Notable changes in geochemical and mineralogical characteristics of different phases of episyenitization: insights on the radioactive and shielding of the late phase
dc.authorid | Ene, Antoaneta/0000-0002-6976-0767 | |
dc.authorid | Issa, Shams/0000-0002-9166-7497 | |
dc.authorid | Taalab, Sherif A./0000-0003-4643-7243 | |
dc.authorid | ZAKALY, Hesham M.H./0000-0002-7645-9964 | |
dc.authorid | Tekin, Huseyin Ozan/0000-0002-0997-3488 | |
dc.authorwosid | Ene, Antoaneta/C-1386-2011 | |
dc.authorwosid | Issa, Shams/M-6825-2017 | |
dc.authorwosid | Taalab, Sherif A./HCI-9951-2022 | |
dc.authorwosid | ZAKALY, Hesham M.H./E-8136-2016 | |
dc.authorwosid | Tekin, Huseyin Ozan/J-9611-2016 | |
dc.contributor.author | Taalab, Sherif A. | |
dc.contributor.author | Zakaly, Hesham M. H. | |
dc.contributor.author | Ivanov, V. | |
dc.contributor.author | Alrowaily, Albandari W. | |
dc.contributor.author | Awad, Hamdy A. | |
dc.contributor.author | Abed, Neveen S. | |
dc.contributor.author | Issa, Shams A. M. | |
dc.date.accessioned | 2024-05-19T14:40:46Z | |
dc.date.available | 2024-05-19T14:40:46Z | |
dc.date.issued | 2023 | |
dc.department | İstinye Üniversitesi | en_US |
dc.description.abstract | Kab 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.sponsorship | Princess Nourah bint Abdulrahman University, Riyadh, Saudi Arabia [PNURSP2023R378] | en_US |
dc.description.sponsorship | The 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.doi | 10.3389/feart.2023.1241975 | |
dc.identifier.issn | 2296-6463 | |
dc.identifier.scopus | 2-s2.0-85177237707 | en_US |
dc.identifier.scopusquality | Q1 | en_US |
dc.identifier.uri | https://doi.org10.3389/feart.2023.1241975 | |
dc.identifier.uri | https://hdl.handle.net/20.500.12713/5014 | |
dc.identifier.volume | 11 | en_US |
dc.identifier.wos | WOS:001104225000001 | en_US |
dc.identifier.wosquality | N/A | en_US |
dc.indekslendigikaynak | Web of Science | en_US |
dc.indekslendigikaynak | Scopus | en_US |
dc.language.iso | en | en_US |
dc.publisher | Frontiers Media Sa | en_US |
dc.relation.ispartof | Frontiers In Earth Science | en_US |
dc.relation.publicationcategory | Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı | en_US |
dc.rights | info:eu-repo/semantics/openAccess | en_US |
dc.snmz | 20240519_ka | en_US |
dc.subject | Desilicified Episyenite | en_US |
dc.subject | Bazzite Mineral | en_US |
dc.subject | Isovalents | en_US |
dc.subject | Radiation Shielding Applications | en_US |
dc.subject | Dequartzification | en_US |
dc.subject | Rare Earth Elements | en_US |
dc.subject | Geochemistry | en_US |
dc.subject | Kab Amiri | en_US |
dc.title | Notable changes in geochemical and mineralogical characteristics of different phases of episyenitization: insights on the radioactive and shielding of the late phase | en_US |
dc.type | Article | en_US |