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 of longitudinal bars in the Elyato river (South Western Fariman)

H Ghaderi Fijani; M Khanehbad; R Moussavi Harami; A. Mahboubi

Volume 26, Issue 101 , December 2017, , Pages 69-78


  The elongated Elyato River catchment, covering about 52.89 Km2 areas, is located in southwestern Fariman. To understand the grain size variation and effective factors in downstream fining, 35 samples from central axis of Longitudinal Bars have been collected and analyzed. The results indicate that the ...  Read More

Provenance of shales of the Kashafrud Formation in the Navia section (West of Bojnourd), based on geochemical data

N. Sarbaz; A. Mahboubi; R. Moussavi-Harami; M. Khanehbad

Volume 26, Issue 104 , September 2017, , Pages 199-210


  The Koppeh- Dagh Basin in the northeast Iran formed after closure of the Paleotethys in the south of Turan plate. Kashafrud Formation in the Navia Section (west of Bojnourd) with a thickness of 749 m is composed of silici-clastic rocks (conglomerate, sandstone and shale). In order to interpret provenance ...  Read More

Stratigraphy and Palaeontology
Sequence stratigraphy of the Aitamir Formation (Albian-Cenomanian) in Baghak and shurijeh sections-east Koppeh Dagh Basin

M. Allameh; A. Mahboubi; R. Moussavi-Harami; M. Khanehbad

Volume 26, Issue 103 , June 2017, , Pages 3-12


  The Aitamir Formation (Albian-Cenomanian) composed of siliciclastic rocks and several carbonate horizons. In order to study depositional environment and sequence stratigraghy, two stratigraghic sections studied in east Koppeht Dagh basin near the Baghak and Shurijeh villages. Field and petrograghic studies ...  Read More

Depositional environment, electrofacies and sequence stratigraphy of the Fahliyan Formation (lower Cretaceous), Abadan plain

A Ramezani Akbari; H Rahimpor-Bonab; M.R Kamali; R Moussavi-Harami; A Kadkhodaie

Volume 26, Issue 102 , March 2017, , Pages 339-350


  The Fahliyan Formation of Khami Group is hosting important hydrocarbon reserves in Iran and also is a main reservoir rock in the Abadan Plain oil fields which is Neocomian in age. In the studied wells its thickness is about 440 meters. In the Abadan Plain, the Fahliyan Formation transitionally overlies ...  Read More

Hydrogeochemical Study of Water Resources in Shahid Hashemi-Nejad Gas Refinery and Surrounding Areas Using Compound Diagrams, Saturation Indices and Ionic Ratios

M Tajbakhshian; M.H Mahmudy; A Mahboubi; R Moussavi Harami; I Ejlali

Volume 25, Issue 97 , December 2016, , Pages 71-84


  Hydrogeochemistry of surface and ground waters is a useful way to identify performing reactions in aquifers and also in recognizing effective natural and anthropogenic polluting factors in these sources. In order to study surface and ground waters quality of shahid Hashemi- Nejad gas refinery region, ...  Read More

Geochemistry of Streambed Sediments of Sarbaz River, South East of Iran: Determining Sediment Provenance and its Impact on Possible Environmental Pollution

M Shahraki; M.H Mahmudy Gharaie; R Moussavi-Harami; A Ahmadi

Volume 25, Issue 97 , December 2016, , Pages 237-250


  In this research the catchment of the Sarbaz river, SE Iran, has been studied to determine sediment provenance and its possible pollution potential. 30 sediment samples collected from the riverbed were analyzed for major and trace elements, using combined XRF and AAS methods. Based on major and trace ...  Read More

Origin of limestone conglomerates in the Unit 2 of Deh-Sufiyan Formatrion, Mila Group, Central Alborz, Northern Iran

A Bayet-Goll; R Moussavi-Harami; A Mahboubi

Volume 25, Issue 100 , September 2016, , Pages 79-90


  Carbonate deposits of members 1 to 2 of the Mila Group (Middle Cambrian) in Central Alborz that call the Deh-Sufiyan Formation in this research, were studied in Shahmirzad, Tueh-Darvar, Mila-Kuh and Deh-Molla sections. The Unit 2 of Deh-Sufiyan Formatrion in Central Alborz of Northern Iran consists mainly ...  Read More

Affection of Diagenesis on Reservoir Quality of Dariyan Formation in South Pars Field

M.R Rahmani; R Moussavi – Harami; M Arian

Volume 25, Issue 100 , September 2016, , Pages 165-178


  Dariyan formation is one of the oil reservoirs in the south pars field. This formation has been studied in wells SPO-1, SPO -2 and Spo-3. Thickness of Dariyan formation in mentioned wells are 109, 113 and 114 meters respectively. Based on the studies of thin sections from the Dariyan formation of three ...  Read More

