En
  • دکتری (1395)

    زمین شناسی اقتصادی

    تبریز، تبریز، ایران

  • کارشناسی‌ارشد (1391)

    زمین شناسی اقتصادی

    تربیت مدرس، تهران، ایران

  • کارشناسی (1387)

    زمین شناسی

    ارومیه، ارومیه، ایران

  • کانسارهای روی- سرب رسوبی-بروندمی،
  • ذخایر فلزی همراه با سنگهای آتشفشانی،
  • متالوژنی ذخایر معدنی،
  • مطالعات سیالات درگیر و ژئوشیمی ایزوتوپی،
  • ذخایر فسفات و تبخیری،
  • آزمایشگاه مطالعات سیالات درگیر

تاریخ تولد: 1364 محل تولد: بخش محمدیار شهرستان نقده وضعیت تأهل: متأهل

ارتباط

رزومه

Chemical composition of magnetite and chlorite from the stringer zone of the Nudeh volcanogenic massive sulfide (VMS) deposit, Iran: geological implications

Sajjad Maghfouri, Fardin Mousivand, Ebrahim Rastad, David R Lentz
Journal PapersMineralogy and Petrology , 2021 February 1, {Pages 16-Jan }

Abstract

The southwest Sabzevar basin situated in the Sabzevar zone is considered to be an attractive metallogenic province in Iran that hosts both volcanogenic massive sulfide (VMS) and stratiform manganese deposits. The Nudeh Besshi-type VMS deposit is located in the Lower Late Cretaceous volcano-sedimentary sequence. The ore mineralization in this deposit is hosted in the alkali olivine basalt flow and tuffaceous silty sandstone rocks. The Nudeh VMS deposit consists of 2 million metric tons of Cu-Zn massive sulfide overlying a Cu-Fe-rich stringer. The massive sulfide orebody consists dominantly of pyrite, chalcopyrite, friedrichite, magnetite, and sphalerite, together with minor quartz, chlorite, and sericite. Chloritization, silicification, and

The Eocene Poshteh Ba–Pb–Zn–Cu deposit, Iran: geological, mineral–chemical, fluid inclusion, and S–O isotopic analysis of a Kuroko-type VMS deposit with paleo-hydrothermal vent?…

Fardin Mousivand, Golshan Ghaffari, Sajjad Maghfouri, Valeriy Maslennikov, Sergey A Sadykov
Journal PapersInternational Journal of Earth Sciences , 2021 January 2, {Pages 25-Jan }

Abstract

The Poshteh deposit is the first documented paleo-hydrothermal chimney-bearing volcanogenic massive sulfide (VMS) deposit in Iran. It occurs in the form of well-developed lensoid orebodies within the Eocene volcano-sedimentary sequence, and comprises of laminated, brecciated, banded, massive, and disseminated textures. The stratiform part of this deposit is approximately 500?m long and up to 20?m thick, and consists of massive to semi-massive sulfides and barites, some of which are banded, which are overlain by barite and siliceous exhalites. The stringer zone stratigraphically underlies the stratiform mineralization. Veins within the stringer zone are composed of quartz, barite, pyrite, galena, sphalerite, and chalcopyrite. Th

Sediment hosted stratiform Barite-(Cu-Zn-Pb) deposits in the southwest Mahabad, Iran; implications for geology, ore textural, compositional, and SO isotopes geochemistry

S Sharifiyan, M Hosseinzadeh, S Maghfouri, M Moayyed
Journal Papers , , {Pages }

Abstract

Geology, mineralogy and fluid inclusion studies of the Yamaghan Manto-type Cu (Ag) deposit, southeast Zanjan, NW Iran

Z Jiba, M Ghaderi, S Maghfouri
Journal Papers , , {Pages }

Abstract

Ore-forming processes, O–C isotopes geochemistry, and fluid inclusions in the Darreh-Zanjir fault control MVT-type Zn–Pb deposit: Iran

S Maghfouri, F Choulet
Journal Papers , , {Pages }

Abstract

Evolution of the Garmab-e-Paein native copper-rich volcanogenic massive sulfide deposit from northeast Iran: Insights from sulfur isotope and chlorite chemistry

