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
Mineralization, fluid inclusion and sulfur isotope studies in The Gardane-Shir Pb-Zn deposit ,Ardestan,Isfahan Province

Fatemeh Sabahi; Mohammad Lotfi; Peyman Afzal; nima nezafati

Volume 31, Issue 1 , June 2021, , Pages 177-186


  Gardaneshir carbonate-hosted Pb-Zn deposit on the ground of study area located southwest of Ardestan in Isfahan province. Base on lithostratigraphy,the main structure, besides the small outcrops of Jurassic shales, has been made up of carbonate and detrital rock materials depending on Paleozoic,Triassic ...  Read More

Economic Geology
Vein-type copper mineralization in the Zarandieh area based on mineralogy, geochemistry and fluid inclusions studies, Saveh, Markazi province

seyran yousefi; masoud alipourasl

Volume 28, Issue 111 , May 2019, , Pages 203-214


  The Zarandieh district is situated approximately 42 km northeast Saveh (Markazi province) and in the northwestern part of the Urumieh-Dokhtar magmatic belt. In this area, mineralization is hosted by Eocene andesitic lava and Oligo-Miocene diorite and gabbroic rocks. According to the geochemical evidence, ...  Read More

geology, petrography, mineralization and fluid inclusion studies in the mesgarabad exploration area, southeast of tehran

M Norouzi; M. Lotfi; M. H. Emami; H. Jamali; A. Abedini

Volume 27, Issue 106 , March 2018, , Pages 243-256


  Mesgarabad area is located in ~10 km southeast of Tehran, the Central- Alborz structural zone (CASZ) of Iran. The rock units exposed in the area consist of Eocene volcanics, volcano-sedimentary and sedimentary rocks intruded by post upper Eocene granodiorite to quartz monzo-diorite. These subvolcanic ...  Read More

Fluid inclusion and stable isotope study of the Gazestan magnetite-apatite deposit, Central Iran

S Afzali; N Nezafati; M Ghaderi

Volume 26, Issue 101 , December 2017, , Pages 35-44


  The Gazestan magnetite–apatite deposit is located 78 km east of Bafq, in the Bafq-Poshtebadam subzone of the Central Iran structural zone. The rock units in the area belong to the Rizou series and consist of carbonate rocks, shale, tuff, sandstone and volcanic rocks. Intrusive rocks in the form ...  Read More

The evolution of ore-forming fluids and genesis of Nukeh iron deposit, North Semnan based on evidence from fluid inclusions and S, C, O stable isotopes

S. Esmailnezhad; N. Taghipour; A. A. Hassannezhad

Volume 26, Issue 103 , June 2017, , Pages 309-322


  The Nukeh iron deposit is situated at the north of Semnan and at south of Central Alborz structural zone. Volcano-pyroclastic rocks with Eocene age are the host of this deposit. Iron mineralization occurs as massive, disseminated, vein and breccia types in the Nukeh deposit and magnetite, hematite, pyrite, ...  Read More

Genesis of the Hamyerd iron Deposit, NE Semnan: Using Fluid Inclusion and Stable Isotope (S, C, O) Studies

M Hajibahrami; N Taghipour; G Ghorbani

Volume 25, Issue 97 , December 2016, , Pages 61-70


  The Hamyerd iron deposit is located in the northeast of Semnan in the boundary of the southern Alborz and Central Iran structural zones. A sub-volcanic body of monzonite and monzodiorite composition intruded limestone and pyroclastic rocks (equivalent to the middle Eocene Karaj formation). The iron mineralization ...  Read More

Determination of Physicochemical Properties of Ore-Forming Fluids Using Combined Mineralogy and Fluid Inclusion Microthermometric Studies in the Ravanj Pb-Ba-Ag Deposit, Delijan, Markazi Province

M Nejadhadad; B Taghipour; A.R Zarasvandi; A.R Karimzadeh Somarin; S Salamab Elahi

