The South Um Mongul Cu-Mo-Au prospect in the Eastern Desert of Egypt: from a mid-Cryogenian continental arc to Ediacaran post-collisional appinite-high Ba-Sr …

Y Abd El-Rahman, T Seifert, J Gutzmer, A Said… - Ore Geology …, 2017 - Elsevier
Abstract The South Um Mongul prospect is a Cu-Mo-Au porphyry system. It is covered by
porphyritic dacite and hornblende gabbro. Both units are intruded by monzogranite, which …

The Gulf of Suez rifting: implications from low-temperature thermochronology

S Mansour, N Hasebe, K Abdelrahman… - International Geology …, 2024 - Taylor & Francis
ABSTRACT The Gulf of Suez is a continental rift basin that has been developed during the
Oligocene-Miocene as a northern extension of the Red Sea rift system. The Oligo-Miocene …

Structural and tectonic framework of Neoproterozoic basement of Egypt: from gneiss domes to transpression belts

AR Fowler, Z Hamimi - The geology of Egypt, 2020 - Springer
The Neoproterozoic tectonic evolution of the Egyptian Eastern Desert (EED) basement is
documented, principally through its history of structural events, and to a lesser degree …

Precambrian basement complex of Egypt

MZ El-Bialy - The geology of Egypt, 2020 - Springer
Surface exposure of the Egyptian Precambrian basement complex covers ca. 100 000 km 2.
Outcrops of the basement rocks extend over extensive areas in southern Sinai, the Eastern …

Postcollisional ferani volcanics from north arabian–nubian shield (south Sinai, Egypt): petrogenesis and implication for ediacaran (607–593 Ma) geodynamic …

M Sami, M Azer, AA Abdel-Karim - The Journal of Geology, 2022 - journals.uchicago.edu
Abstract The Ediacaran (607–593 Ma) Ferani volcanic rocks are exposed in South Sinai, at
the extreme northern tip of the Arabian-Nubian Shield (ANS). The studied volcanics …

Lu–Hf and O isotopic compositions on single zircons from the North Eastern Desert of Egypt, Arabian–Nubian Shield: Implications for crustal evolution

KA Ali, BA Zoheir, RJ Stern, A Andresen… - Gondwana …, 2016 - Elsevier
Neoproterozoic juvenile crust is exposed in the Eastern Desert of Egypt, between the Nile
and the Red Sea, forming the basement to Cambrian and younger sedimentary strata in the …

Spatial association of Neoproterozoic continental arc I-type and post-collision A-type granitoids in the Arabian–Nubian Shield: the Wadi Al-Baroud older and younger …

MZ El-Bialy, MM Omar - Journal of African Earth Sciences, 2015 - Elsevier
Abstract The Neoproterozoic basement of Wadi Al-Baroud area located at the northern
Eastern Desert (ED) of Egypt, at the northernmost segment of the Arabian–Nubian Shield …

Risk assessment and rare metals mineralization associated with alteration aspects of Rhyolite flow tuffs, Egypt

MY Hanfi, AEA Gawad, AM Abu-Donia… - Radiation Physics and …, 2024 - Elsevier
Argillic alteration and hematitization are the two extensive alterations that affected Um Safi
rhyolite flow tuffs. Rare metal mineralization including radioactive minerals (thorite …

U–Pb chronology and geochemistry of detrital monazites from major African rivers: constraints on the timing and nature of the Pan-African Orogeny

K Itano, T Iizuka, Q Chang, JI Kimura… - Precambrian Research, 2016 - Elsevier
The African continent consists of several cratons rimmed by orogenic belts, which were
mainly formed by collisions of the cratons during the Gondwana supercontinent assembly …

Post-collisional volcanism with adakitic signatures in the Arabian-Nubian Shield: A case study of calc-alkaline Dokhan volcanics in the Eastern Desert of Egypt

BA Abuamarah, MK Azer, PD Asimow, Q Shi - Lithos, 2021 - Elsevier
A volcano-sedimentary succession, including the Guruf volcanic series, is exposed at Gabal
Um Guruf in the north Eastern Desert of Egypt. A series of intermediate to silicic volcanic …