M Tashi, F Mousivand, H Ghasemi, S Maghfouri, V Maslennikov, JM Peter, ...
Journal Papers , , {Pages }

Abstract

Nature of ore-forming fluids in the Mehdiabad world-class sub-seafloor replacement SEDEX-type Zn-Pb-Ba-(Cu-Ag) deposit, Iran; constraints from geochemistry, fluid inclusions …

S Maghfouri, MR Hosseinzadeh, DR Lentz, HA Tajeddin, M Movahednia, ...
Journal Papers , , {Pages }

Abstract

Geological and geochemical constraints on the Farahabad vent-proximal sub-seafloor replacement SEDEX-type deposit, Southern Yazd basin, Iran

Sajjad Maghfouri, Mohammad Reza Hosseinzadeh, David R Lentz, Flavien Choulet
Journal PapersJournal of Geochemical Exploration , Volume 209 , 2020 February 1, {Pages 106436 }

Abstract

Farahabad is a Lower Cretaceous-age sandy dolomite, sandstone and silty limestone hosted zinc-lead deposit in the southern Yazd basin, Iran. This deposit occurs in the lower part of Taft Formation. The Farahabad deposit is a stratiform and stratabound accumulation of hydrothermal sulfides. The mineralized zone at Farahabad is lens shaped and has a relatively flat top. It also ranges greatly in thickness, from a few meters to >30?m. Three styles of ore facies have been differentiated at the deposit. Feeder zone, bedded ore facies, whereas the bulk of ore is contained within sphalerite and galena breccias that record a prolonged and texturally complex history of ore replacement (massive-replacement ore facies). The shape and size of the miner

The Ab-Bagh Late Jurassic-Early Cretaceous sediment-hosted Zn-Pb deposit, Sanandaj-Sirjan zone of Iran: Ore geology, fluid inclusions and (S–Sr) isotopes

Mehdi Movahednia, Ebrahim Rastad, Abdorrahman Rajabi, Sajjad Maghfouri, Francisco J Gonz?lez, Pura Alfonso, Flavien Choulet, Carles Canet
Journal PapersOre Geology Reviews , 2020 March 20, {Pages 103484 }

Abstract

The Ab-Bagh clastic- and carbonate-hosted stratabound and stratiform Zn-Pb deposit in the Sanandaj-Sirjan zone, in the southeastern corner of the Malayer-Esfahan metallogenic belt of Iran, is typical of several sedimentary–exhalative (SEDEX) deposits in this metallogenic belt. The deposit is hosted in a late Jurassic-early Cretaceous sedimentary sequence. Based on position, There are two Zn-Pb-bearing stratigraphic ore horizons. Ore horizon 1 is hosted by late Jurassic-early Cretaceous black shale and siltstone. The wedge-shaped ore body is located close to a synsedimentary normal fault. Petrographic studies indicates that mineralization comprises three sulfide ore facies: stockwork, bedded and massive ore facies. Ore horizon 2 occurs in

Geological, Isotope geochemical and Fluid inclusion constraints on the Mishu SEDEX-type Barite (Pb-Cu-Zn) system, NW Iran

Mahsa Ghorbani Derakhshi, Mohammad Reza Hosseinzadeh, Mohsen Moayyed, Sajjad Maghfouri
Journal PapersOre Geology Reviews , 2020 March 24, {Pages 103493 }

Abstract

The Late Precambrian sedimentary-volcanic sequence of the Kahar Formation at Mishu mountains, NW Iran, hosts the oldest SEDEX-type barite-(Pb-Cu-Zn) mineralization of Iran. These occurrences include Aralan-Pyrbala, Almas, Shanjan, and Daryan that are hosted by organic material-bearing shales, siltstones, and fine-grained sandstones of the Kahar Formation. Based on the morphology of the mineralization and its textures, the mineralization has formed as strata-bound (stockwork zone and massive ore) and stratiform (bedded ore) ore bodies. The stockwork zone consists of an irregular network of vein-veinlets that cross-cut the sedimentary host rocks. The massive ore contains both massive barite and semi-massive sulfide minerals (galena, chalcopyr

