Remains of past sea levels such as tidal notches may provide valuable information for the
investigation of relative sea-level changes (RSL) of eustatic/tectonic origin. In this review, we …

Understanding the distribution of sedimentary facies, their texture and diagenetic alterations
in deep-marine rift systems are critical for improved reservoir quality predictions in the …

As a young (< 5 Myr old) active rift with high resolution spatial and temporal constraints, the
Corinth Rift is a natural laboratory for testing models of rift and fault network development in …

Landscape evolution models that invert topography for rock uplift can improve our
understanding of both tectonic and geomorphic processes when properly constrained with …

Syn‐rift deep‐water muds and mudstones preserve a relatively complete stratigraphic
record of tectonic and climatic events. This paper investigates mud‐dominated deposits and …

Considerable progress has been made in modelling the response of rivers to tectonic
perturbation in order to decode the tectonic signals embedded in river long profiles and …

The Corinth basin (Greece) is a young continental rift that recorded cyclic basin
paleoenvironment variations (ie, marine to lacustrine) caused by glacio-eustatic sea level …

The volume and grain‐size of sediment supplied from catchments fundamentally control
basin stratigraphy. Despite their importance, few studies have constrained sediment budgets …

Understanding early rifting of continental lithosphere requires accurate descriptions of up‐
bended rift margins and footwalls that ought to correlate in space and time with the elastic …

Drainage reversals, an end-member case of drainage reorganization, often occur toward
cliffs. Reversals are commonly identified by the presence of barbed tributaries, with a …