Structural architecture and tectonic evolution of the Yelleg inverted half graben, northern Sinai, Egypt

- The Yelleg Anticline is one of the northern Sinai Syrian Arc folds.
- The Yelleg folds represent the inversion of a Jurassic half graben.
- The main (SE) bounding fault of the Yelleg half graben has zigzag shape.
- The NW bounding fault of the Yelleg half graben is a system of en echelon faults.
- Inversion in northern Sinai decreases toward the southern Jurassic rift boundary.

The Gebel Yelleg area includes a number of folds belonging to the northern Sinai Syrian Arc structures. Detailed surface structural mapping and subsurface (seismic and borehole) data show that the Gebel Yelleg structures are related to Late Cretaceous-Early Tertiary inversion of a Jurassic asymmetric (or half) graben formed during the opening of Neotethys. The inversion structures include a large (45-km long) asymmetric fold (Yelleg Anticline) with a steep flank overlying the southeastern (main) bounding fault of the inverted half graben as well as some right-stepped en echelon folds overlying the northwestern bounding fault of the half graben. The large inversion anticline is dissected by a large number of long, nearly orthogonal normal faults whereas the en echelon folds are dissected by transverse normal faults and two sets of oblique-slip faults. Inversion of the northern Sinai extensional basins is related to Africa-Eurasia convergence and was probably transpressional with a small component of dextral slip. This study shows that the magnitude of inversion in the northern Sinai fold belt decreases toward the southern boundary of the Jurassic extensional province.