Volume 34 (2024)
Volume 33 (2023)
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)
Depositional and post-depositional history of the Guri Member in the south-east of Zagros sedimentary basin

A. Zohdi; S. A. Moallemi; M. A. Salehi

Volume 27, Issue 106 , March 2018, , Pages 129-142

https://doi.org/10.22071/gsj.2018.58327

Abstract
  In the Zagros sedimentary basin, the maximum thickness of the Guri Member carbonates is belonging to the eastern parts of the Bandar-Abbas region. In this research, the Guri Member in five outcrops at the Bandar-Abbas region has been sedimentological and stratigraphic studied. The Guri Member mainly ...  Read More

Sedimentary Environment, Diagenesis and Geochemistry of the Fahliyan Formation in the Type Section (Fahliyan Anticline) and Gachsaran Oil Field

M. A. Salehi; M. H. Adabi; H. Ghalavand; M. Khatibi-Mehr

Volume 19, Issue 76 , January 2010, , Pages 33-44

https://doi.org/10.22071/gsj.2010.55642

Abstract
  The Fahliyan Formation with the age of Lower Cretaceous (Berriasian-Hauterivian) were studied for microfacies analysis, diagenesis and original carbonate mineralogy in the type section at Fahliyan Anticline and subsurface section in well number 55 of Gachsaran Oil Field. Petrographic studies led to the ...  Read More

Diagenesis and Geochemistry of the Ziyarat Formation in the Type Section, Tochal, (Alborz (

M. H. Adabi; M. Khatibi Mehr; A. Moallemi; A. Sadeghi; M. A. Salehi

Volume 19, Issue 73 , January 2009, , Pages 153-163

https://doi.org/10.22071/gsj.2010.57219

Abstract
  The Ziyarat Formation is an Upper Paleocene to Middle Eocene carbonate sequences, located in North of Tochal Village (south-east of Tehran), near Emam Zadeh Abdollah. The Ziyarat Formation with the total thickness of 212.5 m conformably overlies the Fajan conglomerate and is overlain by greenish tufaceous ...  Read More