Supergene nonsulfide Zn–Pb mineralization in the Mehdiabad world-class sub-seafloor replacement SEDEX-type deposit, Iran

Sajjad Maghfouri, Mohammad Reza Hosseinzadeh, Flavien Choulet
Journal PapersInternational Journal of Earth Sciences , 2020 August 25, {Pages 25-Jan }

Abstract

The world-class Mehdiabad nonsulfide deposit consists of several accumulations of Zn–Pb–Fe nonsulfide minerals, derived from supergene of a vent-proximal sub-seafloor replacement SEDEX-type deposit hosted in lower Cretaceous clastic–carbonate rocks of the Taft and Abkuh Formations. The main sulfides are galena, sphalerite, pyrite, and minor amounts of chalcopyrite, which have been partially or completely transformed into nonsulfide minerals by supergene processes. Currently, the Zn mineralization in the Abkuh Formation (ore horizon II) is almost fully oxidized: the Mehdiabad deposit which can be assigned to both direct replacement and wall-rock replacement types. The time of the formation of the nonsulfide deposit has not been determi

Temporal–spatial distribution of sediment-hosted stratabound copper deposits in Iran; Implications for future exploration

Sajjad Maghfouri, Ebrahim Rastad, Gregor Borg, Mohammad Reza Hosseinzadeh, Mehdi Movahednia, Amir Mahdavi, Fardin Mousivand
Journal Papers , 2020 October 17, {Pages 103834 }

Abstract

Iran is hosting to numerous sediment-hosted stratabound copper (SSC-type) deposits/occurrences. The major structural zones of Iran that host SSC-type deposits are: (1) the Zagros zone, (2) the Tabas Block, (3) the Central Iranian geological and structural gradual zone (CIGS), (4) the Sabzevar zone, and (5) the Kopeh Dagh zone. The SSC-type deposits formed during discrete time periods and in Iran mostly comprise: (1) the Early Cambrian-Ordovician (with the Dehmadan and Khongah deposits in the Zagros zone), (2) the Permian (with the Ghareh Tapeh deposit in the CIGS), (3) the Upper Jurassic (that include Cu mineralizations in the Garedu Red Bed Formation of the Ravar-Tabas-Eshghabad area (RTEA)), (4) the Upper Jurassic to Lower Cretaceous (wit

Nohkuhi volcanogenic massive sulfide deposit: a sample of Bathurst-type mineralization in northwest of Kerman

Sanajerdi A Pakizeh, F Mousivand, A Rajabi, S Maghfouri
Journal Papers , Volume 29 , Issue 115, 2020 January 1, {Pages 11-122 }

Abstract

The Nohkuhi copper deposit located at 40 Km Northwest of Kerman, occurred in the Central Iran structural zone (Bafq-Posht-e-Badam block), within Late Precambrian-Early Cambrian volcano-sedimentary sequences. Host sequence of mineralization consists of dominantly black shale, sandstone and dacitic lava of Rizu Series. Mineralization occurred as stratabound (vein-veinlets) and stratiform (bedded) in the three copper-and two iron-manganese horizons. The mineralization in the Nohkuhi area involves four ore facieses including stringer, vent complex, bedded, and hydrothermal-exhalative banded iron and manganese-rich sediments. Ore textures are dominantly vein-veinlets, laminated, banded, massive, semi-massive, brecciated, and disseminated. This m

Metallogeny and temporal–spatial distribution of sediment-hosted stratabound copper (SSC-type) deposits in Iran; implications for future exploration

Sajjad Maghfouri, Ebrahim Rastad, Gregor Borg, Mohammad Reza Hosseinzadeh, Mehdi Movahednia, Amir Mahdavi, Fardin Mousivand
Journal Papers , Volume 127 , 2020 December 1, {Pages 103834 }

