Drainage networks in continental rifts are generally reported as dynamic features that
produce transitions between endorheic and exorheic conditions. While this is of major …

The occurrence of endorheic basins on the Tibetan Plateau, both in its Pleistocene history
and (fewer in number) at the present day, has been attributed to the 'basin-and …

This paper explores an inverse approach to the problem of characterizing sediment
sources'(“source” samples) age distributions based on samples from a particular depocenter …

Erosion and sedimentation constantly rework topography created by tectonics but also
modulate stresses in the underlying crust by redistributing surficial loads. Decades of …

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 …

Located in the easternmost portion of the Central Apennines, the Mt. Morrone normal fault
system is one of the highest seismic hazards in Italy. Previous geological and …

The top-down drainage basin integration and drainage network evolutionary processes of
lake overflow and aggradational spillover (or aggradational piracy), collectively referred to …

The generation and evolution of continental topography are fundamental geologic and
geomorphic concerns. In particular, the history of landscape development might contain …

Abstract The Colorado River in the southwestern US provides an excellent natural
laboratory for studying the origins of a continent-scale river system, because deposits that …

We use tectonic subsidence patterns from wells and stratigraphic sections to describe the
mid-Miocene to present tectonic subsidence history of the Rio Grande rift. Tectonic …