Geochemical and isotopic signatures, and zircon UPb ages of the oldest known intrusive rocks associated with porphyry Cu deposits in the central Urumieh–Dokhtar …

D Raeisi, S Babazadeh, LE Long, M Zhao… - Journal of Geochemical …, 2024 - Elsevier
The Zafarghand pluton, having~ 10 km 2 of outcrop exposure, lies within the central
Urumieh–Dokhtar magmatic arc (UDMA) in Iran, of~ 34 Ma age. Zafarghand plagioclase is …

Middle to Late Miocene K-rich magmatism in Central Iran: Geochemical characterization of the post-collision mantle beneath the Urumieh–Dokhtar magmatic arc

S Babazadeh, T Furman, M Santosh, D Raeisi… - Chemical …, 2024 - Elsevier
High-K magmatism of the central Urumieh–Dokhtar magmatic arc (UDMA) documents the
final stages of Neo-Tethyan Ocean subduction. The temporal and spatial development of …

Arc magmatism associated with continental convergence in the SE segment of the UDMA, Iran: Insights from zircon geochronology and Hf–Sr–Nd–Fe isotopes

S Babazadeh, J Ghalamghash, D Raeisi, M Santosh… - Lithos, 2024 - Elsevier
Magmatic suites provide the keys to evaluate the growth and reworking of continental crust.
Late Cretaceous to Pleistocene convergence in the Urumieh–Dokhtar magmatic arc (UDMA) …

Zircon U–Pb–Hf and whole‐rock Sr–Nd isotopic insights on the Silurian syenite–monzonite shoshonitic magmatism of Central Iran

N Nayebi, D Raeisi, S Babazadeh, XP **a… - Geological …, 2024 - Wiley Online Library
The Palaeozoic magmatic history of Central Iran is related to the subduction of the Proto‐
Tethys Ocean and the amalgamation of Gondwana continental fragments. This study …

Geochemical and Sr–Nd–Hf isotopic evidence for Cenozoic partial melting of mantle beneath Natanz, Central Iran

S Babazadeh, M D'Antonio, D Raeisi, T Furman… - Lithos, 2024 - Elsevier
The products of Cenozoic continental arc magmatism in Iran provide an outstanding natural
laboratory for investigating subduction-related processes. Here we present whole rock …

[HTML][HTML] The spatial–temporal evolution of Neotethyan subduction in central to Southeast Iran: Constraints from geochemistry, zircon U–Pb–Hf, and Sr–Nd–Pb …

S Babazadeh, D Raeisi, M Santosh, T Furman… - Chemical …, 2024 - Elsevier
Igneous rocks in central Iran preserve proof of several episodes of Late Mesozoic–Cenozoic
Neotethyan subduction, and record temporal and spatial variations from subduction to …

Lamprophyre as the source of zircon in the Veneto region, Italy

D Zaccaria, N Vicentini, MG Perna, G Rosatelli… - Minerals, 2021 - mdpi.com
Discrete zircons, up to 9 mm in length, occur in alluvial deposits from the Veneto area. They
are likely derived from the disaggregation of lamprophyric rocks belonging to a regional …

Resende lamprophyres: new petrological and structural interpretations for a regional Upper Cretaceous alkaline mafic dyke swarm

BN Macedo, R Peternel, AC Santos… - Brazilian Journal of …, 2022 - SciELO Brasil
New petrographic, lithogeochemical and structural analyses were performed on the Upper
Cretaceous lamprophyres emplaced in the Proterozoic basement rocks of the Resende …

Post‐collisional alkaline lamprophyre magmatism in northern Iran: Implications from whole‐rock geochemistry and mineral compositions

H Omrani, C Günter, GH Shamanian, M Omrani - Island Arc, 2022 - Wiley Online Library
The Shanderman lamprophyre dykes crop out in the western part of the Alborz Mountains
(Talesh). These rocks are classified as camptonites, composed of primary olivine, Ti‐rich …

Geology of the Tabakoto gold deposit, Kédougou-Kéniéba Inlier, West African Craton, Mali

M Diallo, S Salvi, L Baratoux… - BSGF-Earth …, 2024 - pubs.geoscienceworld.org
The Tabakoto gold deposit is part of the highly endowed west-Malian gold belt, which hosts
several world-class deposits. Located in the Paleoproterozoic Kédougou-Kéniéba Inlier …