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)
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

https://doi.org/10.22071/gsj.2016.40693

Abstract
  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

Geophysics
Fast Earthquake Relocation Using ANFIS Neuro-Fuzzy Network Trained Based on the Double Difference Method

Hamidreza Samadi; Roohollah Kimiaefar; Alireza Hajian

Volume 32, Issue 3 , September 2022, , Pages 93-102

https://doi.org/10.22071/gsj.2022.296260.1922

Abstract
  One of the most important issues in seismology is to accurately determine the epicenter of earthquake, mainly because the accuracy of dependent studies such as seismic risk analysis, fault mechanism, depends on the accuracy of mentioned parameter. Double difference method is one of the conventional relative ...  Read More

Petrology
Mineral chemistry of Cr-Spinel in the Sargaz-Abshur ultramafic-mafic intrusion, SE of Iran : An implication to tectonic setting of the intrusion

Seyed Ali Akbar Asadi; Habibollah Ghasemi; Mohsen Mobasheri

Volume 32, Issue 4 , December 2022, , Pages 103-118

https://doi.org/10.22071/gsj.2022.317848.1960

Abstract
  Sargaz-Abshur (Sikhoran) ultramafic-mafic complex, which is situated in Esfandagheh area, SE Sanandaj-Sirjan metamorphic- magmatic zone,  intruded into Upper Paleozoic- Triassic metamorphic rocks and covered by Jurassic sedimentary rocks. This complex consists of harzburgite and porphyroclastic ...  Read More

Geotechnical Behavior of Tehran Alluvial Deposits against Possible Seismic Events

F. Rezaie; H. Nazari; S. Rahmanian; A. R. Shahidi

Volume 24, Issue 94 , March 2015, , Pages 35-40

https://doi.org/10.22071/gsj.2015.48703

Abstract
  Due to the fast urban developing and construction of surface and sub-surface structures such as several subway lines, requiring the geotechnical studies on these structures is increasingly emphasized. The metropolitan Tehran, in south of the Central Alborz, lying on the set of Quaternary alluvial deposits ...  Read More

Biostratigraphic Interpretation and Systematics of Some Alveolina Species Assemblages in the Ziarat Formation from Soltanieh Mountains (Western Alborz)

M Hadi; H Mosaddegh; N Abbassi

Volume 24, Issue 95 , June 2015, , Pages 39-44

https://doi.org/10.22071/gsj.2015.42254

Abstract
  Carbonate successionsof the Ziarat Formation with introduce the Baghdareh and Gheynarjehsections in the Soltanieh Mountains(southern Zanjan) are rare locality in the western Alborzzone,which are contains of great abundance oflarge benthic foraminifera (LBF), particularly species of Alveolina. In fact, ...  Read More

Studies of Mineralogy and Rare Earth Elements Geochemistry of Ba-Fe-Mn Ores in Ghareh-bolagh, East of Mahabad, West-Azarbaidjan Province

M Roohafza; S Alipour; A Abedini

Volume 23, Issue 90 , March 2014, , Pages 39-44

https://doi.org/10.22071/gsj.2014.43904

Abstract
  Ghareh-bolagh area is located in 20 Km of east of Mahabad, south of West-Azarbaidjan province. Carbonate rocks of Bayandour formation and dolomites of Soltanieh formation in this area are the host of mineralizations from Barium, iron and manganese. Based upon mineralogical investigations, barite, magnetite, ...  Read More

Neotectonic Analysis of Mosha-North Tehran Fault Zone, Based on Morphotectonic Features, Central Alborz, Northern Iran

N Bagha; M Ghorashi; M Arian; M Pourkermani; A Solgi

Volume 24, Issue 1393 , March 2015, , Pages 41-52

https://doi.org/10.22071/gsj.2015.43329

Abstract
  Structural development, caused by active tectonics leads to deformation of morphology features. The Mosha-North Tehran fault zone, located in south edge of the Central Alborz consists of significant tectonic structures. Hence, study on morphotectonic signs is a proper method for evaluation of relative ...  Read More

The role of geological structures in fractal dimension of fractures and drainages in Southwestern Lenjan-Isfahan

A. S Khalifeh Soltani; S. A Alavi; M. R Ghassemi

Volume 26, Issue 101 , December 2017, , Pages 45-56

https://doi.org/10.22071/gsj.2016.41007

Abstract
  Fractal analysis of drainages and fractures is a useful tool to determine the maturity structure of a region. With the help of fractal geometry, this study investigates the fractal dimension of drainages and fractures in the southwestern part of Lenjan, and examines the role of geological structures ...  Read More

Planktic Foraminiferal Palaeobathymetry of the Santonian-Campanian Boundary in Eastern Kopeh-Dagh Basin, Northeastern Iran

