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)
Sedimentology
The Qatar-Cowbandi arc in Persian Gulf during Late Cretaceous- Eocene Epoch

naser abdi; Reza Moussavi-Harami

Volume 28, Issue 110 , December 2018, , Pages 13-22

https://doi.org/10.22071/gsj.2018.87684.1133

Abstract
  The Qatar-Cowbandi arc is a giant regional anticline with northeast- southwest direction, runs through the Qatar peninsula, extends northeastward through the Iranian sector of the Persian Gulf. The arc in the Iranian part is subject of the study meditation. In this paper the interpretation of 2D seismic ...  Read More

The Study of relation between fault and fracture systems based on subsurface data and analogue modeling: one of the Eastern Persian Gulf hydrocarbon fields

E. Kosari; A. Bahroudi; M. Talebian; A. Chehrazi

Volume 27, Issue 105 , December 2017, , Pages 157-166

https://doi.org/10.22071/gsj.2017.53939

Abstract
  One of the essential studies in exploration, exploitation and development of hydrocarbon fields is to evaluate the fault and fracture systems and the role that they can play in reservoir quality and geometry. If the hydrocarbon reservoir is a fractured carbonate reservoir, assessing the mentioned properties ...  Read More

Sedimentary environment, diagenesis and reservoir quality of Upper Sarvak Formation in the Persian Gulf

N Shahverdi; H Rahimpour- Bonab; M.R Kamali; B Esrafili- Dizagi

Volume 25, Issue 98 , March 2016, , Pages 55-66

https://doi.org/10.22071/gsj.2016.41161

Abstract
  The Albian-TuronianSarvak Formation is one of the main oil reservoirs in south and southwest Iran that hosts significant amount of hydrocarbon resources in this region. Facies analysis in seven oil fields of Persian Gulf led to identification of 7 microfaceis that are deposited in four facies belts in ...  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

https://doi.org/10.22071/gsj.2015.41712

Abstract
  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

Compilation of Seismic Attributes and Artificial Neural Networks in Identifying Fault Systems in the Hormuz Strait Area

M.S Mirkamali; H.R Ramazi; M.R Bakhtiari; H Ramesh

Volume 24, Issue 95 , June 2015, , Pages 351-358

https://doi.org/10.22071/gsj.2015.42125

Abstract
  This study has focused on identifying fault systems in the HormuzStrait area using compilation of seismic attributes and artificial neural networks. Faults and fractures play an important role in creating areas of high porosity and permeability. In addition, they cut off the cap and reservoir rocks along ...  Read More

Determination of Sedimentation Rate and Verification of Holocene Sediments in Northeastern Part of the Persian Gulf: ACase Study in Southern Bandar Abbas

R Lak; M Taghizadeh

Volume 24, Issue 94 , March 2015, , Pages 183-192

https://doi.org/10.22071/gsj.2015.42608

Abstract
  The Persian Gulf has an area about 240000 km2, considered as the northern part of the counterclockwise movement of Arabian Plate and as a recent example of Holocene carbonated sedimentary environment in dry (arid) climate. The basin volume, regarding to its average depth (36m), is estimated about 87,000km3. ...  Read More

Organic Geochemistry of Khowr-e-Mussa's Sediments and its Adjacent Marine Areas, Northwest of the Persian Gulf

R Behbahani; R Lak; N Chanani; G Hosseinyar

Volume 23, Issue 92 , September 2014, , Pages 55-67

https://doi.org/10.22071/gsj.2014.43652

Abstract
  In order to study of organic geochemistry of bed sediments in Khowr-e-Mussa and its adjacent marine areas, 61 surface sediment samples were collected. Based on granulometric analysis of the sediments, 4 major sedimentary types comprising mud, sandy mud, muddy sand, and slightly gravelly muddy sand were ...  Read More

Carbonate Marine Terraces of Qeshm Island, a Symbol of Sea Level Changes of the Persian Gulf in the Quaternary

P Rezaee; R Zarezadeh

Volume 23, Issue 92 , September 2014, , Pages 67-74

https://doi.org/10.22071/gsj.2014.43653

Abstract
  Qeshm is the largest island of the Persian Gulf and is located at the southern end of the folded Zagros zone. The stratigraphic units of the QeshmIsland include the Hormoz series, Mishan formation, Aghajari formation and the Quaternary deposits. The Quaternary calcareous marine terraces are an important ...  Read More

Porosity Types, Their Genesis and Reservoir Zonation of the Upper Carbonates of the Dalan Formation in the Surmeh Mountain Section and Persian Gulf

