Rare Metal Distribution and Mineralization Potentiality of Pegmatites in Gabal El Fereyid Granite, South Eastern Desert, Egypt

[1] Abd El Naby H. H.(2003)Radioelement distribution in the proterozoic granites and associated pegmatites of Gabal El Fereyid area, Southeastern Desert, Egypt Appl. Radiation Isotopes 59 289-299

[2] Saleh G. M.(1980)“Geology and litho–stratigraphy of the Arabian Desert orogenic belt of Egypt between lat. 25°35′ and 25°30′,” 1st Appl. Geol Jeddah Bull. 4 127-134

[3] Akaad M. K.(2007)Geochemistry of U–Th–REE bearing minerals, in radioactive pegmatite in Um Swassi–Dara area, north eastern desert, Egypt Jordan Atomic Energy Comm. 1 197-209

[4] Nowier A. M.(1996)Controls on the fractionation of isovalent trace elements in magmatic and aqueous system; evidence from Y/Ho, Zr/Hf and lanthanide tetrad effect Contrib. Mineral. Petrol. 123 323-333

[5] Ali B. A.(1994)The late Precambrian Timna igneous complex, southern Israel: evidence for comagmatic–type sanukitoid monzodiorite and alkali granite magma Lithos 31 103-124

[6] Bau M.(2000)Chemical variations of zircon compared with morphological evolution during magmatic crystallization: an example from the Valle del Cervo Pluton (Western Alps) Eur. J. Mineral. 12 779-794

[7] Beyth M.(1991)Rare–element granitic pegmatites. 1. Anatomy and internal evolution of pegmatite deposits Geosci. Canada 18 49-67

[8] Stern R. J.(2005)The classification of granitic pegmatites revisited Can. Mineral. 43 2005-2026

[9] Altherr R.(1986)“Fractionation trends of the Nb and Ta–bearing oxide minerals in the Greer Lake pegmatitic granite and its pegmatite aureole,” southeastern Manitoba Am. Mineral. 71 501-517

[10] Kröner A.(2012)Granitic pegmatites as reflections of their sources Elements 8 289-294

[1] Abd El Naby H. H.(2003)Radioelement distribution in the proterozoic granites and associated pegmatites of Gabal El Fereyid area, Southeastern Desert, Egypt Appl. Radiation Isotopes 59 289-299

[2] Saleh G. M.(1980)“Geology and litho–stratigraphy of the Arabian Desert orogenic belt of Egypt between lat. 25°35′ and 25°30′,” 1st Appl. Geol Jeddah Bull. 4 127-134

[3] Akaad M. K.(2007)Geochemistry of U–Th–REE bearing minerals, in radioactive pegmatite in Um Swassi–Dara area, north eastern desert, Egypt Jordan Atomic Energy Comm. 1 197-209

[4] Nowier A. M.(1996)Controls on the fractionation of isovalent trace elements in magmatic and aqueous system; evidence from Y/Ho, Zr/Hf and lanthanide tetrad effect Contrib. Mineral. Petrol. 123 323-333

[5] Ali B. A.(1994)The late Precambrian Timna igneous complex, southern Israel: evidence for comagmatic–type sanukitoid monzodiorite and alkali granite magma Lithos 31 103-124

[6] Bau M.(2000)Chemical variations of zircon compared with morphological evolution during magmatic crystallization: an example from the Valle del Cervo Pluton (Western Alps) Eur. J. Mineral. 12 779-794

[7] Beyth M.(1991)Rare–element granitic pegmatites. 1. Anatomy and internal evolution of pegmatite deposits Geosci. Canada 18 49-67

[8] Stern R. J.(2005)The classification of granitic pegmatites revisited Can. Mineral. 43 2005-2026

[9] Altherr R.(1986)“Fractionation trends of the Nb and Ta–bearing oxide minerals in the Greer Lake pegmatitic granite and its pegmatite aureole,” southeastern Manitoba Am. Mineral. 71 501-517

[10] Kröner A.(2012)Granitic pegmatites as reflections of their sources Elements 8 289-294