Volume 25, Issue 97 , December 2016, , Pages 131-140


  Located 20 km north of the Delijan city, the Pb-Ba-Ag ore deposit was mineralized in the lower Cretaceous carbonate host rocks in the Ravanj anticline. Geographically, the Ravanj anticline is part of the Urumieh-Dokhtar magmatic arc in the Zagros orogenic belt. Deposition of the ore took place in the ...  Read More

Recognition of Qahr-Abad fluorite deposit occurrence based on REE data, southeast Saqqez, Kurdistan province

M Barati; A Akbarpour; E Fazel Tale; B Talai; M Moslehi

Volume 25, Issue 100 , September 2016, , Pages 155-164


  The Qahr-abad fluorite deposit is located ~58 km southeast of Saqqez city, Kurdistan province. This deposit is developed as scatter lenses, veins, and veinlets (stockwork structure) within carbonate rocks. Violet, green and colorless fluorites are recognized. Quartz, dolomite, calcite and barite are ...  Read More

Source of polymetal epithermal veins at Nikuyeh district (West of Qazvin) based on mineralogy, alteration and fluid inclusion studies

S Aghajani Marsa; M Emami; M Lotfi; k Gholizadeh; M Ghasemi Siani

Volume 25, Issue 99 , June 2016, , Pages 157-168


  The mineralized veins at Nikuyeh are located south of the Tarom-Hashtjin metallogenic province in Alborz-Azarbayejan belt (West Alborz). Rhyodacite and andesite/andesitic basalt volcanic rocks are hosting the vein mineralization in the Nikuyeh ore district. Hydrothermal alteration in host rocks consists ...  Read More

Geochemistry, petrography and fluid inclusion studies of Baba-Nazar Garnet Index, Takab, West Azarbaijan province

S Alipour; P Shirmohammadi; Y Rahimsouri; H Bagheri

Volume 25, Issue 98 , March 2016, , Pages 349-362


  Baba-Nazar garnet occurrence is located in northwest part of Sanandaj-Sirjan geological zone. Rock units in the area, including hornfels, garnetite and extensively weathered host rocks in contact with granite indicate garnet may have formed by metamorphism of clay-argillite, sandstone and calcareous ...  Read More

The Recognition of Copper Mineralization on the Basis of Fluid Inclusions Studies in Haj Alibay Kandy Area, Sheivar Dagh, Ahar

B Hajalilou; Z Karimzadeh; M Advai

Volume 24, Issue 96 , September 2015, , Pages 167-176


  The properties and situation of copper mineralization in the  Haj Alibay Kandi area determined by quartz vein fluid inclusion and geophysical explorations in this study. The most important rock units include Oligocene intrusive rocks with monzonite and quartzmonzonite compositions. These rocks belong ...  Read More

Using of Rare Earth Elements and Fluid Inclusions in Determination of Fluid Origin producing Panah-Kuh Skarn, NW Taft, Yazd Province

A Zahedi; M Boomeri

Volume 24, Issue 95 , June 2015, , Pages 329-340


  The Panah-Kuh skarn is situated in 50km NW of Taft City in Yazd province. Inrtusion of granodioritic stock into the calcareous-dolomitic rocks of Permian Jamal Formation led to formation of calcic and magnesian skarns. The REE patterns of skarns and its forming garnets show Eu/Eu* and Ce/Ce*ratios increase ...  Read More

Stages and Mineralization Conditions of Dardvey Iron Skarn Based on Mineralogy and Fluid Inclusion Evidences, Sangan Area (Khorasan Razavi)

E. Tale Fazel; B. Mehrabi; A. Khakzad; R. Kianpour

Volume 21, Issue 82 , December 2011, , Pages 139-150


  Sangan iron ore deposit is located in 308 km southeast of Mashhad and eastern structural zone of Iran. Due to the high grade, low P-content and high reserve, Sangan is regarded as one of the major iron ore deposits in Iran. The important anomalies in Sangan consist of east, central and west anomalies ...  Read More