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)
Economic Geology
The occurrence of boiling process based on mineralogical, textural and fluid inclusion evidences in epithermal deposits: a case study of Chah-Morad deposit, Sistan and Baluchistan, Iran

Leila Amini; Mohammad Maanijou

Volume 33, Issue 4 , December 2023, , Pages 1-20

https://doi.org/10.22071/gsj.2023.378554.2046

Abstract
  One of the common processes that lead to the formation and enrichment of precious metal deposits is boiling. The existence of a spatial relation between fluid boiling and deposition of precious metals is a valuable tool in exploration of epithermal deposits. Therefore, the investigating of the process ...  Read More

Economic Geology
An approach to the origin of the Nineh Lead-Zinc deposit, the north of Mahallat, Markazi Province; insight from mineralogical, fluid inclusion and stable isotope (C-O-S) studies

Shayan Akrami; Mohammad Ali Aliabadi; Mohammad Reza Hazareh; Abbas Askari; Tayebeh Ramezani

Volume 33, Issue 1 , February 2023, , Pages 197-212

https://doi.org/10.22071/gsj.2022.314372.1951

Abstract
  Nineh Pb-Zn deposit is located in the east of the Markazi province, in the Middle to Upper Jurassic rock units of the Malayer-Esfahan  metallogenic belt. Stratified and epigenetic mineralization, in the form of veins, replacement and open spaces filling, including the main minerals of galena, sphalerite ...  Read More

Economic Geology
Deformation, alteration and fluid inclusion studies in the Mirgenaghshineh orogenic gold deposit, Northwest of Sanandaj-Sirjan Zone

Hossein Ali Tajeddin; Ebrahim Rastad; Abdolmajid Yaghoubpour; Mohammad Mohajjel

Volume 32, Issue 4 , December 2022, , Pages 319-336

https://doi.org/10.22071/gsj.2022.232116.1795

Abstract
  The Mirgenaghshineh gold deposit is located 43 km northwest of Saqqez in the northwestern part of the Sanandaj–Sirjan zone. The rocks in the deposit area predominantly consist of Precambrian volcanosedimentary sequences of schist, metasandstone, slate and metaandesite which are intruded by granitoid ...  Read More

Economic Geology
Geology, mineralization, alteration and fluid inclusion studies of the Janja porphyry Cu-Mo deposit, Sistan Suture Zone, SE Iran

Nima Rahimi; Shojaeddin Niroomand; Mohammad Lotfi; Mojtaba Rahimi Shahid

Volume 32, Issue 3 , September 2022, , Pages 13-30

https://doi.org/10.22071/gsj.2022.274408.1889

Abstract
  The Janja Cu-Mo porphyry deposit is located at 70 km south of the Nehbandan, Sistan suture zone, Eastern Iran. The porphyry mineralization in the Janja deposit is temporally and spatially associated with the diorite to quartz diorite and granodiorite granular to porphyry stocks that intruded in the Cretaceous ...  Read More

Economic Geology
Mineralization, Fluid inclusion, and stable isotope studies (O, S) of the Godar Sorkh gold deposit, Muteh, Sanandaj-Sirjan

Monireh Sakhdari; Mehrdad Behzadi; Mohammad Yazdi; Nematollah Rashidnejad-Omran; Morteza Sadeghi Naeini

Volume 32, Issue 3 , September 2022, , Pages 49-60

https://doi.org/10.22071/gsj.2021.291598.1914

Abstract
  The Godar Sorkh area is located in the central part of the Sanandaj-Sirjan zone, 20 km southwest of the Muteh region. Gold mineralization at Godar Sorkh occurs in quartz-sulfide veins that hosted in metasedimentary rocks. Veins of mineralization typically formed along normal faults.  Rock sequences ...  Read More

Economic Geology
Mineralization, geochemistry and fluid inclusion studies of silicic veins in Sarikhanloo area, NW Meshgin Shahr, NW Iran

Hadi Mohammadian; vartan simmonds; kamal Siahcheshm

Volume 32, Issue 1 , March 2022, , Pages 119-136

https://doi.org/10.22071/gsj.2021.253954.1856

Abstract
  The Sarikhanloo area is located within the Qaradagh metallogenic zone in northwest Meshgin Shahr. Igneous rocks cropped out in this area include successions of Paleocene-Eocene pyroclastic rocks (tuff and andesitic-dacitic lavas with intercalations of ignimbrite) and basaltic andesite lava flows. Igneous ...  Read More

