Eustatic sea-level changes of the Cretaceous are reevaluated based on a synthesis of
global stratigraphic data. A new terminology for local/regional or relative sea-level changes …

No consensus currently exists regarding the magnitude of Cretaceous short-term (less than
3 Ma in duration) eustatic sea-level change. The lack of a consensus limits the ability to …

There is an abundance of evidence for short intervals of cold climatic conditions during the
Early Cretaceous. However, the lack of a high-resolution, long-term Early Cretaceous …

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 …

The mid-Cretaceous was marked by emplacement of large igneous provinces (LIPs) that
formed gigantic oceanic plateaus, affecting ecosystems on a global scale, with biota forced …

Several studies have been conducted to reconstruct temperature variations across the
Aptian Stage, particularly during early Aptian Oceanic Anoxic Event (OAE) 1a. There is a …

The origin of moderate magnitude (tens of metres), short-term Cretaceous eustatic cycles
remains enigmatic. The historical view of ubiquitous Cretaceous warmth casts doubt on the …

Middle Eastern carbonate petroleum reservoirs exhibit a range of heterogeneities which
consist of variable combinations of primary stratigraphic and secondary diagenetic and …

During the Albian age, siliciclastic input in the Arabian carbonate-dominated shelf formed
important petroleum system elements. Hence, the Albian Burgan-Kazhdumi succession …

Even though it is well accepted that the Earth's surface topography has been affected by
mantle-convection induced dynamic topography, its magnitude and time-dependence …