The Tell-Rif (Tell in Algeria and Tunisia; Rif in Morocco) is the orogenic system fringing to
the south the West Mediterranean basins. This system comprises three major tectonic …

The fluvio-tidal transition zone (FTZ) is sedimentologically and ichnologically complex,
encompassing variable sedimentary facies. Published research on the FTZ implies a wide …

Crevasse-splay deposits form a volumetrically significant component of many fluvial
overbank successions (up to 90% in some successions). Yet the relationships between the …

A branch of the Paleo‐Tethys Ocean once separated the north China plate from the south
China plate. However, the mode of closure of the northeastern Paleo‐Tethys Ocean during …

Sedimentation in the fluvial–marine transition is governed by the interaction of river and tidal
currents. Tidal currents act continuously, albeit with small variations in strength as a result of …

Despite advances in estuarine facies models, ancient bayhead delta deposits are not widely
recognized or utilized, and their facies characteristics are poorly documented …

The large-scale effects of tidal waves entering the Cretaceous Western Interior Seaway from
the Gulf of Mexico have previously been modeled, but the field evidence for tides in the …

A source‐to‐sink analysis incorporating geochronometric and thermochronometric data from
the Sevier fold‐thrust belt (SFTB) and proximal synorogenic strata of the Canyon Range …

Abstract The Lower Jurassic Junggar Basin is a low-accommodation basin in northwestern
China. Because of low subsidence rates and a warm, wet climate, deposits of the Central …

Quantitative reconstruction of palaeohydrology from fluvial stratigraphy provides
sophisticated insights into the response, and relative impact, of tectonic and climatic drivers …