Economic Geology
Determination of mineralization conditions based on fluid inclusions data in the Oshvand- Skarn deposit, W of Iran

Mehrdad Movahedi; Mohammad Yazdi; Mehrdad Behzadi

Volume 31, Issue 4 , December 2021, , Pages 111-122

https://doi.org/10.22071/gsj.2021.263309.1871

Abstract
  The Oshvad skarn type deposit was formed during the intrusion of a felsic mass into the Permian and Triassic carbonate rocks and ion exchange occurred between the intrusion mass and these units. In order to determine the properties of the mineralizing fluid in this skarn, several fluid inclusions in ...  Read More

Economic Geology
Petrography, mineralogy, litho-geochemistry and study of fluid inclusions in Gheshlaghe Mil gold-copper ore deposit, northwest of Saveh, Iran

maryam sadat lajouei kalaki; Afshin Akbarpour; Alexandre Tarantola; Shohreh Hassanpour; Behzad Mohammadi; Monireh Poshtkoohi

Volume 31, Issue 2 , September 2021, , Pages 199-212

https://doi.org/10.22071/gsj.2020.209775.1728

Abstract
  The Gheshlaghe mil deposit is located in the Urumieh-Dokhtar magmatic belt. Vein- type mineralization is concordance within the rhyodacitic and rhyolite meta-tuff with Eocene age. Alteration zones of sericite, silica, argillic and iron oxides are observed in the investigated area. Primary sulfide minerals ...  Read More

Economic Geology
Mineralogy, alteration, fluid inclusion and stable isotopes studies of the Sharifabad -Bardeskan copper deposit, NE Iran

Susan Ebrahimi; Alireza Arabamiri; Hadi Ghanbari

Volume 30, Issue 117 , December 2020, , Pages 135-146

https://doi.org/10.22071/gsj.2020.197243.1687

Abstract
  The Sharifabad-Bardeskan copper mineralization is located in northeast of Bardeskan and south section of Sabzevar Zone. Mineralization occurs as vein in the pyroxene andesite, tuff, sandstone and conglomerate of Eocene age, which bearing local sericite - carbonate and silicic alterations and regional ...  Read More

Economic Geology
Mineralogical, Geochemical and Genetic Aspects of Mineralization in Abgareh copper deposit; Typical vein-type Cu deposits

Raziyeh Mahabady; Farajollah Fardoost

Volume 29, Issue 116 , August 2020, , Pages 99-110

https://doi.org/10.22071/gsj.2019.158749.1573

Abstract
  Abgareh copper deposit located in 140 km southwest of shahrood and part of a volcanic-sedimentary Torud-Chah shirin belt that has facies in the northern edge Structural-sedimentary zones of Central Iran. Field and petrographical studies, deposit area, consist of andesite, basaltic andesite and basalt ...  Read More

Economic Geology
Rashidi copper vein deposit, North Khur, Eastern Iran: hydrothermal alteration, mineralization, geochemistry, fluid inclusion and stable isotope investigations

Maryam Javidi Moghaddam; M.H Karimpour; Azadeh Malekzadeh Shafaroudi

Volume 29, Issue 116 , August 2020, , Pages 265-276

https://doi.org/10.22071/gsj.2019.128676.1460

Abstract
  The Rashidi area, which comprises a part of the north Khur in eastern Iran is located at 120 km northwest of Birjand city. Preliminary prospecting in the area using the image processing of ASTER data by Spectral Angle Mapper (SAM) algorithm resulted in the identification of propylitic and argillic alteration ...  Read More

Economic Geology
Thermobarometric Properties of Epigenitic Mineralization Based on Fluid Inclusion Data in Dehkoyeh Salt Dome, Lar, Fars Province

Mohammad Jabarian; mehrdad karimi; Mohammad Lotfi; kamal noori khankahdani

Volume 29, Issue 115 , June 2020, , Pages 289-300

https://doi.org/10.22071/gsj.2018.93957.1210

Abstract
  Dehkooye salt dome is located 30 km northeast of Lar in Fars province, Iran. The salt dome occurred in Zagros folded zone where infracambrian thick evaporate strata (Hormoz series) intruded Cenozoic sedimentary rocks. Core of the dome mainly made up of salt and gypsum and overlain by marl, gypsum, limestone, ...  Read More

Exploration and Mining
Potassic and Phyllic Alteration Zoning Based on the Results of 3D Modeling of Fluid Inclusion Data by Artificial Neural Networks

