The Geology of Egypt Zakaria Hamimi

1. Turin Papyrus Map and Historical Background of Geological Work in Egypt

2. The Egyptian Nubian Shield Within the Frame of the Arabian–Nubian Shield

3. Rock Succession in Egyptian Nubian Shield

4. The Sinai Metamorphic Complexes from Rodinia Rifting to the Gondwana Collision

5. The Infracrustal Rocks in the Egyptian Nubian Shield: An Overview and Synthesis

6. The Ophiolite-Dominated Suprastructure, Eastern Desert, Egypt

7. Ediacaran Post-collisional Volcanosedimentary Successions in Egypt

8. Neoproterozoic Ophiolitic and Arc Metavolcanics of the Egyptian Nubian Shield

9. The Egyptian Granitoids: an up-to-date Synopsis

10. The Ediacaran Post-collisional Dokhan Volcanics

11. Ediacaran Sedimentary Rocks “so-called Hammamat” of the Egyptian Shield

12. The Mantle Section of Neoproterozoic Ophiolites from the Pan-African Belt, Eastern Desert, Egypt: Tectonomagmatic Evolution, Metamorphism, and Mineralization

13. Petrogenetic Evolution of the Neoproterozoic Igneous Rocks of Egypt

14. History of Mineral Exploration and Exploitation of the Egyptian Nubian Shield

15. Active Plate Margin-Associated Base- and Precious-Metal Deposits

16. Convergent-Margin Polymetallic Volcanic-Hosted Massive Sulfide Deposits

17. Banded Iron Formation in the Egyptian Nubian Shield

18. Ophiolite-Associated Cu, Ni, and Cr Deposits

19. The Anatomy of Gold-Bearing Juvenile Neoproterozoic Crust (~870–550 Ma) in the Egyptian Segment of the Nubian Shield

20. Sukari Gold Mine: Opportunities and Challenges

21. Sn-W-Ta-Mo-U-REE Mineralizations Associated with Alkali Granite Magmatism in Egyptian Nubian Shield

22. The Pan-African Nonmetallic Mineral Deposits of Egypt: Genetic and Exploration Constraints

23. Application of Remote Sensing in Detecting Mineralized Zones in the Pan-African Belt of Egypt

24. Application of Magnetic Susceptibility and Its Anisotropy in Deciphering the Tectonic Evolution of the Pan-African Belt of Egypt

25. Geophysical Data for Mapping Structural Features and Hydrothermal Alteration Zones in Baseme