The lower shoreface provides the connection between the continental shelf and the
shoreline via its onshore transition called the upper shoreface. Lower shorefaces are …

The carbonate factories model, as defined at the beginning of the century, provides a
subdivision of marine carbonate sediment production‐systems based on the style of …

Abstract Lower to Middle Eocene organic-rich deep-water limestones of the∼ 335-m-thick
(1100 ft) Radwany (Thebes-equivalent) Formation represent a source rock and a potential …

Precipitation of methane-derived authigenic carbonates (MDAC) is an integral part of marine
methane production and consumption, but MDAC's relative significance to the global marine …

Abstract Otavi Group is a 1.5–3.5-km-thick epicontinental marine carbonate succession of
Neoproterozoic age, exposed in an 800-km-long Ediacaran− Cambrian fold belt that rims …

The study of carbonate rocks is primarily reliant on microfacies analysis, which is strongly
based on the comparison with modern allochem assemblages. Despite the existence of …

Prediction of carbonate distributions at a global scale through geological time represents a
challenging scientific issue, which is critical for carbonate reservoir studies and the …

Abstract The end Pliensbachian–Toarcian is characterized by several carbon-cycle
perturbations and faunal turnovers (eg, ammonites and foraminifera), which are most likely …

Abstract The Oligocene–Miocene (OM) depositional sequences (Asmari Formation) are
marked by remarkable changes in thickness, lithology, depositional facies characteristics …

A sequence stratigraphic framework predicts that time averaging and hiatus durations will be
long at times of fastest sea‐level rise. This prediction does not necessarily apply to …