Abstract

Iran is hosting to numerous sediment-hosted stratabound copper (SSC-type) deposits/occurrences. The major structural zones of Iran that host SSC-type deposits are: (1) the Zagros zone, (2) the Tabas Block, (3) the Central Iranian geological and structural gradual zone (CIGS), (4) the Sabzevar zone, and (5) the Kopeh Dagh zone. The SSC-type deposits formed during discrete time periods and in Iran mostly comprise: (1) the Early Cambrian-Ordovician (with the Dehmadan and Khongah deposits in the Zagros zone), (2) the Permian (with the Ghareh Tapeh deposit in the CIGS), (3) the Upper Jurassic (that include Cu mineralizations in the Garedu Red Bed Formation of the Ravar-Tabas-Eshghabad area (RTEA)), (4) the Upper Jurassic to Lower Cretaceous (wit

Nature of ore-forming fluids in the Mehdiabad world-class sub-seafloor replacement SEDEX-type Zn-Pb-Ba-(Cu-Ag) deposit, Iran; constraints from geochemistry, fluid inclusions?…

Sajjad Maghfouri, Mohammad Reza Hosseinzadeh, David R Lentz, Hossein Ali Tajeddin, Mehdi Movahednia, Akbar Shariefi
Journal PapersJournal of Asian Earth Sciences , 2020 December 17, {Pages 104654 }

Abstract

The Mehdiabad deposit is the largest accumulation of siliciclastic-carbonate hosted zinc in the world, with a total resource of 394 Mt, grading 4.2% Zn, 1.6% Pb, and 36 g/t Ag. In this study, trace element, fluid inclusions studies, and O-C-Sr isotopic analyses were carried out on the host rock and related sulfide ores in the Mehdiabad deposit, aiming to reveal the nature of ore-forming fluids. The average REE contents of the ore samples are higher than those of the host rock samples. The Cd values of sphalerite in the ores range from 0.11 to 0.63 wt.%, which suggested that the Mehdiabad Zn-Pb-Ba-(Cu-Ag) mineralization was formed in a sedimentary-exhalative environment. Investigation of the fluid inclusions reveals relatively moderate tempe

Application of structural data, chemistry of sulfide minerals and fluid inclusion in mineralization type determination of Zn-Pb carbonate hosted Gardaneshir ore deposit in?…

Mohammad Jafar Kupayi, Ebrahim Rastad, Madanipour Saeed, Sajad Maghfouri
Journal PapersJournal of Advanced Applied Geology , Volume 10 , Issue 3, 2020 October 22, {Pages 452-467 }

Abstract

Gardeneh-Shir zinc and lead deposit is located at 38 km southwest of Ardestan in Central Iran. The host rocks of this deposit includes carbonates of Middle Triassic Shotory Formation juxtaposed over Upper Triassic Naiband Formation by thrust faulting. The mineralization in these deposits is in the form of vein-veinlet, breccia and filling of karstic cavities with dolomitization and silicification and mainly controlled by Strike-slip faults with the normal component and normal faults with strike slip component those are cross cutting older generation of thrust faults. The results of fluid inclusion studies of on quartz and dolomite in Gardeneh-Shir deposits Area show a fluid with a salinity of 23.2-18.6% by weight of salt, temperature range

Yazdan Lead-Zinc and Barite deposit, an example of SEDEX-Type deposits in the western Central Iran structural zone

Mohammad Jafar Kupayi, Ebrahim Rastad, Saeed Madanipour, Sajjad Maghfouri
Journal PapersJournal of Geoscience , Volume 30 , Issue 117, 2020 November 21, {Pages 275-286 }

Abstract

Cretaceous sedimentary sequence in the Yazdan area is consisting of four rock units as, from the old to the new, clastic-carbonate (Kc), carbonate (Kl), Shale and marl (Km) sequences, and Sandy limestone and sandstone (Kls). The Kls unit is host of ore mineralization in the study area and formed from four members. Ore mineralization in the Yazdan Deposit has occurred as a stratiform horizon in the sandstone units of the third member. Texture and structures studies, shown three ore facies with elemental zonation in the Yazdan Deposit. These ore facies includes, stringer zone, massive ore facies and the bedded ore facies. This ore facies formed from laminated and layered sulfide and sulfate minerals. Fluid inclusions studies represents 255-13

Metallogeny and temporal–spatial distribution of sediment-hosted stratabound copper (SSC-type) deposits in Iran; implications for future exploration