Sedimentary Facies and Sequence Stratigraphy of Qom Formation Deposits in NE Delijan,NW Central Iran

M Karavan; A Mahboubi; H Vaziri-Moghaddam; R Moussavi-Harami

Volume 24, Issue 94 , March 2015, , Pages 229-236


  The Oligocene Qom Formation deposits in NW Central Iran (NE Delijan) are widespread in NE-SW trend.Four members of the Qom Formation (unknown, a, b& c1) in the study area consist of mainly marly limestone, limestone, sandy limestone and a minor amounts of sandstone. It disconformablyoverliesthe Lower ...  Read More

The Trace Fossil Cruziana and Rusophycus: A Study from the Ordovician Succession of Kalmard Block, Central Iran

A. Bayet-Goll; R. Moussavi-Harami; A. Mahboubi

Volume 22, Issue 87 , December 2013, , Pages 101-112


  Trace fossils are abundant in the clastic succession throughout the Shirgesht Formation of Kalmard Block, Central Iran. At certain horizons there are beds full of Cruziana and Rusophycus. This study presents an evaluation of the arthropod ichnotaxa of the Cruziana and Rusophycus from the Ordovician succession ...  Read More

Microbiostratigraphy of the Aitamir Formation in North West of Kopeh Dagh Basin (Maraveh Tappeh Section)

M. Motamedalshariati; A. Sadeghi; H. Vaziri Moghadam; R. Moussavi Harami

Volume 22, Issue 85 , December 2013, , Pages 225-236


  A stratigraphic section in west of Maraveh Tappeh town has been selected and measured in order to study the Aitamir Formation in north west of Kopeh Dagh. The Aitamir Formation with 1070 m thickness, consists of sandstone in the lower part and shale and marl in the upper part. The lower and upper boundaries ...  Read More

Facies Analysis and Environmental Interpretation of Planolites and Palaeophycus Trace Fossils from Paleozoic Sediments of Mid-Iran Zone

A. Bayat Gol; N. Abbassi; A. Mahboubi; R. Moussavi-Harami; H. Amin Rasouli

Volume 21, Issue 83 , December 2012, , Pages 185-196


  Some of Paleozoic sediments from Alborz and Central Iran subzones from Mid-Iran zone evaluated for distinction of Palaeophycus and Planolites ichnofossils. These sediments include Shale Member of Lalun Formation, Shirgesht Formation, member 5 of Mila Formation and Geiroud Formation.  A diverse ichnofauna  ...  Read More

Cyclostratigraphy of Ab-Deraz Formation in East Kopet-Dagh Basin and Influence of Milankovitch Cycles

L. Fateh Bahari; M.H. Mahmoudi Gharaei; A. Mahboubi; R. Moussavi-Harami

Volume 20, Issue 77 , January 2010, , Pages 57-62


  Ab-Deraz Formation (Turonian to Santonian) is a marly - Carbonates sequence consists of three marl-chalky limestones intervals. This formation widely crops out in Kopet-Dagh Basin in NE of Iran. Chalk and calcareous marl couplets show decimeter to meter scale cycles. Carbonate content of chalky beds ...  Read More

Interpretation of Paragenetic Sequence of Siliciclastic Sediments of Dahu Formation (Late Camberian), in E and SE Zarand, Kerman

R. Moussavi-Harami; A. Mahboubi; A. Kheradmand; H. Zandmoghadam

Volume 18, Issue 70 , February 2009, , Pages 126-139


  For interpretation of paragenetic sequence and post depositional history of siliciclastic sediments of Dahu Formation (Late Camberian), two stratigraphy sections were measured at Dahuieh (type section) and Gazuieh in the NE and E of Zarand, with the thickness of 240 and 227 meters, respectively. The ...  Read More

Lithfacies Analysis and Depositional Model of Lateshur River,South East Tehran

M. Khoddami; A. Mahboubi; R. Moussavi-Harami; S. Feiznia

Volume 16, Issue 63 , March 2007, , Pages 110-123


  The Lateshur Watershed is a part of Central Iranian drainage basin located northeast of the city of Pakdasht in northeastern TehranProvince. This watershed has an elongate form and its surface area is more than 22.2 square kilometer. It is a part of central Alborz zone and geologically is composed of ...  Read More

Environmental Interpretation of Kashafrud Formation (Upper Bajocian- Lower Bathonain) based on Ichnofossils, NE Iran

M. R. Poursoltani; R. Moussavi Harami; Y. Lasemi

Volume 17, Issue 65 , March 2007, , Pages 170-194


        The KopetDaghBasin of northeast Iran formed in the NeotethysOcean after the closure of Paleotethys in the south of Turan plate. A thick sequence of Jurassic to Miocene sediments has been deposited in this basin without any major break. The siliciclastic Kashafrud Formation ...  Read More