The evolution of Pan-African mafic-felsic suite of the Dara area, Northern Eastern Desert, Egypt: Implication for the genesis of Iron Oxide-Copper–Gold (IOCG) mineralization

Author:

Baghdady Noha E.ORCID,El-Sayed Mohammed M.,El-Sundoly Hassan I.,Khalil Khalil I.

Publisher

Springer Science and Business Media LLC

Subject

General Earth and Planetary Sciences,General Environmental Science

Reference85 articles.

1. Abdel Aty M (2009) Geochemical and geochronological studies on the Neoproterozoic granitoids between G. Dara and G. Gharib area, North Eastern Desert. Unpublished PhD, Faculty of Science, Menoufia University, Egypt., p 173

2. Abdel Rahman AM, Doig R (1987) The Rb-Sr geochronological evolution of the Ras Gharib segment of the northern Nubian Shield. J Geol Soc Lond 144:577–586

3. Ahmed HA, Gharib ME (2016) Porphyry Cu mineralization in the eastern desert of Egypt: inference from geochemistry, alteration zones, and ore mineralogy. Arab J Geosci 9(179):1–26

4. Al-Boghdady AA, Bishady AM, Shalaby MH, Bassiouni MI (2003) Copper mineralization of Wadi Dara area, north Eastern Desert, Egypt: fluid inclusions and mineral chemistry evidence. 5th International Conference on the Geology of the Middle East, 643-658

5. Barton MD, Johnson DA (1996) Evaporitic-Source Model for Igneous-Related Fe oxide-(REE-Cu-Au-U) Mineralization. Geology 24:259–262. https://doi.org/10.1130/0091-7613(1996)024<0259:esmfir>2.3.co;2

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