Maliheh Abbaszadeh; Ardeshir Hezarkhani; Saeed Soltani-Mohammadi

Volume 29, Issue 113 , November 2019, , Pages 115-122

https://doi.org/10.22071/gsj.2018.104239.1301

Abstract
  In recent years, economic geology studies have become very popular method in mineral exploration studies. Modeling fluid inclusion data is one of the common studies in economic geology. In this research artificial neural networks method, as one of the machine learning algorithms, is used for three-dimensional ...  Read More

The study on mineralization of Khankeshi copper deposit by using ineralogy, geochemical and fluid inclusion zata, Markazi province

R. Pourmasoomi; A. R. Jafari rad; M. Lotfi; P. Afzal

Volume 28, Issue 112 , August 2019, , Pages 129-140

https://doi.org/10.22071/gsj.2019.92884

Abstract
  The Khankeshi stratabound copper deposit is located in Markazi province, 80 Km SW of Tehran. The area is covered by a sequence of  E-W trending  lava flows and  pyroclastic of Late Eocene age. The volcanic rocks can be classified as  trachyandesite and andesite.The rocks contain a ...  Read More

Economic Geology
Thermometry and Origin of Mineralizing Fluid at Barika Gold Deposit, East of Sardasht

H Tajeddin; Ebrahim Rastad; Abdolmajid Yaghoubpour; Mohammad Mohajjel; Richard Goldfarb

Volume 28, Issue 111 , May 2019, , Pages 17-28

https://doi.org/10.22071/gsj.2017.77436.1029

Abstract
  Barika gold (and silver)-rich volcanogenic massive sulfide deposit is located 18 km east of Sardasht city in the northwestern of Sanandaj–Sirjan metamorphic Zone. The rocks in the vicinity of the Barika deposit predominantly consist of Cretaceous volcanosedimentary sequences of phyllite, slate, ...  Read More

Investigation on the physical and chemical conditions of the formation of hexagonal colored quartz crystals in Qohrud area based on petrographic evidence and fluid and solid inclusion studies

M. R. Rezapour; V. Simmonds; M. Moazzen; R. Hajialioghli

Volume 28, Issue 111 , May 2019, , Pages 95-104

https://doi.org/10.22071/gsj.2019.88144

Abstract
  The Qohrud granitoid body of Miocene age is located 40 km SW Kashan, ranging in composition from granite through granodiorite to tonalite. Hydrothermal activities following the magma intrusion have brought about formation of various coarse automorphic and colored quartz crystals within the fractures ...  Read More

Economic Geology
Geology and mineralization of Sebandoon gold deposit, North of Bardeskan

Behzad Hamamipour; H. A. Tajeddin; Leila Barahmand

Volume 27, Issue 108 , September 2018, , Pages 155-168

https://doi.org/10.22071/gsj.2017.77437.1030

Abstract
  The Sebandoon gold deposit is located 40 km north of the Bardaskan in the northern part of the Central Iran. The rock units exposed in the area consist of upper Cretaceous volcano-sedimentary sequences of trachyte-trachyandesite, andesibasalt,tuff and carbonaceous shale which intruded by post Eocene ...  Read More

Mineralization, geochemistry, fluid inclusion and stable isotopes (O, S) studies in the Takht Fe-skarn deposit, NE Hamedan

S. N. Haghighi Bardineh; R. Zarei Sahamieh; H. Zamanian; A. Ahmadi Khalaji

Volume 27, Issue 107 , June 2018, , Pages 99-112

https://doi.org/10.22071/gsj.2018.63797

Abstract
  The Takht iron deposit is located 120 km northeast of the Hamedan City in the Urumieh-Dokhtar magmatic belt. The Miocene Takht granodiorite intruded into the Cretaceous carbonates and resulted in Fe-skarn formation. Epigenetic mineralization in the Takht Deposit occurred predominantly as vein and lenticular ...  Read More

Mineralization and geochemical characteristics of ore-forming fluids in Bahr Aseman area, southeast of Kerman magmatic belt

M. R. Hosseini; S. Alirezaei; J. Hassanzadeh

Volume 27, Issue 105 , December 2017, , Pages 143-156

https://doi.org/10.22071/gsj.2017.54183

Abstract
  The Bahr Aseman volcanic-plutonic complex is located to the southeast of the Kerman magmatic belt. Unlike Kerman magmatic belt which formed and evolved during Cenozoic in a dominantly continental arc and post-collision tectonic setting, Bahr Aseman complex formed during Late Cretaceous in an oceanic ...  Read More

