Hoseini

Volume 23, Issue 89 , December 2013, , Pages 187-198


   In this study the upper part of Gurpi Formation and the lower part of Pabdeh Formation have been investigated with regard to the calcareous nannofossils. The thinkness of the studied section is about 127 meter and it consists of Marls, gray-green shales and purple shales. 50 genus and 101 species ...  Read More

The Pabdeh-Asmari Boundary Facies in Kuh e-Asmari Section: Evidence for Unconformable Ruplian-Chattian Boundary in Iran

Hadi Amin-Rasouli; Y. Lasemi; M. Ghomashi; S. Zaheri

Volume 21, Issue 83 , December 2012, , Pages 59-66


  The uppermost layers of the Pabdeh Formation in Kuh e-Asmari section consist of microbial (tufa and stromatolite) facies interpreted to have been deposited in a lacustrine environment. These deposits are unconformably overlain by basal anhydrite and transitional zone of the Asmari and Pabdeh Formations. ...  Read More

Depositional Environment and Sequence Stratigraphy of the Pabdeh Formation in Shiraz area

R. Mirzaee Mahmoodabadi; Y. Lasemi; M. Afghah

Volume 19, Issue 73 , January 2009, , Pages 139-146


  Shaley Pabdeh Formation (Paleocene-Oligomiocene) expanded in Fars, Khozestan and Lorestan. Lower Lithostratigraphical limit with Gurpi Formation recognized by purple shale. Upper Lithostratigraphical limith with Asmari Formation is transitional. In order to study sedimentary environments and sequence ...  Read More

Clay Mineral Study of Pabdeh Formation in Type Section and it´s Comparison with NGS Data from Kupal Oil Field (Well No. 12 & 38)

M. Hosseini-Barzi; R. Alinejad-Kurdi; H. Ghalavand

Volume 17, Issue 67 , February 2008, , Pages 198-209


  The calcimeteric analysis of samples from Pabdeh Formation, in type section (north of Dezful embayment subzone), represent a marl and shaly marl lithology. SEM images from these samples represent chlorite flakes with diagenetic origin (transformation of illite to chlorite) and imply the possible existence ...  Read More