We present detailed data of channel morphology for a river undergoing a transient response
to active normal faulting where excellent constraints exist on spatial and temporal variations …

Understanding the manner and degree to which topography in active mountain ranges
reflects deformation of the Earth's surface remains a first order goal of tectonic …

Hydrocarbon reservoirs of fluviatile origin are the product of a number of geological
processes acting on a variety of scales. Reservoir characterization must be approached …

Abstract Changes in long profile, gradient, gradient index, pseudo-hypsometric integral,
valley incision, and sinuosity fractal dimension for rivers in western Oregon were studied to …

Responses of both modern and ancient fluvial depositional systems to growing folds can be
interpreted in terms of interactions among competing controlling variables which can be …

The role of channel width and slope adjustments to differential uplift in rivers within actively
deforming terrains remains contentious. Here high‐resolution topographic surveying of …

Various, but related, models have been proposed to explain the architectural arrangement of
channel stacking patterns in avulsion-dominated alluvial sequences. The early models …

In an extended series of papers by M. Leeder, JRL Allen, JS Bridge, J. Alexander, and
others, the depositional stacking patterns of channel-belt deposits were related to tectonic …

We present new field data from rivers draining across active normal faults that incise across
the same lithology at the fault, have been subjected to similar climatic regimes and tectonic …

Since tectonic subsidence in sedimentary basins provides the potential for long-term facies
preservation into the sedimentary record, analysis of geomorphic elements in modern …