The recognition of terminal fluvial systems, otherwise termed 'terminal fans' or 'distributary
fluvial fan systems', preserved in the ancient rock record is based primarily on the …

The evolution of depositional environments in the Late Pennsylvanian-early Permian of the
Paradox Basin in Utah, USA, is investigated through detailed sedimentological and high …

Loess is abundant today, primarily in mid-to high-latitude regions, and is well recognized as
a high-fidelity archive of terrestrial climate change. Much of this 'Quaternary'loess is linked …

Consideration of petrographic and U-Pb provenance data and paleocurrent analysis of
Kungurian (upper Leonardian) Cutler Group strata in the salt anticline province of the …

Sedimentologic, pedologic, and magnetic data within the upper Paleozoic lower Cutler beds
of the southwestern Paradox basin (Utah) record high-and low-frequency climate changes …

The Lower Permian (Wolfcampian) Abo Formation of south-central New Mexico was
deposited by a silt-dominated fluvial system along the western half of the Orogrande basin a …

Fluvial systems and their preserved stratigraphic expression as the fill of evolving basins are
controlled by multiple factors, which can vary both spatially and temporally, including …

Abstract The Permo-Pennsylvanian Cutler Formation in the proximal Paradox basin
(western equatorial Pangea) has long been interpreted as low-latitude alluvial-fan deposits …

Abstract The Pennsylvanian to Permian lower Cutler beds collectively form the lowermost
stratigraphic unit of the Cutler Group in the Paradox Basin, southeast Utah. The lower Cutler …

Loading of subsurface salt during accumulation of fluvial strata can result in halokinesis and
the growth of salt pillows, walls and diapirs. Such movement may eventually result in the …