GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT
EL-AFANDY, A., EMBABY, A., EL HARAIREY, M. (2015). GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT. EKB Journal Management System, 4(1), 61-83. doi: 10.21608/nssj.2015.30838
ADEL H. EL-AFANDY; ABD ALRAHMAN EMBABY; MONA A. EL HARAIREY. "GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT". EKB Journal Management System, 4, 1, 2015, 61-83. doi: 10.21608/nssj.2015.30838
EL-AFANDY, A., EMBABY, A., EL HARAIREY, M. (2015). 'GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT', EKB Journal Management System, 4(1), pp. 61-83. doi: 10.21608/nssj.2015.30838
EL-AFANDY, A., EMBABY, A., EL HARAIREY, M. GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT. EKB Journal Management System, 2015; 4(1): 61-83. doi: 10.21608/nssj.2015.30838

GEOLOGY, GEOCHEMISTRY AND RADIOACTIVITY OF GRANITOID ROCKS OF ABU MARW AREA, SOUTH EASTERN DESERT, EGYPT

Nuclear Sciences Scientific Journal
Article 5, Volume 4, Issue 1, 2015, Page 61-83  XML PDF (2.12 MB)
Document Type: Original Article
DOI: 10.21608/nssj.2015.30838
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Authors
ADEL H. EL-AFANDY1; ABD ALRAHMAN EMBABY2; MONA A. EL HARAIREY2
1Nuclear Materials Authority,Cairo, Egypt
2Fac. Sci., Damietta Univ.
Abstract
Abu Marw area is located in the southeastern part of the Eastern Desert, about 150km south east of
Aswan. The Abu Marw area is mainly covered by late Proterozoic igneous and metamorphic rocks. These
basement rocks are unconformably overlain by late Cretaceous Nubian sandstones in the western and
northern parts of the area. Abu Marw granitoid batholiths comprises a co-magmatic calc alkaline I type
peraluminous suite of rocks ranging in composition from tonalite, granodiorite, monzogranite, syenogranite
to alkali feldspar granite. The variations of some major and trace elements with SiO2 suggest a crystal
fractionation model.The tonalite rocks probably had evolved within a continental arc/continental collision
environment, while the granodiorite, monzogranite, syenogranite and alkali feldspar granite rocks had
evolved in within plat environment.
The studied tonalite and granodiorite samples have ΣREE lower than the average REE values (250ppm)
of granitic rocks, while the monzogranite, syenogranite and alkali feldspar granite samples have ΣREE
above the average REE values of granitic rocks. Chondrite-normalized REE patterns of the considered
granites display a gull-wing shape, characterized by large to moderately fractionated patterns and high
LREE relative to the MREE and HREE contents. Furthermore, the studied rocks have a steadily decreasing
Eu/Eu* values from the tonalite to the alkali feldspar granite with simultaneous increase in the ΣREE
contents.
The average contents of U and Th in the different granitic rocks resemble the average contents of some
international equivalent rocks. The average of U contents increases with differentiation. The uranium and
thorium contents in the studied granitic rocks are present in the accessory minerals particularly monazite,
zircon, allanite, sphene, apatite and iron oxides, The radioactive minerals in the pegmatite anomalies are
mainly zircon, uranothorite and fluorite, while in the sheared granites uranophane as secondary minerals
and zircon, allanite, xenotime and uranothorite which are known as U and Th bearing minerals.
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