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dc.contributor.authorSami, M.en
dc.contributor.authorAdam, M. M. A.en
dc.contributor.authorLv, X.en
dc.contributor.authorLasheen, E. S. R.en
dc.contributor.authorEne, A.en
dc.contributor.authorZakaly, H. M. H.en
dc.contributor.authorAlarifi, S. S.en
dc.contributor.authorMahdy, N. M.en
dc.contributor.authorAbdel, Rahman, A. R. A.en
dc.contributor.authorSaeed, A.en
dc.contributor.authorFarahat, E. S.en
dc.contributor.authorFathy, D.en
dc.contributor.authorAli, S.en
dc.date.accessioned2024-04-05T16:19:15Z-
dc.date.available2024-04-05T16:19:15Z-
dc.date.issued2023-
dc.identifier.citationSami, M, Adam, MMA, Lv, X, Lasheen, ESR, Ene, A, Zakaly, HMH, Alarifi, SS, Mahdy, NM, Abdel rahman, ARA, Saeed, A, Farahat, ES, Fathy, D & Ali, S 2023, 'Petrogenesis and Tectonic Implications of the Cryogenian I-Type Granodiorites from Gabgaba Terrane (NE Sudan)', Minerals, Том. 13, № 3, стр. 331. https://doi.org/10.3390/min13030331harvard_pure
dc.identifier.citationSami, M., Adam, M. M. A., Lv, X., Lasheen, E. S. R., Ene, A., Zakaly, H. M. H., Alarifi, S. S., Mahdy, N. M., Abdel rahman, A. R. A., Saeed, A., Farahat, E. S., Fathy, D., & Ali, S. (2023). Petrogenesis and Tectonic Implications of the Cryogenian I-Type Granodiorites from Gabgaba Terrane (NE Sudan). Minerals, 13(3), 331. https://doi.org/10.3390/min13030331apa_pure
dc.identifier.issn2075-163X-
dc.identifier.otherFinal2
dc.identifier.otherAll Open Access, Gold3
dc.identifier.otherhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-85152364482&doi=10.3390%2fmin13030331&partnerID=40&md5=04177caa1cd6c754a73aa6de241aa8591
dc.identifier.otherhttps://www.mdpi.com/2075-163X/13/3/331/pdf?version=1677482814pdf
dc.identifier.urihttp://elar.urfu.ru/handle/10995/130382-
dc.description.abstractThe widely distributed granitic intrusions in the Nubian Shield can provide comprehensive data for understanding its crustal evolution. We present new bulk-rock geochemistry and isotopic (zircon U-Pb and Lu-Hf) data from the Haweit granodiorites in the Gabgaba Terrane (NE Sudan). The dated zircons presented a 206Pb/238U Concordia age of 718.5 ± 2.2 Ma, indicating that they crystallized during the Cryogenian. The granodiorites contain both biotite and amphibole as the main mafic constituents. The samples exhibit metaluminous (A/CNK = 0.84–0.94) and calc-alkaline signatures. Their mineralogical composition and remarkable low P2O5, Zr, Ce, and Nb concentrations confirm that they belong to I-type granites. They exhibit subduction-related magma geochemical characters such as enrichment in LILEs and LREEs and depletion in HFSEs and HREEs, with a low (La/Yb)N ratio (3.0–5.9) and apparent negative Nb anomaly. The positive Hf(t) values (+7.34 to +11.21) and young crustal model age (TDMC = 734–985 Ma) indicates a juvenile composition of the granodiorites. The data suggest that the Haweit granodiorites may have formed from partially melting a juvenile low-K mafic source. During subduction, the ascending asthenosphere melts might heat and partially melt the pre-existing lower crust mafic materials to generate the Haweit granodiorites in the middle segment of the Nubian Shield. © 2023 by the authors.en
dc.description.sponsorshipKing Saud University, KSUen
dc.description.sponsorshipThis research was supported by Researchers Supporting Project number (RSP2023R496), King Saud University, Riyadh, Saudi Arabia. The author AE would like to thank “Dunarea de Jos” University of Galati, Romania, INPOLDE infrastructure, for the material and technical support.en
dc.description.sponsorshipThis research was supported by Researchers Supporting Project number (RSP2023R496), King Saud University, Riyadh, Saudi Arabia. The author A.E. would like to thank “Dunarea de Jos” University of Galati, Romania, INPOLDE infrastructure, for the material and technical support. The authors would like to thank the editors and the reviewers for their precious time, detailed and constructive reviews, and additional comments which significantly improved the manuscript.en
dc.format.mimetypeapplication/pdfen
dc.language.isoenen
