Zircon trace element geochemical constraints on the evolution of the Ediacaran (600–614 Ma) post-collisional Dokhan Volcanics and Younger Granites of SE Sinai …

MZ El-Bialy, KA Ali - Chemical Geology, 2013 - Elsevier
Abstract The post-collisional stage (620–590 Ma) of the Egyptian part of the Arabian–Nubian
Shield was characterized by the eruption and emplacement of the Dokhan Volcanics and …

Geochemistry, geochronology, and Sr–Nd isotopes of the Late Neoproterozoic Wadi Kid volcano-sedimentary rocks, Southern Sinai, Egypt: implications for tectonic …

AKM Moghazi, KA Ali, SA Wilde, Q Zhou, T Andersen… - Lithos, 2012 - Elsevier
The Kid Group is one of the few exposures of Neoproterozoic metavolcano-sedimentary
rocks in the basement of southern Sinai in the northernmost Arabian–Nubian Shield. It is …

A discussion on the tectonic implications of Ediacaran late‐to post‐orogenic A‐type granite in the northeastern Arabian Shield, Saudi Arabia

FA Robinson, B Bonin, V Pease, JL Anderson - Tectonics, 2017 - Wiley Online Library
The transition from late‐orogenic to post‐orogenic magmatism following major orogenic
episodes such as the Neoproterozoic to Cambrian East African Orogen (EAO) is an …

Neoproterozoic tectonic events of Egypt

M ABD EL‐WAHED, Z Hamimi - Acta Geologica Sinica‐English …, 2021 - Wiley Online Library
Abstract The Egyptian Nubian Shield (ENS) represents the northwestern part of the Arabian‐
Nubian Shield and the northern extension of the East African Orogen. The ENS is regarded …

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 …

Development of the Arabian-Nubian Shield along the Marsa Alam-Idfu transect, Central-Eastern Desert, Egypt: geochemical implementation of zircon U-Pb …

S Mansour, N Hasebe, K Abdelrahman… - Geochemical …, 2024 - Springer
The magmatic complex along the Marsa Alam-Idfu transect, Central-Eastern Desert of Egypt,
represents the northern segment of the Arabian–Nubian Shield (ANS), which developed …

Geochemical and isotopic constraints on island arc, synorogenic, post-orogenic and anorogenic granitoids in the Arabian Shield, Saudi Arabia

FA Robinson, JD Foden, AS Collins - Lithos, 2015 - Elsevier
Abstract The Arabian Shield preserves a protracted magmatic record of repeated
amalgamation of juvenile subduction terranes that host granite intrusions ranging in age …

New insights into Cryogenian arc granitoids hosting Th-U mineralized Ediacaran syenogranite dikes, Ra's Abdah area in the northern Egyptian Nubian Shield …

OK Dessouky, W Sun, WS Ibrahim, HH Ali… - Precambrian …, 2021 - Elsevier
During the transition from compressional to extensional-related magmatism, at Ra's Abdah
area of the northern Eastern Desert of Egypt, Ediacaran uraniferous syenogranite dikes with …