Abstract The Red Sea formed as a consequence of Cenozoic rifting between the African and
Arabian plates. While continuous oceanic spreading is active in the southern and central …

The formation of oceanic crust in the southern and central Red Sea is generally accepted to
have started at c. 5 Ma. However, the nature of the crust in the northern Red Sea is still …

We determined the basement depths in the fold-and-thrust belt (FTB) and the associated
Aruma and Pabdeh foreland basins of the United Arab Emirates. Additionally, we …

With methods for processing remote sensing data becoming widely available, the ability to
quantify changes in spatial data and to evaluate the distribution of diverse landforms across …

Intra-and trans-continental tectonic lineaments and tectonic structures cutting Africa and
Gondwana have long been identified by many authors. These structures were initially …

Several volcanic buildups have been documented using gravity and magnetic data at
specific locations in the Northern Red Sea (NRS). Most of these volcanoes were never …

Komombo Basin is the only hydrocarbon-producing basin in southern Egypt. However, its
petroleum system is still poorly understood, leaving numerous geological questions …

The petroleum system elements in the Komombo Basin have not yet been fully assessed.
This study aims to evaluate source rocks, reservoirs and seals within the basin by integrating …

Quantitative analysis of tectonic subsidence patterns of 13 wells from the margins of Dahra
and Beda Platforms provides new insights into the development of two major fault blocks in …

Kharit basin is an interior Cretaceous rift basin hosted in a Precambrian basement complex
of the Arabian-Nubian shield. Satellite images and potential geophysical data previously …