Abstract Chlorite, an Fe-and Mg-rich aluminosilicate clay, may be either detrital or authigenic
in sandstones. Detrital chlorite includes mineral grains, components of lithic grain, matrix …

The kaolinite-group minerals kaolinite, dickite, nacrite, halloysite including its metaform and
their associates allophane and imogolite are phyllosilicates characterized by a rather simple …

The Aptian evaporitic transitional sequence (sag phase) of the Brazilian marginal basins
records the first connection between the Central and South Atlantic oceans in the equatorial …

Abstract The Central European Variscides and their epicontinental basins and grabens
(Mesoeurope sensu Stille) subsided into the uplifted basement as well as the Alpidic …

Abstract The Rifian Corridor was a seaway between the Atlantic Ocean and the
Mediterranean Sea during the late Miocene. The seaway progressively closed, leading to …

Crevasse subdeltas develop on modern river-dominated delta plains, and may be affected
by the interaction of river currents and marine processes. However, their sedimentology and …

Existing facies models of tide‐dominated deltas largely omit fine‐grained, mud‐rich
successions. Sedimentary facies and sequence stratigraphic analysis of the exceptionally …

Deposits of marginal marine depositional systems make up significant hydrocarbon
reservoirs in the rock record. These systems are deposited by a complex interaction …

Interpreting the whole range of fluvial, wave, and tidal interactions recorded in shallow-
marine, coastal successions can be challenging. The complexity arises because …

Sandstone tidal cross‐strata are the predominant sedimentary feature of strait‐fill
stratigraphic successions. However, although widely described in numerous studies, tidal …