Hybrid granite magmatism during orogenic collapse in the Eastern Desert of Egypt: Inferences from whole-rock geochemistry and zircon U–Pb–Hf isotopes

Author:

Zoheir Basem,Zeh Armin,El-Bialy Mohammed,Ragab Azza,Deshesh Fatma,Steele-MacInnis Matthew

Funder

Alexander von Humboldt-Stiftung

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference120 articles.

1. The role of the Najd Fault System in the tectonic evolution of the Hammamat molasse sediments, Eastern Desert, Egypt;Abd El-Wahed;Arabian J. Geosci.,2010

2. Neoproterozoic alkaline magmatism of the Eastern Desert of Egypt: Eamples of Atalla Felsites. 2nd International conference on the Geology of Africa;Abu El-Ela;Assiut University.,2001

3. Lithostratigraphy of the Hammamat-Um Seleimat District, Eastern Desert, Egypt;Akaad;Nature,1969

4. Geometry and texture of quartz veins in Wadi Atalla area, Central Eastern Desert, Egypt;Akawy;J. African Earth Sci.,2007

5. U-Pb zircon and Sr–Nd–Hf isotopic evidence for a juvenile origin of the c 634 Ma El-Shalul Granite, Central Eastern Desert, Egypt;Ali;Geol. Mag.,2012

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