Transpressional deformation has played a key role in the development of the East African Orogenic Belt and the Arabian-Nubian Shield during the Neoproterozoic. This study examines the folding structures in the Kharit shear zone in the southern Eastern Desert of Egypt. This work aims to investigate the relationship between the development of large-scale folds and the mechanism of transpressional inversion within the Kharit shear zone. The structural analysis reveals the occurrence of extensive folds formed through three generations of folding and their associated fabrics. The F1 folds developed during an early phase of north-south shortening, while the F2 folds, distinguished by their overturned and doubly plunging forms, are associated with dextral transpressional deformation along the Kharit shear zone. The subsequent F3 folds, in contrast, are indicative of sinistral transpressional shearing, implying a transpressional inversion that evolves from pure shear to increasingly intricate patterns of fold interference throughout the shear zone. Regionally, the interference pattern changes from west to east, transitioning from lobate-cuspate shapes to mushroom shapes and then to crescent shapes. The refolding of map-scale northeast-trending folds by northwest- and west-northwest-trending folds leads to the formation of this fold interference structure. Transpressional shear systems rework and reactivate the rocks along opposing kinematic planes. This shear-sense reversal emerged from the oblique convergence of East and West Gondwana, coinciding with the activity of the Najd Fault System between 620 and 540 Ma.
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