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

Clinoforms are ubiquitous depositional surfaces in sedimentary systems. The quintessential
shape, with a flat or gentle topset, slo** foreset, and gentle to flat bottomset, is …

The study of many slope channel systems has led to the development of rules in the form of
observations, measurements, and hypotheses. For example, we hypothesize that high …

Submarine gravity flows are a key process for transporting large volumes of sediment from
the continents to the deep sea. The location, volume, and character of the sediment …

The kinematic evolution of the Patagonian fold-and-thrust belt and cogenetic Magallanes
retroarc foreland basin is reconstructed using new geologic map**, two-dimensional (2-D) …

The processes within deep-sea sediment-routing systems are difficult to directly monitor.
Therefore, we rely on other means to decipher the sequence and relative magnitude of the …

Recently developed data collection techniques allow for improved characterization of
sedimentary outcrops. Here, we outline a workflow that utilizes unmanned aerial vehicles …

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

The˜ 4000 m thick and∼ 20 Myr deep-water sedimentary fill of the Upper Cretaceous
Magallanes Basin was deposited in three major phases, each with contrasting stratigraphic …

We present a general model for channel inception and evolution in the deep sea by
integrating observations from two complementary datasets:(1) high-resolution multibeam …