Clinoforms are inclined and normally basinward-dipping horizons developed over a range
of spatial and temporal scales in both siliciclastic and carbonatic systems. The study of …

Restoration of river deltas involves diverting sediment and water from major channels into
adjoining drowned areas, where the sediment can build new land and provide a platform for …

Turbidity currents, and other types of underwater sediment density flow, are arguably the
most important flow process for moving sediment across our planet. Direct monitoring …

The source-to-sink (S2S) concept is focused on quantification of the various components of
siliciclastic sedimentary systems from initial source sediment production areas, through the …

This cutting-edge summary combines ideas from several sub-disciplines including geology,
geomorphology, oceanography and geochemistry to provide an integrated view of Earth …

The basin of giant Lake Pannon in Central Europe was filled by forward accretion of
sediment packages during the Late Miocene and Early Pliocene. Successive positions of the …

It is well established that sedimentary margins grow by sediments bypassing through shelf-
and slope-incising canyons onto the basin floor and by sediments being deposited …

This special issue dealing with the recent advances on modern and ancient clinoform‐
stratified sedimentary successions arises from a European Geoscience Union (EGU) …

In the Late Miocene–Early Pliocene Lake Pannon, regression went on for about 6Ma.
Sediments arriving from the Alpine–Carpathian source area were partly accumulated on the …

Abstract The Barrow Group was deposited in the Northern Carnarvon Basin from the latest
Tithonian to the Late Valanginian. This moderately deep-water shelf-margin is composed …