M Shafiee Ardestani; M Vahidinia; A Sadeghi

Volume 24, Issue 94 , March 2015, , Pages 45-64

https://doi.org/10.22071/gsj.2015.42573

Abstract
  In this research, we documented a paleontological study on the basis of planktic foraminifera, in five stratigraphic sections (Type, Padeha village, Shorab, Abderaz village and Qarehso) across the Santonian-Campanian transitional boundary in the eastern Kopeh-Dagh sedimentary basin. In all sections, ...  Read More

The Study of Influence of Bubble Surface Area Flux on Flotation Rate Constant of Coal Particles

B Shahbazi; B Rezai; S.M.J Koleini; M Noaparast

Volume 23, Issue 91 , June 2014, , Pages 45-52

https://doi.org/10.22071/gsj.2014.43763

Abstract
  In this research the effect of bubble surface area flux on flotation rate constant of coal particles was investigated and the results showed that flotation rate constant increased with increasing bubble surface area flux. The obtained Maximum flotation rate constant was 3.30 /min while the particle size ...  Read More

Engineering Geology Studies of Freeway Route Using Analytic Hierarchy Process and GIS (Case Study: Qazvin - Rasht Freeway District Roudbar)

M Kamani; A Uromeihy; M Joorabchi

Volume 24, Issue 95 , June 2015, , Pages 47-56

https://doi.org/10.22071/gsj.2015.42149

Abstract
  Roads are of linear engineering projects passing various rock units and geological conditions, so it is necessary to engage the engineering geological studies along the way. The studies continue until the end of the construction and operation. In the route selection process, large volumes of data and ...  Read More

Tidal Energy Extraction in Chabahar Bay

S Shirinmanesh; V Chegini

Volume 24, Issue 93 , December 2014, , Pages 47-52

https://doi.org/10.22071/gsj.2014.43516

Abstract
  Development of modern energies is one of the most important issues that all countries have focused on and have tried to find a new model in that respect. One of the greatest energy-resources in the world is oceans and tidal currents are one of the specific indicators of oceanic current. The movement ...  Read More

Sequence Stratigraphy of Padeha and Bahram Formations in Baghin Section (West of Kerman) based on Lithofacies and Conodontfacies

Z Khosravi; S.M Hosseini-Nezhad

Volume 23, Issue 92 , September 2014, , Pages 47-55

https://doi.org/10.22071/gsj.2014.43651

Abstract
  The carbonate and terrigenous sedimentary sequence of the Padeha and Bahram formations (late Givetian- late Frasnian) with a total thickness of 126 m have a gradational and conformable contact at Baghin region of W Kerman in Central Iran. The terrigenous facies are mainly consisting of sandstone and ...  Read More

Mechanism of Deformation and the Associated Microstructures in the Basic Mylonitic Rocks, NW Urumieh

K. Mohammadiha; M. Sabzehie; M. Ghahraie pour; J. Radfar

Volume 22, Issue 85 , December 2013, , Pages 47-54

https://doi.org/10.22071/gsj.2012.54020

Abstract
  A large widespread outcrop of granitoid - mylonitic gabbros complexes is observed in northeastern part of Serow, NW Iran. Those rocks were considered as Precambrian gneiss and metamorphic rocks (Haghipour and Aghanabati, 1977), or alternatively, a complex of acidic to basic igneous rocks which have undergone ...  Read More

Petrography, Geochemistry, Mineralogy, Fluid Inclusions and Mineralization Study of Vorezg- Qayen Copper Deposit

V. Alizadeh; M. Momenzadeh; M. H. Emami

Volume 22, Issue 86 , December 2012, , Pages 47-58

https://doi.org/10.22071/gsj.2012.54056

Abstract
  Based on Qayen 1:100000 geological map, the copper mineralization of Vorezg in volcanic rocks is attributed to Paleocene-Lower Eocene. Submarine volcanic rocks of the study area are found in two forms of lava and pyroclastics. Based on field and laboratory investigations, the outcropped rocks in Vorezg ...  Read More

Liquefaction Hazard of Tehran based on Past Studies

F. Askari; H. Garivani

Volume 20, Issue 77 , January 2010, , Pages 47-56

https://doi.org/10.22071/gsj.2010.55306

Abstract
  Tehran is the largest and the most populous city of  Iran that have been recently regarded from the risk management point of view because of possibility of the earthquake damages. An important destructive phenomenon that may happen in Tehran during an earthquake is liquefaction.  In the last ...  Read More

Calculation and Interpretation of Some Morphotectonic Indices Around the Torud Fault, South of Damghan

M. Khademi

Volume 19, Issue 75 , January 2010, , Pages 47-56

https://doi.org/10.22071/gsj.2010.55433

Abstract
  The only geologic evidence of the neotectonic activity of theTorud region is its seismisity which assumed to be related to the Torud seismogenic fault. This fault has been overlain by the Quaternary alluvium in the major part of its length. Therefore, the study of morphotectonical characteristics of ...  Read More

Crustal Structure in the Eastern Part of the Alborz Mountains (Iran) from Converted P wave Phases