Different types of vein- veinlets related to mineralization and fluid inclusion studies in the Sonajil porphyry Cu- Mo deposit, Arasbaran magmatic zone

M.R Hosseinzadeh; S Maghfouri; M Ghorbani; M Moayyed

Volume 26, Issue 101 , December 2017, , Pages 219-230

https://doi.org/10.22071/gsj.2016.41069

Abstract
  The study area is located in Arasbaran metallogenic zone. Rocks of the Sonajil region include Eocene andesite lava, porphyry microdiorite, Incheh granitoid and Ozuzdaghi Plioquaternary volcanic rocks. Porphyry microdiorite is the main host rock of porphyry type Cu- Mo mineralization in the Sonajil deposit. ...  Read More

Economic Geology
Ore mineralization and fluid inclusion and sulfur isotope studies on the Shekarbeig deposit, southwest Mahabad, Sanandaj–Sirjan Zone

A. Baharvandi; M. Lotfi; M. Ghaderi; M. R. Jafari; H. A. Tajeddin

Volume 26, Issue 103 , June 2017, , Pages 201-218

https://doi.org/10.22071/gsj.2017.46614

Abstract
  Shekarbeig barite deposit is located 46 km southwest of Mahabad in northwestern part of the Sanandaj-Sirjan zone. The outcropped rock units in the area are Late Protrozoic metamorphosed volcano-sedimentary rocks, equivalent to Kahar Formation. The main ore mineral occurs as stratiform barite lenses in ...  Read More

Cathodoluminescence, micro thermometry and laser raman spectroscopy studies on hydrothermal quartz in Latala deposit, Central Iran

F Padyar; M Rahgoshay; S Alirezaei; M Pourmoafi; A Tarantola; O Vanderhaeghe; M Caumon

Volume 26, Issue 102 , March 2017, , Pages 39-52

https://doi.org/10.22071/gsj.2017.44072

Abstract
  The Latala base and precious metals deposit is hosted by quartz veins, associated with a porphyry pluton intruded into a Cenozoic volcanic sequence. Euhedral quartz with sulfide mineralization such as pyrite, chalcopyrite, galena and sphalerite, with minor sulfosalts occurs in these veins as open space ...  Read More

SW Sorkh-Kuh copper vein, Lut block, Eastern Iran: mineralization, fluid inclusions and oxygen stable isotopes studies

A Hosseinkhani; M.H Karimpour; A Malekzadeh Shafaroudi

Volume 26, Issue 102 , March 2017, , Pages 165-176

https://doi.org/10.22071/gsj.2017.44144

Abstract
  The SW Sorkh-Kuh area makes part of the Tertiary volcanic-plutonic rocks in the west of the Lut Block, SW of Birjand city. Geology of this area consists of andesitic and basaltic volcanic rocks intruded by hornblende diorite, hornblende microdiorite, hornblende diorite porphyry, hornblende quartz diorite ...  Read More

The Madan Bozorg, volcanic-hosted copper deposit, East Shahroud; an example of Manto type copper deposits in Iran

L Salehi; I Rasa; S Alirezaei; A Kazemi Mehrnia

Volume 25, Issue 98 , March 2016, , Pages 93-104

https://doi.org/10.22071/gsj.2016.41166

Abstract
  The Madan Bozorg deposit is located in the Abbas Abad mining district, about 130 km east of Shahroud. The area is covered by a NE-SW trending belt of intermediate-mafic lava flows and pyroclastic materials, as well as interlayered sedimentary rocks. Eight copper deposits have been identified in the district. ...  Read More

Ore-genests study of The Cu-Au vein-type deposit in The Taron- Granitoid (North Zanjan) based on mineralogical, geochemical and fluid inclusion evidences

H Zamanian; Sh Rahmani; M.R Jannessary; R Zareii Sahamiieh; B Borna

Volume 25, Issue 98 , March 2016, , Pages 255-282

https://doi.org/10.22071/gsj.2016.41228

Abstract
  Lohneh gold and copper deposits lay in the north west of Iran, 100 kilometers north of Zanjan province. Lohneh mining area is a part of the Tarommetallogenic zone in the Alborz-Azerbaijan region. The presence of numerous minerals, slag melting of mining activities (such as cows and exploratory pits, ...  Read More