The results of a multiproxy study on Mishrif carbonates from the margins of the Central
Mesopotamian Basin of Iraq display a wide range of rock fabrics and diagenetic features, all …

In this study, the Sarvak Formation in the Kuh-e Zana stratigraphic section has been
investigated in terms of Cenomanian biostratigraphy, microfacies analysis, and depositional …

Abstract The Sarvak Formation is a carbonate sequence of Late Albian–Early Turonian age
in Zagros Basin in Iran. In this investigation, the Sarvak Formation at the Pyun Anticline …

Abstract The three Mesozoic divisions (Triassic, Jurassic, and Cretaceous) are represented
in Egypt by sedimentary rocks on the surface and subsurface areas by different percentages …

The analysis of high-resolution stratigraphic data from the Cenomanian–Turonian
successions in three sections from Sinai (northeast Egypt) revealed the mechanisms behind …

Rudist-rich carbonates are common in central Tunisia. They constitute frequent
intercalations in Upper Cretaceous series, particularly within the Cenomanian-Campanian …

Abstract Within the Aptian-Cenomanian formations of Sinai successions in Egypt, lateral and
vertical changes occur in the numerous benthic communities. Microbenthos such as …

Based on newly-collected exhaustive rudist materials from the Turonian Abu Roash
Formation at El-Hassana dome, Durania cornupastoris (Des Moulins) was clearly-identified …

New well‐preserved rudist materials come from the Barremian–Turonian marine formations
in the Yelleg, Minsherah, Maaza, and Raghawi sections in North Sinai, northern Egypt …

The Cretaceous marine successions of North Egypt are rich in rudists and their associations.
The Egyptian rudists are generally recorded from late Barremian to Turonian carbonate …