N Afsari; F Taghizadeh-Farahmand; M.R Ghassemi

Volume 24, Issue 95 , June 2015, , Pages 49-56

https://doi.org/10.22071/gsj.2015.41849

Abstract
  The AlborzMountains are part of the Alpine-Himalayan orogenic belt, situated to the south of the Caspian Sea and north of the Central Iran. . The region is undergoing extensive crustal deformation and shortening between the north-central Iran and the rigid SouthCaspianBasin crust. In this study, we used ...  Read More

Petrogenesis, Tectonomagmatic Setting and Mineralization Potential of Dehsalm Granitoids, Lut Block, Eastern Iran

R Arjmandzadeh; M.H Karimpour; S.A Mazaheri; J F.Santos; M Medina

Volume 23, Issue 89 , December 2013, , Pages 49-58

https://doi.org/10.22071/gsj.2013.44017

Abstract
  The dehsalm porphyritic granitoids belong to the Lut Block volcanic-plutonic belt in East - Central Iran. The intrusive rocks range in composition from gabbro - diorite to granite and can be classified as high-K calc alkaline to shoshonitic volcanic arc granites. Elevated contents of Mo, Cu, Au, Pb, ...  Read More

Geochemistry and Petrogenesis of the Adakites in the Southern Domains of the Northern Sabzevar Ophiolites; With Emphasis on Sr-Nd-Pb Isotopes Results

E Mohammadi; Gh Ghorbani; H Shafaii Moghadam

Volume 24, Issue 95 , June 2015, , Pages 51-62

https://doi.org/10.22071/gsj.2015.42381

Abstract
  The studied volcanic rocks are situated in NW of the Sabzevar, mainly at southern domains of the Northern Sabzevar ophiolitic belt. Abundant rhyolitic domes (e.g., Sarough, Zard-Kuhi, Kuh-e-Sefid Mehr and Nahr domes) in the southern margin of the Davarzan-Sabzevar ophiolitic belt crosscut the above-mentioned ...  Read More

The Authentication of Paleo High by Geochemical Methods in the Center of Binak Oilfield, South Iran

B Alizadeh; R. Fouladvand

Volume 22, Issue 88 , December 2013, , Pages 51-56

https://doi.org/10.22071/gsj.2013.53640

Abstract
  The main goal of this study is to introduce a paleo high in the central part of Binak oilfield using geochemical parameters. Despite the effect of this phenomena on sedimentation, due to its low amplitude of uplift and lack of unconformity, so far remained unknown in this oilfield. Seismic and well log ...  Read More

Using Biogeochemistry Exploration in Reconnaissance of Copper, Lead and Zinc Mineralization in Masjed_dagi, Julfa (Eastern Azerbaijan)

F. Farjandi; H. Bastani

Volume 22, Issue 87 , December 2013, , Pages 51-64

https://doi.org/10.22071/gsj.2013.53830

Abstract
  The aims of present study are investigation of endemic plants in Masjed-Daghi area introducing hyperaccumulator and indicator plants for gold and copper, and also describe the biogeochemical response pattern over a known mineralized site, namely the "Au- Cu" mineralization at Masjed-Daghi area. Masjed_Daghi ...  Read More

Application of Structural Attributes in Petroleum Exploration and Development of an Interference Belt

A. Arzani; S.A. Alavi; M. Pooladzadeh; A.R. Golalzadeh; Z. Mehdipoor

Volume 19, Issue 74 , February 2010, , Pages 51-56

https://doi.org/10.22071/gsj.2010.57320

Abstract
  The area that will be discussed in this study is located between Zagros and Arabian structural zones in Iran in which full fold 3D seismic data has been acquired and interpreted using sophisticated techniques. This paper covers the role of structural sensitive seismic attributes including first and Second ...  Read More

Study of Mineralizing Fluids Characterization by Use of Fluid Inclusion and Oxygen-Hydrogen Isotopes in Bondar Hanza Porphyry Copper Deposit (Southeast of Kerman)

A Mohebi; A Hezarkhani; M Behzadi; H Mirnejad; H Taghi Zadeh

Volume 24, Issue 96 , September 2015, , Pages 53-64

https://doi.org/10.22071/gsj.2015.41676

Abstract
  Bondar Hanza porphyry copper deposit occurs 150 km southeast of Kerman, in southern part of the Urmia-Dokhtar zone and in Dehaj-Sardoiyeh zone. This ore deposit has formed in diorite to granodiorite rocks. The present paper deals with the study of fluid inclusion on quartz and hornblende samples as well ...  Read More

The study of Permian system in Baghvang section S. Shirgesht area (Central Iran)

M.R Partoazar; B Hamdi; S.A Aghanabati

Volume 26, Issue 102 , March 2017, , Pages 53-62

https://doi.org/10.22071/gsj.2017.44073

Abstract
  Foraminiferal contents of the Permian strata of the Kuh-e Baghvang in central Iran has been investigated. The section is located some 45Km Northwest of Tabas and south of Shirgeshtvillage. The Permian deposits of the Jamal Fm. with a thickness of 270 meters are underlain by the Sardar Fm. disconformably ...  Read More