Oppositely dipping thrusts and transpressional imbricate zone in the Central Eastern Desert of Egypt

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, kinematics and geometry. Our study revealed the existence of prevalent dextral and minor sinistral conjugate shear zones. The MBSB is metamorphic belt (greenschist-amphibolite) characterized by at least three post-collisional (740-540 Ma) ductile Neoproterozoic deformation events (D-1, D-2 and D-3) followed by a brittle neotectonic deformation (D-4). DI event produced early top-to-the-northwest thrust displacements due to NW-SE shortening. Dy produced discrete zones of NNW-trending upright folds and culminated in initiation of major NW-trending sinistral shear zones of the Najd Fault System (NFS, at c. 640-540 Ma ago) as well as steeply dipping Sy foliation, and shallowly plunging L-2 lineation. NW-to NNW-trending Fy folds are open to steep and vary in plunge from horizontal to vertical. Dy deformational fabrics are strongly overprinted by D-3 penetrative structures. D-3 is characterized by a penetrative S-3 foliation, steeply SE- to NW-plunging and shallowly NE-plunging stretching lineations (L-3), asymmetric and sheath folds (F-3) consistent with dextral sense of movement exhibited by delta- and sigma-type porphyroclast systems and asymmetric boudinage fabrics. D-2-D-3 represent a non-coaxial progressive event formed in a dextral NE- over NW-sinistral shear zone during a partitioned transpression in response to E-W-directed compression during oblique convergence between East and West Gondwana developed due to closure of the Mozambique Ocean and amalgamation of the Arabian-Nubian Shield in Cryogenian-early Ediacaran time. (C) 2014 Elsevier Ltd. All rights reserved.