Deposition of the Upper Cretaceous of central-east Sinai was controlled by a long-term
transgressive phase and several higher order sea-level fluctuations. The paper gives a first …

Environmental and depositional changes across the Late Cenomanian oceanic anoxic
event (OAE2) in the Sinai, Egypt, are examined based on biostratigraphy, mineralogy, δ 13 …

The lithology and the faunal content of late Albian–Turonian inner shelf deposits of present-
day west-central Jordan have been investigated to provide an integrated stratigraphic …

The Cenomanian–Turonian succession exposed in the Wadi Feiran, Sinai, Egypt, is
composed of siliciclastic and carbonate sediments belonging to the Raha (at the base), Abu …

We studied upper Albian to Turonian shallow-marine shelf deposits (Ajlun Group) of west
central Jordan along a NNE-SSW running transect. The carbonate-dominated succession …

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 A thick succession of Late Cretaceous-Early Paleogene age is well exposed in
Gabal Mussaba Salama area. The succession can be subdivided into nine formations …

The changes in macrofauna and microfauna, before, during and after the latest Cenomanian
global Oceanic Anoxic Event (OAE2), from the Eastern Desert of Egypt are documented …

The Areif el Naqa (AeN) is an anticline in the Syrian Arc of eastern Sinai that exposes a
Cretaceous succession composed of mainly marine near-shore (Upper Albian to Coniacian) …

The upper Cenomanian shallow-marine, platform dolostone in northern Israel is topped by a
calcrete crust. It is unconformably overlain by a chaotic unit, 8 m thick, consisting of various …