dc.publisherMDPIen
dc.rightsinfo:eu-repo/semantics/openAccessen
dc.rightscc-byother
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/unpaywall
dc.sourceMinerals2
dc.sourceMineralsen
dc.subjectCRYOGENIANen
dc.subjectGABGABA TERRANEen
dc.subjectI-TYPE GRANITEen
dc.subjectNE SUDANen
dc.subjectPARTIAL MELTINGen
dc.subjectZIRCON U-PB-LU-HF ISOTOPESen
dc.titlePetrogenesis and Tectonic Implications of the Cryogenian I-Type Granodiorites from Gabgaba Terrane (NE Sudan)en
dc.typeArticleen
dc.typeinfo:eu-repo/semantics/articleen
dc.type|info:eu-repo/semantics/publishedVersionen
dc.identifier.doi10.3390/min13030331-
dc.identifier.scopus85152364482-
local.contributor.employeeSami, M., Geology Department, Faculty of Science, Minia University, El-Minia, 61519, Egypten
local.contributor.employeeAdam, M.M.A., Faculty of Earth Resources, China University of Geosciences, Wuhan, 430074, Chinaen
local.contributor.employeeLv, X., Faculty of Earth Resources, China University of Geosciences, Wuhan, 430074, China, Geological Survey, Faculty of Earth Resources, China University of Geosciences, Wuhan, 430074, Chinaen
local.contributor.employeeLasheen, E.S.R., Geology Department, Faculty of Science, Al-Azhar University, Cairo, 11884, Egypten
local.contributor.employeeEne, A., INPOLDE Research Center, Department of Chemistry, Physics and Environment, Faculty of Sciences and Environment, Dunarea de Jos University of Galati, Galati, 800008, Romaniaen
local.contributor.employeeZakaly, H.M.H., Institute of Physics and Technology, Ural Federal University, Yekaterinburg, 620002, Russian Federation, Physics Department, Faculty of Science, Al-Azhar University, Assiut, 71524, Egypten
local.contributor.employeeAlarifi, S.S., Department of Geology and Geophysics, College of Science, King Saud University, P.O. Box 2455, Riyadh, 11451, Saudi Arabiaen
local.contributor.employeeMahdy, N.M., Nuclear Materials Authority, El-Maadi, Cairo, 11381, Egypten
local.contributor.employeeAbdel Rahman, A.R.A., College of Petroleum Geology and Minerals, University of Bahri, Khartoum North, 11116, Sudanen
local.contributor.employeeSaeed, A., College of Petroleum Geology and Minerals, University of Bahri, Khartoum North, 11116, Sudanen
local.contributor.employeeFarahat, E.S., Geology Department, Faculty of Science, Minia University, El-Minia, 61519, Egypten
local.contributor.employeeFathy, D., Geology Department, Faculty of Science, Minia University, El-Minia, 61519, Egypten
local.contributor.employeeAli, S., Geology Department, Faculty of Science, Minia University, El-Minia, 61519, Egypten
local.issue3-
local.volume13-
dc.identifier.wos000959552400001-
local.contributor.departmentGeology Department, Faculty of Science, Minia University, El-Minia, 61519, Egypten
local.contributor.departmentFaculty of Earth Resources, China University of Geosciences, Wuhan, 430074, Chinaen
local.contributor.departmentGeological Survey, Faculty of Earth Resources, China University of Geosciences, Wuhan, 430074, Chinaen
local.contributor.departmentGeology Department, Faculty of Science, Al-Azhar University, Cairo, 11884, Egypten
local.contributor.departmentINPOLDE Research Center, Department of Chemistry, Physics and Environment, Faculty of Sciences and Environment, Dunarea de Jos University of Galati, Galati, 800008, Romaniaen
local.contributor.departmentInstitute of Physics and Technology, Ural Federal University, Yekaterinburg, 620002, Russian Federationen
local.contributor.departmentPhysics Department, Faculty of Science, Al-Azhar University, Assiut, 71524, Egypten
local.contributor.departmentDepartment of Geology and Geophysics, College of Science, King Saud University, P.O. Box 2455, Riyadh, 11451, Saudi Arabiaen
local.contributor.departmentNuclear Materials Authority, El-Maadi, Cairo, 11381, Egypten
local.contributor.departmentCollege of Petroleum Geology and Minerals, University of Bahri, Khartoum North, 11116, Sudanen
local.identifier.pure37494417-
local.description.order331-
local.identifier.eid2-s2.0-85152364482-
local.identifier.wosWOS:000959552400001-
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