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[HTML][HTML] Orogen styles in the East African Orogen: A review of the Neoproterozoic to Cambrian tectonic evolution
Abstract The East African Orogen, extending from southern Israel, Sinai and Jordan in the
north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …
north to Mozambique and Madagascar in the south, is the world́s largest Neoproterozoic to …
Late Cryogenian–Ediacaran history of the Arabian–Nubian Shield: a review of depositional, plutonic, structural, and tectonic events in the closing stages of the …
During the late Cryogenian–Ediacaran (650–542Ma), the Arabian–Nubian Shield (ANS)
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …
underwent final assembly and accretion to the Saharan Metacraton concurrent with the …
Three successive Proterozoic island arcs in the Northern Arabian–Nubian Shield: Evidence from SIMS U–Pb dating of zircon
Four isolated metamorphic complexes located within post-collisional granitoids occupying
up to 70% of the total area, were distinguished in Sinai (Egypt) and Elat area (southern …
up to 70% of the total area, were distinguished in Sinai (Egypt) and Elat area (southern …
Geochemistry of the Neoproterozoic metasediments of Malhaq and Um Zariq formations, Kid metamorphic complex, Sinai, Egypt: Implications for source-area …
MZ El-Bialy - Lithos, 2013 - Elsevier
Abstract The Um Zariq and Malhaq formations occupy roughly the northern half of the Kid
metamorphic complex of SE Sinai, in the NE part of the Arabian–Nubian Shield. The Um …
metamorphic complex of SE Sinai, in the NE part of the Arabian–Nubian Shield. The Um …
Geochemistry, geochronology, and Sr–Nd isotopes of the Late Neoproterozoic Wadi Kid volcano-sedimentary rocks, Southern Sinai, Egypt: implications for tectonic …
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 …
rocks in the basement of southern Sinai in the northernmost Arabian–Nubian Shield. It is …
Genesis of the gneissic core complexes in the Arabian-Nubian Shield and its tectonic implications: A regional overview
Metamorphic core complexes (MCCs) are a domed structures cored by high grade gneiss
overlain by low grade supracrustal rocks. They are characterized by some common features …
overlain by low grade supracrustal rocks. They are characterized by some common features …
Structural and tectonic framework of Neoproterozoic basement of Egypt: from gneiss domes to transpression belts
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 …
documented, principally through its history of structural events, and to a lesser degree …
Mineral resources in Egypt (I): Metallic ores
Mineral resources in Egypt are diverse. This chapter deals with the metallic ores. The
chapter starts with the iron ores in Egypt and special emphasis is given to the origin of …
chapter starts with the iron ores in Egypt and special emphasis is given to the origin of …
[HTML][HTML] Remote Sensing, Petrological and Geochemical Data for Lithological Map** in Wadi Kid, Southeast Sinai, Egypt
The Wadi Samra–Wadi Kid district in southeastern Sinai, Egypt, has undergone extensive
investigation involving remote sensing analysis, field geology studies, petrography, and …
investigation involving remote sensing analysis, field geology studies, petrography, and …
The Wadi Zaghra metasediments of Sinai, Egypt: new constraints on the late Cryogenian–Ediacaran tectonic evolution of the northernmost Arabian–Nubian Shield
The depositional age of the Wadi Zaghra metasediments (Zaghra Formation) of the Sa'al-
Zaghra metamorphic complex (Sinai) in the Arabian–Nubian Shield (ANS) has been …
Zaghra metamorphic complex (Sinai) in the Arabian–Nubian Shield (ANS) has been …