Notable changes in geochemical and mineralogical characteristics of different phases of episyenitization: insights on the radioactive and shielding of the late phase

dc.authoridEne, Antoaneta/0000-0002-6976-0767
dc.authoridIssa, Shams/0000-0002-9166-7497
dc.authoridTaalab, Sherif A./0000-0003-4643-7243
dc.authoridZAKALY, Hesham M.H./0000-0002-7645-9964
dc.authoridTekin, Huseyin Ozan/0000-0002-0997-3488
dc.authorwosidEne, Antoaneta/C-1386-2011
dc.authorwosidIssa, Shams/M-6825-2017
dc.authorwosidTaalab, Sherif A./HCI-9951-2022
dc.authorwosidZAKALY, Hesham M.H./E-8136-2016
dc.authorwosidTekin, Huseyin Ozan/J-9611-2016
dc.contributor.authorTaalab, Sherif A.
dc.contributor.authorZakaly, Hesham M. H.
dc.contributor.authorIvanov, V.
dc.contributor.authorAlrowaily, Albandari W.
dc.contributor.authorAwad, Hamdy A.
dc.contributor.authorAbed, Neveen S.
dc.contributor.authorIssa, Shams A. M.
dc.date.accessioned2024-05-19T14:40:46Z
dc.date.available2024-05-19T14:40:46Z
dc.date.issued2023
dc.departmentİstinye Üniversitesien_US
dc.description.abstractKab Amiri granites are submitted to post-magmatic hydrothermal solutions through fracture and faults, causing several alteration processes. The most common processes are episyenitization, saussuritization, hematitization, sericitization, kaolinization, albitization, chloritization, silicification, and muscovitization. Kab Amiri granites are vuggy, with the vugs partially to completely refilled with new constituents. The least episyenitized granites have elevated amounts of Fe, P, Zr, Ni, U, Th, Ba, Y, Hf, Nb, and As, which are correlated with their mobilization from biotite, k-feldspar, plagioclase and metamict zircon. These elemental changes are related the partial albitization, muscovitization, desilicification and chloritizatiom, which lead to the mobilization of these elements and forming of specific mineral association in the least altered granites such as autonite, tripiolite, columbite, Zircon and galena. On the second stage, granites were subjected to intense alteration processes by mineralizing fluids, causing wholly muscovitization of biotite and feldspar, albitization of plagioclase, carbonitization and apatitization. Many elements were mobilized from these altered minerals, including Ti, Al, Mn, Mg, Ca, Na, K, Mo, Cu, Pb, Zn, Ag, Co, Sr, V, Cr, Sn, Rb, Ta, Li, Sc, W, S, In, and Tl, leading to definite mineralization as kaslite, monazite, xenotime, polycrase and apatite. The mineralizing fluids in the least and highly episyenitized granites are incorporated in some ore minerals like uranophane, fergusonite, bazzite and garnet. Notably, the presence of elements such as U, Th, and other heavy metals in Kab Amiri granites highlights the potential for these rocks in radiation shielding applications. The unique combination of elements and minerals resulting from the alteration processes can be leveraged for developing new materials or enhancing existing materials used in radiation shielding.en_US
dc.description.sponsorshipPrincess Nourah bint Abdulrahman University, Riyadh, Saudi Arabia [PNURSP2023R378]en_US
dc.description.sponsorshipThe authors express their gratitude to Princess Nourah bint Abdulrahman University Researchers Supporting Project (Grant No. PNURSP2023R378), Princess Nourah bint Abdulrahman University, Riyadh, Saudi Arabia. The work of the author AE and APC was covered by Dunarea de Jos University of Galati, Romania.en_US
dc.identifier.doi10.3389/feart.2023.1241975
dc.identifier.issn2296-6463
dc.identifier.scopus2-s2.0-85177237707en_US
dc.identifier.scopusqualityQ1en_US
dc.identifier.urihttps://doi.org10.3389/feart.2023.1241975
dc.identifier.urihttps://hdl.handle.net/20.500.12713/5014
dc.identifier.volume11en_US
dc.identifier.wosWOS:001104225000001en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.indekslendigikaynakScopusen_US
dc.language.isoenen_US
dc.publisherFrontiers Media Saen_US
dc.relation.ispartofFrontiers In Earth Scienceen_US
dc.relation.publicationcategoryMakale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.snmz20240519_kaen_US
dc.subjectDesilicified Episyeniteen_US
dc.subjectBazzite Mineralen_US
dc.subjectIsovalentsen_US
dc.subjectRadiation Shielding Applicationsen_US
dc.subjectDequartzificationen_US
dc.subjectRare Earth Elementsen_US
dc.subjectGeochemistryen_US
dc.subjectKab Amirien_US
dc.titleNotable changes in geochemical and mineralogical characteristics of different phases of episyenitization: insights on the radioactive and shielding of the late phaseen_US
dc.typeArticleen_US

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