Predicting facies distribution in turbidite systems is essential for resource exploration and
identifying geohazards from an economic standpoint. Models that describe facies …

Submarine sediment density flows play a pivotal role in transporting clastic material to the
deep sea. The volume of sediment they transport, which bypasses a specific point or …

The organic-rich, black mudstones that were initially described as the Black Band in
Lincolnshire, Humberside and Yorkshire are known to be a local representation of the …

Foraminifera (single-celled protists) have a long geological record. They are both numerous
and taxonomically diverse in assemblages throughout the Mesozoic and Cenozoic and …

Interpretations of sea-level changes over geological time are mainly based on analyses of
sediments deposited within stable platforms. One of the criteria for recognizing these …

Micropalaeontological and isotopic studies of the upper Cenomanian turbiditic/hemipelagic
sediments from the High-Tatric unit (Central Western Carpathians; Polish part of the Tatra …

This study is a detailed lithofacies analysis of the Wiar and Leszczyny members of the deep-
marine Ropianka Formation (Campanian–Paleocene) exposed in the Hucisko Jawornickie …

Lower Oligocene coccolith limestones, known as Tylawa Limestones, in the Polish part of
the Outer Carpathians have been analyzed using back-scattered electron (BSE) and charge …

Organic-rich black shales intercalated with green radiolarian shales and bentonites, 2.2 m
thick, represent an equivalent of the Bonarelli Level in the Outer Carpathian deep-water …

The long-running debate over the use of a formally defined Middle Cretaceous is discussed
in terms of the distribution of both planktic and benthic foraminifera. The planktic …