The Khashir gabbro-tonalite suite in the Eastern Desert of Egypt: A root of a rifted Tonian oceanic arc system in the northwestern tip of the accretionary Arabian-Nubian orogen
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Elsevier BV
Reference81 articles.
1. Cryogenian ophiolite tectonics and metallogeny of the Central Eastern Desert of Egypt;Abd El-Rahman;Int. Geol. Rev.,2012
2. Not all Neoproterozoic iron formations are glaciogenic: Sturtian-aged non-Rapitan exhalative iron formations from the Arabian-Nubian Shield;Abd El-Rahman;Mineral. Deposita,2020
3. Tonian-Cryogenian bimodal volcanism and related sulfide ores in the Arabian-Nubian Shield: an example from the Dendekan prospect in the Eastern Desert of Egypt;Abd El-Rahman;Geochemistry,2023
4. Hf isotopic composition of single zircons from Neoproterozoic arc volcanic and post-collision granites, Eastern Desert of Egypt: Implications for crustal growth and recycling in the Arabian-Nubian Shield;Ali;Precambrian Res.,2013
5. U-Pb zircon geochronology and Hf-Nd isotopic systematics of Wadi Beitan granitoids gneisses, South Eastern Desert;Ali;Gondwana Res.,2015
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