Deforming belts in the Arabian‐Nubian Shield (ANS) are classified into (1) suture‐related
belts, including arc–arc and arc‐continental, and (2) post‐accretionary systems, including N …

Abstract The Arabian-Nubian Shield (ANS), the northern extension of the East African
Orogen (EAO), consists of a number of amalgamated island-arc tectonic terranes, separated …

The tectonic evolution of the Arabian–Nubian Shield (ANS), the northern continuation of the
East African Orogen (EAO), is enigmatic and a matter of controversy. The EAO is observed …

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 …

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 …

The Hammamat molasse sediments of the Eastern Desert of Egypt were deposited in
isolated basins formed during an initial stage of orogen parallel N–S extension (650–580 …

The NE–SW trending Mubarak shear belt in the Central Eastern Desert (CED) of Egypt
records the structural features of a transpression regime. Structural interpretation of satellite …

This paper documents the 40–60 km wide ENE–WSW trending Mubarak–Barramiya shear
belt (MBSB) in the Central Eastern Desert of Egypt by examining its structural styles …

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 …

Field and structural studies supported by remote sensing and thermobarometeric data are
attempted to decipher the deformation and metamorphic histories of Umm Gheig shear belt …