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Torabi, Ghodrat (2011) Middle Eocene volcanic shoshonites from western margin of Central-East Iranian Microcontinent (CEIM), a mark of previously subducted CEIM-confining oceanic crust. Petrology, 19 (7) 675-689 doi:10.1134/s0869591111030039

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Reference TypeJournal (article/letter/editorial)
TitleMiddle Eocene volcanic shoshonites from western margin of Central-East Iranian Microcontinent (CEIM), a mark of previously subducted CEIM-confining oceanic crust
JournalPetrology
AuthorsTorabi, GhodratAuthor
Year2011 (December)Volume19
Issue7
PublisherPleiades Publishing Ltd
DOIdoi:10.1134/s0869591111030039Search in ResearchGate
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Mindat Ref. ID506073Long-form Identifiermindat:1:5:506073:7
GUID0
Full ReferenceTorabi, Ghodrat (2011) Middle Eocene volcanic shoshonites from western margin of Central-East Iranian Microcontinent (CEIM), a mark of previously subducted CEIM-confining oceanic crust. Petrology, 19 (7) 675-689 doi:10.1134/s0869591111030039
Plain TextTorabi, Ghodrat (2011) Middle Eocene volcanic shoshonites from western margin of Central-East Iranian Microcontinent (CEIM), a mark of previously subducted CEIM-confining oceanic crust. Petrology, 19 (7) 675-689 doi:10.1134/s0869591111030039
In(2011, December) Petrology Vol. 19 (7) Pleiades Publishing Ltd

See Also

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Torabi, Ghodrat, Hemmati, Omid (2011) Alkaline basalt from the Central Iran, a mark of previously subducted Paleo-Tethys oceanic crust. Petrology, 19 (7) 690-704 doi:10.1134/s0869591111070034
Torabi, Ghodrat (2010) Early Oligocene alkaline lamprophyric dykes from the Jandaq area (Isfahan Province, Central Iran): Evidence of Central-East Iranian microcontinent confining oceanic crust subduction. Island Arc, 19 (2). 277-291 doi:10.1111/j.1440-1738.2009.00705.x
Rajabi, Samineh, Torabi, Ghodrat, Morishita, Tomoaki (2024) Granulitic xenoliths from the Eocene and Oligocene volcanic rocks in NW of Central-East Iranian microcontinent: Evidence from petrology of deep crust. Neues Jahrbuch für Mineralogie - Abhandlungen, 199 (1). doi:10.1127/njma/2024/0424
Paniz Shadman, , Torabi, Ghodrat, Morishita, Tomoaki (2022) Eocene Calc-Alkaline Volcanic Rocks from Central Iran (Southeast of Khur, Isfahan Province); an Evidence of Neotethys Syn-Subduction Magmatism. Petrology, 30 (6) 671-689 doi:10.1134/s0869591122060042
Shirdashtzadeh, Nargess, Torabi, Ghodrat, Schaefer, Bruce (2018) A magmatic record of Neoproterozoic to Paleozoic convergence between Gondwana and Laurasia in the northwest margin of the Central-East Iranian Microcontinent. Journal of Asian Earth Sciences, 166. 35-47 doi:10.1016/j.jseaes.2018.07.008
Ghadirpour, Marzieh; Torabi, Ghodrat; Shirdashtzadeh, Nargess; Meisel, Thomas C.; Morishita, Tomoaki (2025) A post-ophiolitic plutonism record in the Central-East Iranian Microcontinent: Evidence for Pre-Eocene age of Neo-Tethys subduction. Journal of African Earth Sciences, 228. doi:10.1016/j.jafrearsci.2025.105628
Torabi, Ghodrat, Arai, Shoji, Abbasi, Hamideh (2014) Eocene continental dyke swarm from Central Iran (Khur area) Petrology, 22 (6) 617-632 doi:10.1134/s086959111406006x
Khalili, khadijeh, Nosouhian, Narges, Torabi, Ghodrat (2019) Mineral chemistry using for evaluation of the Esmaeilabad granite generation in the Posht-e-Badam area (Central- East Iranian Microcontinent) Iranian Journal of Crystallography and Mineralogy, 27 (2) 307-320 doi:10.29252/ijcm.27.2.307
Torabi, Ghodrat, Arai, Shoji (2013) Back-arc Paleo-Tethys related blueschist from Central Iran, south of Chupanan, Isfahan Province. Petrology, 21 (4) 393-407 doi:10.1134/s0869591113040073
TORABI, GHODRAT (2012) Late Permian post-ophiolitic trondhjemites from Central Iran: a mark of subduction role in growth of Paleozoic continental crust. Island Arc, 21 (3). 215-229 doi:10.1111/j.1440-1738.2012.00817.x
Shirdashtzadeh, Nargess, Torabi, Ghodrat, Morishita, Tomoaki (2020) Evolution of lithospheric mantle in the north of Nain‐Baft oceanic crust (Neo‐Tethyan ophiolite of Ashin, Central Iran). Island Arc, 29 (1). doi:10.1111/iar.12342
 
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