The effect of the Najd shear deformation on the Pan-African belt of the central Egyptian Nubian Shield: a synthesis for the post-collision tectonic events

Author:

Hagag Wael,Hamimi ZakariaORCID,Abdelnasser AmrORCID

Funder

United Arab Emirates University

Benha University

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference92 articles.

1. Tectonic–metamorphic evolution ofthe Wadi Hafafit culmination (central Eastern Desert, Egypt). Implication forNeoproterozoic core complex exhumation in NE Africa;Abd El-Naby;Geologica Acta,2008

2. Pan-African strike-slip tectonics of Wadi El-Dabbah area, north Sibaicore complex, Central Eastern Desert, Egypt;Abd El-Wahed;Ann. Egypt. Geol. Surv.,2007

3. The role of the Najd fault system in the tectonic evolution of theHammamat molasse sediments, Eastern Desert, Egypt;Abd El-Wahed;Arab. J. Geosci.,2010

4. Oppositely dipping thrusts and transpressional imbricate zone in theCentral Eastern Desert of Egypt;Abd El-Wahed;J. Afr. Earth Sci.,2014

5. Transpressional imbricate thrust zonescontrolling gold mineralization in the Central Eastern Desert of Egypt;Abd El-Wahed;Ore Geol. Rev.,2016

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