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200454-Tecto-aluminosilicate and peraluminous glasses have been prepared by conventional and laser heating techniques, respectively, in the CaO-Al

and trace element composition of K-feldspars from pera

Eberz GW, Clarke DB, Chatterjee AK, Giles PS (1991) Chemical and peraluminous leucogranites, South Eastern Desert, Egypt: petrogenesis and

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201434-peraluminous granite hosting or acting as source contents in the south Eastern Desert of Egypt. Debon F, Le Fort P (1983) Chemical-

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Pera-Mekron and Kendeil at Sulamania provience.Population of bears are : New Environmental Horizons of Sustainable Development Tanta University, Egypt

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Gabal Rabadi younger granites located at the South Eastern Desert of Egypt peraluminous, calc-alkaline magma that developed in within-plate tectonic

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Origin and Evolution History of Magmatic Garnet-Bearing

Abu Had Area, South Eastern Desert, Egypt: Inference From Petrology and garnets crystallized from silicic melts and of garnet in peraluminous

on Petrogenesis of Homrit Waggat Rare Metal Granite, Egypt

of Homrit Waggat Rare Metal Granite, Egyptperaluminous granodiorite to hypersolvus metaluminouschemical characterization of the highly evolved

Comparative report on the state of the judiciary in Egypt,

201215-Comparative report on the state of the judiciary in Egypt, Jordan, Lebanonperaluminous granitesstronlium isotopesinherited zirconsoxygen

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the late Precambrian granitoids of Wadi Feiran, Sinai, Egypt

Geochemistry and petrogenetic implications of the late Precambrian granitoids of Wadi Feiran, Sinai, Egypt on ResearchGate, the professional network for

in the Central Eastern Desert of Egypt: Petrological and

201451-in the Central Eastern Desert of Egypt: Petrological and geochemical –74wt.%), and have characteristics of high-K calc-alkaline peralumi

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Neoproterozoic magmatism in NW Sinai, Egypt: and normative corundum, indicating a peraluminousIn accordance with this model, the chemical

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GEOCHEMICAL STUDIES ON SOME GRANITIC MASSES IN THE EASTERN DESERT, EGYPTperaluminous characters and alkaline affinity and belong to post-collision A-

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of the El Sukkari Granite, Central Eastern Desert, Egypt

El Sukkari Granite, Central Eastern Desert, EgyptThe El Sukkari granite is predominantly peraEu-enrichment is due largely to chemical

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Publication » Geology and tectonic evolution of Wadi Beitan area, south Eastern Desert, Egypt. Wadi Beitan area, south Eastern Desert, EgyptThe p

Fereyid – Wadi Rahaba Area, South Eastern Desert, Egypt:

Rahaba Area, South Eastern Desert, Egypt: Geological and Geochemical They exhibit high K-calc alkaline magma and peraluminous characteristics and

of the felsic dyke swarms in southwest Sinai, Egypt.

late Pan-African felsic dyke swarms in southwestern Sinai, Egypt Abdel-Aal.Chemically, these felsic dykes are peraluminous, enriched in K and their

Mayit Area and its Environs, Central Eastern Desert, Egypt

proterozoic calc-alkaline magmatic episode in the Southeastern Desert of EgyptCa (1 wt%) metaluminous to low-Ca (1 wt%) peraluminous granites

GEOLOGY OF AFRICA P-P V- 61 – V-87 (OCT. 2009) ASSIUT-EGYPT

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leucogranites of Wadi Nugeus, Southeastern Desert of Egypt

Geologic and uranium mineralization in peraluminous leucogranites of Wadi Nugeus, Southeastern Desert of Egyptreact-text: 104 The abundance and distribution

from granitic rocks of Ras Barud, Eastern Desert, Egypt

Geochemistry of hornblends from granitic rocks of Ras Barud, Eastern Desert, Egypt on ResearchGate, the professional network for scientists. of hornblend

Tow Mica Granites, Southeastern Desert, Egypt: Geochemistry

Representative major, trace, and REEs elements analyses of peraluminous granites from Abu Rusheid – Eir Arib area, southeastern Desert, Egypt. 1 2 3 4

in the Dubr-Igla Intrusive Complex, Egypt: Inference from

Intrusive Complex, Egypt: Inference from Geochemistry and Sr-Nd Isotopic peraluminous character and are relatively enriched in LIL elements but

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ROCKS AT SALAAT EL BALI – EL REDDAH AREA, NORTH EASTERN DESERT, EGYPTSalaat El Bali, El Reddah and Um Nafie granites originated from a pera

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the Cataclastic rocks of Abu Rusheid area, South Eastern Desert, EgyptThe granites are leucocratic and mostly peraluminous in nature with muscovite

Uranium potentiality of Um Ara area, Southeastern Desert, Egypt

Uranium potentiality of Um Ara area, Southeastern Desert, EgyptThe granites are leucocratic and mostly peraluminous in nature with muscovite

along Wadi El-Atrash Area, North Eastern Desert, Egypt.

Pan-African rocks along Wadi El-Atrash Area, North Eastern Desert, Egypt.Older granites are of I-type, peraluminous and calc-alkaline nature. They

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