The Cenomanian–Santonian successions of Sinai mainly consist of inner-shelf siliciclastics
and carbonates. Five formations (Halal, Raha, Abu Qada, Wata, Matulla) have been …

Summary The Areif El Naqa domal anticline in northeastern Sinai is part of the 'Syrian
Arc'which represents an intraplate orogen that has been formed since the late Cretaceous …

Abstract The Cretaceous/Paleogene (K/Pg) boundary in Jordan is marked by a major
depositional hiatus that differs in magnitude from place to place due to variable structural …

Abstract The Cenomanian–Turonian carbonate ramp in the Adıyaman Region of SE Turkey
(Northern Arabian Platform) records an abrupt shift from benthic carbonate deposits to …

Integration of the calcareous nannofossil and planktonic foraminiferal biostratigraphies has
been performed for the Upper Maastrichtian–Palaeocene successions at Gebel Umm …

The Maastrichtian-Lower Eocene sediments on both sides of the northern Gulf of Suez can
be subdivided into eight formal formations (including one group) and one informal formation …

In the Thamad area, east central Sinai, two stratigraphic sections are measured and
sampled; Gebel El Mishiti and G. El Keeh, in order to determine the nannofossil …

The variations in assemblages of calcareous nannofossils are tracked in the Dakhla and
Tarawan Formations exposed at Gebel Nezzazat (central Sinai, Egypt). Five calcareous …

The uppermost Maastrichtian-lower Eocene succession exposed at three sections located
on the western flan of Esh El-Mellaha range, north Eastern Desert at Wadi Dib, Wadi Abu …

Quantitative study of the ostracode assemblages from the Palaeocene to Early Eocene
succession exposed along the area of east-central Sinai extending from the Egma Plateau …