Interaction between aeolian and rivers in a dryland fluvial system with remote sensing techniques

Grain size distribution of unconsolidated sediments at the terminus of a semi-arid river system and its use to reconstruct paleo-geomorphology

On the origin of crevasse-splay amalgamation in the Huesca fluvial fan (Ebro Basin, Spain): Implications for connectivity in low net-to-gross fluvial deposits

Floodplain deposits are abundant in low-gradient dryland river systems, but their contribution to connected reservoir volumes has not yet been fully acknowledged due to their poor detectability with typical wireline log suites and relatively-lower reservoir quality. This study presents an analysis of stacked crevasse splays in the distal part of...