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)
Sedimentology
Tectono-sedimentary Setting of Maastrichtian Deposits along NW-SE Transect in Fars Area, SE Zagros

Somayeh Parham; Alireza Piryaei; Mansur Ghorbani; Seyyed Reza Moosavi Harami

Volume 30, Issue 117 , December 2020, , Pages 253-264

https://doi.org/10.22071/gsj.2019.96479.1241

Abstract
  Late Cretaceous in Zagros encompasses regional tectonics and caused foreland basin to form in northeast of the Arabian Plate. Salt tectonics is also locally affected this area. One of the time periods that can better picture this tectono-sedimentary evolution is Maastrichtian. In order to investigate ...  Read More

Biostratigraphy and Palaeoecology of the Maestrichtian Deposits (Tarbur and Gurpi Formations) at Gardbishe Area (South of Borojen)

H. Vaziri-Moghaddam; A. Safari; S. Shahriari; A. Khazaei; A. Taheri

Volume 22, Issue 87 , December 2013, , Pages 143-162

https://doi.org/10.22071/gsj.2013.53846

Abstract
  In order to study the biostratigraphy and palaeoecology of the Maestichtian deposits (Tarbur and Gurpi formations) in High Zagros, Gardbishe section in south of Borojen was selected. The Tarbur deposits in this region are mainly composed of carbonate and clastic a rock which has been overlaind by Gurpi ...  Read More

Introducing Rudist of Tarbur Formation, Semirum and Khorramabad Sections

I. Maghfouri Moghaddam

Volume 20, Issue 77 , January 2010, , Pages 63-66

https://doi.org/10.22071/gsj.2010.55336

Abstract
  Rudists of the Tarbur Formation, in 7 km southwest of Semirum and 10 km north of Khorramabad, have been studied. Paleontological studies indicate that the age of the Tarbur Formation in both sections is Masstrichtian, and has a rich macrofossil fauna of rudist. The important types of rudist include Radiolites, ...  Read More