In order to facilitate the search for new play concepts and exploration opportunities, a
sequence stratigraphic synthesis of the Cenomanian–Turonian interval of the Arabian Plate …

ABSTRACT The Cretaceous to Eocene succession in central and south Jordan is
characterised by passive continental margin depositional sequences, which pass upward …

The major states, in which Earth's climate operates, ie, icehouse, greenhouse and hothouse,
are epochs of tens of millions of years. These states set long-term boundary conditions that …

The Sarvak Formation (Albian to Turonian in age) of the Zagros basin is a thick sequence of
shallow-water carbonates. This work focuses on the microfacies and sedimentary …

Three stratigraphic sections (Wadi El Dakhl, Abu Darag and Gabal Ataqa) of mixed
siliciclastic/carbonate rocks mark the Cenomanian–Turonian sequence exposed on the …

This study provides a detailed examination of a condensed Cenomanian-Turonian (CT)
succession of two sections (Dokan Dam and Khalakan) in the Kurdistan Region …

We evaluated the structure of planktonic communities and paleoenvironmental conditions
throughout the Cenomanian–Turonian Oceanic Anoxic Event (OAE2) by studying bulk …

Abstract The Asmari Formation is a thick carbonate succession of the Oligo-Miocene in
Zagros Mountains (southwest Iran). In order to interpret the facies and depositional …

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

Shallow-marine carbonate deposition was widespread across the Arabian Plate during
much of the Late Permian–Mesozoic but was significantly interrupted by a major tectonically …