S Maghfouri, E Rastad, G Borg, MR Hosseinzadeh, M Movahednia, ...
Journal Papers , , {Pages }

Abstract

Application of structural data, chemistry of sulfide minerals and fluid inclusion in mineralization type determination of Zn-Pb carbonate hosted Gardaneshir ore deposit in …

MJ Kupayi, E Rastad, M Saeed, S Maghfouri
Journal Papers , , {Pages }

Abstract

Metallogenesis of Precambrian SEDEX-type Barite-(Pb-Cu-Zn) deposits in the Mishu mountain, NW Iran: Constrains on the geochemistry and tectonic evolution of mineralization

Mahsa Ghorbani Derakhshi, Mohammad Reza Hosseinzadeh, Mohsen Moayyed, Sajjad Maghfouri
Journal PapersOre Geology Reviews , Volume 107 , 2019 April 1, {Pages 310-335 }

Abstract

The Precambrian sedimentary-volcanic sequence of Kahar Formation (KF), located in the Mishu mountain, NW Iran, hosts numerous strata-bound and stratiform Barite-(Pb-Cu-Zn) deposits. These deposits include Daryan, Shanjan, Almas, and Aralan-Pyrbala that are hosted by black shale, siltstone, and fine-grained sandstone of the KF. Available evidence such as clastic rocks, bimodal volcanism (rhyolitic and mafic flows) and geochemistry investigations shows that sedimentary host rocks of KF were formed in an extensional environment in the active continental margin. Based on petrographic studies, three different ore facies have been distinguished: 1) a stockwork (feeder) zone including five types of veins and veinlet’s; 2) a massive ore consistin

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دروس نیمسال جاری

  • دكتري
    زمين شناسي ذخاير معدني ( واحد)
    دانشکده علوم پایه، گروه زمين شناسي اقتصادي
  • دكتري
    زمين شيمي ميانبارهاي سيال ( واحد)

دروس نیمسال قبل

  • دكتري
    ذخاير چينه سان و چينه كران ( واحد)
    دانشکده علوم پایه، گروه زمين شناسي اقتصادي
  • كارشناسي ارشد
    ميانبارهاي سيال ( واحد)
  • كارشناسي ارشد
    ميانبارهاي سيال ( واحد)
  • كارشناسي ارشد
    زمين شناسي اقتصادي منابع معدني ايران ( واحد)
  • كارشناسي ارشد
    زمين شناسي اقتصادي منابع معدني ايران ( واحد)
  • 1399
    ساعدپناه, مهرداد
    زمين شناسي، رخساره هاي كانسنگي، ژئوشيمي و ژنز كانسار مس- روي (طلا) چاه فرسخ جنوبي، جنوب دامغان
  • 1400
    اميني جاده كناري, كاوه
  • 1400
    سپهوند, علي
  • 1398
    پاكيزه سناجردي, امير
    عوامل كنترل كننده تشكيل و تكوين ذخاير چينه سان منگنز (آهن) در توالي آتشفشاني- رسوبي حوضه جنوب غرب قم و بازسازي حوضه تشكيل آنها
    داده ای یافت نشد
  • برنده جایزه تحصیلی بنیاد ملی نخبگان در سال تحصیلی 1396-1395
  • دانشجوی نمونه کشوری زمین شناسی اقتصادی در سال 1395
  • دانشجوی نمونه کشوری زمین شناسی در سال 1394
  • رتبه 13 کشوری در گرایش پترولوژی در کنکور کارشناسی ارشد سال 1388
  • رتبه 6 کشوری در گرایش زمین شناسی اقتصادی در کنکور کارشناسی ارشد سال 1388
  • رتبه 7 کشوری در گرایش ژئوشیمی در کنکور کارشناسی ارشد سال 1388
  • رتبه اول دکتری بین ورودی ها در رشته زمین شناسی اقتصادی دانشگاه تبریز با معدل 19.35 در سال 1392.
  • رتبه اول کارشناسی بین ورودیها در رشته زمین شناسی دانشگاه ارومیه در سال 1387
  • عضو استعدادهای درخشان دانشگاه تبریز از سال 1394 تا 1395

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