S Parham; M.R Kamali

Volume 23, Issue 92 , September 2014, , Pages 93-104

https://doi.org/10.22071/gsj.2014.43656

Abstract
  The Dalan Upper member (Permian) with carbonates and evaporite interlayer is one of the most important gas reservoirs in the folded Zagros area and Persian Gulf. In this investigation porosity types, their genesis and controlling factors have been studied at Surmeh surface section and a subsurface section ...  Read More

Introduction and Distribution of the Hyaline Foraminifera in Persian Gulf Coastal Sediments (from Bandar-e Lengeh to Bushehr)

M Sohrabi Mollayousefi; M Sahba

Volume 23, Issue 91 , June 2014, , Pages 89-95

https://doi.org/10.22071/gsj.2014.43778

Abstract
  The study area includes a part of the northern strip of Persian Gulf coast, a distance of approximately 650 kilometers. The Persian Gulf is a marginal, semi-closed, and shallow sea with salty and warm water. It has a circular flow in a clockwise direction along the coast of Iran, caused by the high range ...  Read More

Calcareous Nannoplankton of Holocene Sediment in the Persian Gulf (Shahid Rajaee Port)

A. Pouresmaeil; F. Hadavi; R. Lak

Volume 22, Issue 88 , December 2013, , Pages 111-120

https://doi.org/10.22071/gsj.2013.53684

Abstract
   In this study, a core with 10.5 m lenght and in shallow water in Bandar Abbas (Shahid Rajaee Port area) was studied based on calcareous nannoplankton. In this study, 52 samples of sediment cores were taken and prepared. Most species were photographed by light microscope. For the first time 21 genera ...  Read More

Description of Seismic Facies in Persian Gulf's Sediments, North of Qeshm Island

G. R Hosseinyar; R Moussavi-Harami; R Behbahani

Volume 23, Issue 89 , December 2013, , Pages 183-186

https://doi.org/10.22071/gsj.2013.53607

Abstract
  Using high-resolution shallow seismic data, we have investigated the seismic facies in northern Qeshm Island waterways in East of Persian Gulf. Seismic data obtained with Sub-bottom profiler and then interpreted by ISE software. Studies lead to recognizing 7 types seismic facies on seismic data. These ...  Read More

Microfacies Analysis, Sedimentary Environments and Diagenesis of the upper Carbonates of the Dalan Formation in the Persian Gulf, Iran

S. Parham; M. R. Kamali; F. Fayazi

Volume 22, Issue 86 , December 2012, , Pages 203-212

https://doi.org/10.22071/gsj.2012.54086

Abstract
  The Dalan Formation (Upper Permian) is mainly composed of limestone and dolostone with minor evaporite interbeds. Upper carbonates of the Dalan Formation constitute one of the main gas reservoirs in the Zagros fold thrust belt especially in the Fars and the Persian Gulf. The upper part of the Dalan Formation ...  Read More

Deliberation of Cenomanian- Coniacian Boundary based on Biostratigraphic and Lithostratigraphic Studies in Bahregansar Field, Presian Gulf

K. Kiarostami; S. H. Vaziri; B. Noori; S. Allahmadadi; F. Vakilbaghmisheh

Volume 21, Issue 82 , December 2011, , Pages 113-120

https://doi.org/10.22071/gsj.2011.54447

Abstract
  In order to investigate lithostratighraphical and biostratigraphical as well as determination of exact contact between the Sarvak and Ilam formations in oil well X-01 of Bahregansar field thin microscopic sections, final well reports and its illustrative diagram were studied. The Sarvak Formation with ...  Read More

Petroleum System Modeling of Lower Paleozoic in Persian Gulf Basin

S. Salehi Rad; S. Sherkati; F. Taati Qoaryem; M. H. Noroozi

Volume 20, Issue 79 , January 2011, , Pages 21-30

https://doi.org/10.22071/gsj.2011.54989

Abstract
  The Paleozoic sediments are noteworthy for many of petroleum geologists to research within Arabian Plate during last decades. Significant values of oil and gas was generated from the Silurian source rock in this area. This source rock has been modeled by commercial software's (PetroMod and Genex) in ...  Read More

Foraminiferal Biostratigraphy of the Gurpi and Ilam Formations in East of Kangan Port and Ivan well in Persian Gulf

J. Daneshian; D. Baghbani; Kh. Khosrow- Tehrani; L. Fazli

Volume 19, Issue 74 , February 2010, , Pages 157-162

https://doi.org/10.22071/gsj.2010.57348

Abstract
  In this study, foraminifera of the Ilam and Gurpi Formations, from Kuh-e- Assaluyeh section in east Kangan port in Boushehr province and Ivan well in Persian Gulf are investigated. Ilam Formation in Kuh-e-Assaluyeh section with 30 meter thickness and Ivan well with 68 meter thickness composed of limestone ...  Read More