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)
Stratigraphy and Palaeontology
Systematic Paleontology of Alveolinids in the red continental - clastic Hormak formation, South Eastern of Iran, North of Zahedan, Hormak Section

Reza Moezzi nasab; Mohammad Nabi Gorgij; Mohammad Reza Bakhshi mohebbi

Volume 28, Issue 109 , September 2018, , Pages 229-236

https://doi.org/10.22071/gsj.2017.81959.1084

Abstract
  Hormak Section consist of alternation of Oligomictic conglomerate with mainly Alveolinids and Nummulitid bearing calcareous pebbles and afew andesits, basalt and rhyolitic tuff pebbles, Pebbly Sandstone and red shale. The Sourse of red continental - clastic Hormak formation conglomerate probably was ...  Read More

Facies analyses and sedimentary environments of Upper Cretaceous carbonate deposits in North Bandan (Daghal section)

SH Habibimood; M.N Gorgij; KH Khosrotehrani; A Saidi; S.A Aghanabati

Volume 25, Issue 99 , June 2016, , Pages 39-46

https://doi.org/10.22071/gsj.2016.40769

Abstract
  The studied section is located in the vicinity of the village Daghal on the Zabol – Nehbandan road, 100 kilometersfrom Zabol. The strata under study are 55.57 meters thick here and lie nonconformably on the igneous rocks while the upper contact is now known. In this study the mentioned strata are ...  Read More

Lower Permian Fusulinids Biostratigraphy in Chili Formation (Member of Khan Group) in the Kalmard Area, Eastern Central Iran (Rahdar Section)

H. Yarahmadzahi; M. N. Gorgij; S. A. Aghanabati; A. Saeidi

Volume 22, Issue 87 , December 2013, , Pages 75-82

https://doi.org/10.22071/gsj.2013.53832

Abstract
  The studied section is located west of Tabas (Rahdar Mountion) in the Kalmard Block. The newly named Chili formation, as the first rock unit of the Khan group consist mainly of arenacous limestone, limestone and dolomite and has disconformity contact with underlying lower carboniferous deposits (Padeh ...  Read More