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Geochemical Conditions and Factors Controlling the Distribution of Major, Trace, and Rare Elements in Sul Hamed Granitic Rocks, Southeastern Desert, Egypt

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Заглавие Geochemical Conditions and Factors Controlling the Distribution of Major, Trace, and Rare Elements in Sul Hamed Granitic Rocks, Southeastern Desert, Egypt
 
Автор Abed, N. S.
El, Feky, M. G.
El-Taher, A.
Massoud, E. E. S.
Khattab, M. R.
Alqahtani, M. S.
Yousef, E. S.
Hanfi, M. Y.
 
Тематика GEOCHEMICAL CONDITIONS
GRANITIC ROCKS
RARE AND RAREST ELEMENTS
SUL HAMED
TETRAD EFFECT
 
Описание Egypt is mainly covered by ophiolitic rocks, muscovite, and two mica granites, in addition to different types of acidic and basic dikes. Our field observations indicated that El Sela granites were subjected to alteration types such as silicification, kaolinization, and hematitization, which is associated with uranium mineralization. Petrographic investigations clarified that these rocks were affected by saussiritization, muscovitization, and silicifications as the main alteration types associated with uranium mineralization (uranophane and autunite). We carried out chemical analyses of our samples for major oxides and trace and rare earth elements using ICP-OES and ICP-MS. The studied altered granites had high silica, titanium, and phosphorous as major components, with enhanced amounts of trace elements such as Nb, Ta, Zn, Mo, Pb, and Re, in addition to REE, especially light ones. The average REE content was higher than that of worldwide granites with LREE enrichment. One sample had a strong M-type tetrad effect in the fourth type; other samples had weak W-type in the third type, indicating the effect of hydrothermal alteration processes in the altered granites. This was confirmed by calculating the ratios of most isovalents that deviated from the chondritic ratio in many values. Variation diagrams of U and some trace elements illustrated that U had a weak positive correlation with Y and a strong positive correlation with gold, while it had weak to moderate negative correlation with Hf and Zr/U. In addition, uranium had a weakly defined correlation with the other trace elements, indicating a weak to moderate effect of magmatic processes, while the post-magmatic processes surficial or underground water greatly influenced the redistribution of uranium and other elements. © 2022 by the authors.
Khon Kaen University, KKU, (R.G.P.2/247/43)
Deanship of Scientific Research, King Faisal University, DSR, KFU
The authors extend their appreciation to the Deanship of Scientific Research at King Khalid University (KKU) for funding this research project Number (R.G.P.2/247/43).
 
Дата 2024-04-08T11:06:33Z
2024-04-08T11:06:33Z
2022
 
Тип Article
Journal article (info:eu-repo/semantics/article)
Published version (info:eu-repo/semantics/publishedVersion)
 
Идентификатор Abed, NS, El Feky, MG, El-Taher, A, Massoud, EES, Khattab, MR, Alqahtani, MS, Yousef, ES & Hanfi, MY 2022, 'Geochemical Conditions and Factors Controlling the Distribution of Major, Trace, and Rare Elements in Sul Hamed Granitic Rocks, Southeastern Desert, Egypt', Minerals, Том. 12, № 10, 1245. https://doi.org/10.3390/min12101245
Abed, N. S., El Feky, M. G., El-Taher, A., Massoud, E. E. S., Khattab, M. R., Alqahtani, M. S., Yousef, E. S., & Hanfi, M. Y. (2022). Geochemical Conditions and Factors Controlling the Distribution of Major, Trace, and Rare Elements in Sul Hamed Granitic Rocks, Southeastern Desert, Egypt. Minerals, 12(10), [1245]. https://doi.org/10.3390/min12101245
2075-163X
Final
All Open Access; Gold Open Access
https://www.mdpi.com/2075-163X/12/10/1245/pdf?version=1666315202
https://www.mdpi.com/2075-163X/12/10/1245/pdf?version=1666315202
http://elar.urfu.ru/handle/10995/131314
10.3390/min12101245
85140876671
000873201800001
 
Язык en
 
Права Open access (info:eu-repo/semantics/openAccess)
cc-by
https://creativecommons.org/licenses/by/4.0/
 
Формат application/pdf
 
Издатель MDPI
 
Источник Minerals
Minerals