دکتر سیدمحسن طباطبائی منش

The demand for critical minerals is increasing swiftly as they are essential components for clean energy technologies. Nowadays, lithium (Li) is considered critical due to its wider use in various battery chemistries and the rapid growth of the electric vehicle industry. Pegmatites are considered one of the main sources of lithium worldwide. The pegmatite belt in Afghanistan, known for its enormous resources of critical metals, has recently emerged as an important region for lithium exploration. Multispectral remote sensing imagery is the only technique with large spatial coverage to map lithium-bearing pegmatites on a regional scale. In this study, ASTER and Sentinel 2MSI multispectral remote sensing imagery was used to map lithium-bearing pegmatites in the Tagablor pegmatite field in central Afghanistan. Various spectral mapping methods such as False Color Composite (FCC), Band Ratio (BR) and Spectral Angle Mapper (SAM) as well as supervised classification algorithms, i.e. Support Vector Machine (SVM), Minimum Distance (MD) and Maximum Likelihood (ML), were used to discriminate between altered minerals and lithologies as well as to identify areas with high potential for lithium-bearing pegmatites. Of the classification algorithms tested, SVM showed the highest efficiency in separating pegmatite bodies from their host rocks when applied to Sentinel 2 MSI data. The current study identified six promising pegmatite zones in the Tagablor pegmatite field, five of which were newly discovered and proposed for a comprehensive field campaign. In this study, an overall accuracy of 89 % was achieved in the detection of pegmatites and their surrounding formations, highlighting the potential of multispectral remote sensing for lithium exploration at a regional scale in arid and semi-arid regions. Further geochronological, geochemical and mineralogical investigations are recommended to better understand the age and mineralization potential of these pegmatites in the Tagablor pegmatite field, central Afghanistan. This study highlights the significant potential of multispectral remote sensing in mapping potential zones of critical minerals to enhance the sustainable utilization of minerals for green energy technologies in the future. © 2025 Elsevier B.V.

Subduction-related magmatism (SRM) and its effect on magma fertility: Oligocene–Miocene plutonism evolution in the centre of Urumieh–Dokhtar magmatic arc, Iran

( Article . )

Moghadam, I.R., Tabatabaei manesh, S.M., Shirdashtzadeh, N., Meisel, T.C.

Journal of the Geological Society (2041479X)182(5)

2023

Paleozoic Tensional Intraplate Magmatism and Mantle Evolution in Central Iran Zone: Geochemistry, Nd-Sr Isotope Data of Lamprophyres

( Article . )

Veysi, S., Tabatabaei manesh, S.M., Shirdashtzadeh, N., Santos j.f., J.F.

Petrology (15562085)31(4)pp. 459-474

2022

Golpayegan Metamorphic Complex (Sanandaj–Sirjan Zone, Iran) as Evidence for Cadomian Back-Arc Magmatism: Structure, Geochemistry and Isotopic Data

( Article . )

Ahmadi-bonakdar s., S., Tabatabaei manesh, S.M., Nadimi, A., Mirlohi a., A., Santos j.f., J.F., Parfenova o.v.,

Geotectonics (15561976)56(6)pp. 791-809

Abstract: The Golpayegan metamorphic complex is located in the Sanandaj-Sirjan Zone, Iran. This complex consists of various metamorphic rocks including schists, marbles, slates, gneisses, and amphibolites, most of them have Neoproterozoic age. The presence of structures such as sigma fabrics, boudinage, folded boudinage and interfering fold patterns indicates the occurrence of more than two deformation phases in the Golpayegan metamorphic complex. The measurement of strain intensity in the folds indicated deep immersion of structures and old Precambrian settings that had been influenced by orogenic events in the Neoproterozoic. These deformed rocks were exposed during extensional movements and, subsequently, sheared. The results based on field works shown geochemical relations and initial εNd(600 Ma) values of amphibolites in three sampling points located in Golpayegan region manifested that the protolith of the first (a') and second (b') sampling points had mantle origin (ortho-amphibolite), whilst protolith of the third (c') sampling point had sedimentary origin (para-amphibolite). Geochemically, the Golpayegan ortho-amphibolites showed sub-alkaline basalt-basaltic andesite compositions of tholeiitic affinity. The negative anomalies of Nb and Ti relative to Pb, La, and Ce in the primitive mantle-normalized spider-diagram and εNd(600 Ma) values revealed the subduction environment for ortho-amphibolites. The ortho-amphibolites exhibited the intermediate chemistry between the normal mid-ocean ridge basalt and island-arc tholeiitic basalt. Enrichment in large ion lithophile elements (LILE), light rare earth elements (LREE), and relative depletion in high field strength elements (HFSE) suggest the back-arc basin setting for the Golpayegan ortho-amphibolites. The primitive magma of the ortho-amphibolites was produced by 8–20% melting of spinel lherzolite. According to the Neoproterozoic age of the Golpayegan ortho-amphibolites and their relationship with the Golpayegan granitic gneiss (596‒578 Ma), it shows that they can be related to the Cadomian back-arc basin in the north of Peri-Gondwana at the Neoproterozoic. The high values of 87Sr/86Sr (0.708450‒0.714986) interpreted as result of seawater hydrothermal alteration. © 2022, Pleiades Publishing, Inc.