A sedimentologic, ichnologic, and architectural analysis of the upper Sego and Neslen fms (Campanian) along the Book Cliffs near Harley Dome, UT document a paleoenvironmental evolution from wave and tidally-modified deltaic deposits of the upper Sego Fm to tidally influenced estuarine deposits of the Neslen Fm. Paleoenvironments of the upper Sego include tidal barforms and interdistributary bays while those of the Neslen include distal to proximal tidal-fluvial channels, sandy and muddy tidal flats, and floodplains. A total of 28 trace fossil forms were identified in the upper Sego and Neslen fms including 14 fully marine traces, 11 facies breaking traces, (those traces that can exist in fresh, brackish, or marine salinities), 1 freshw...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
The backwater zone of a river is its distal reach downstream of the point at which the streambed ele...
The Ferron Sandstone Member of the Cretaceous Mancos Shale is composed of three fluvio-deltaic wedge...
A recent, revised regional sequence stratigraphic correlation indicates that outcrop belts along the...
Discerning the roles of autogenic and allogenic controls on the deposition, accumulation and preserv...
The Campanian (Upper Cretaceous) Neslen Formation which crops out in the Book Cliffs, Utah (USA) has...
The process regime of low-gradient coastal plains, delta plains and shorelines can change during tra...
The Campanian (Upper Cretaceous) Neslen Formation which crops out in the Book Cliffs, Utah (USA) has...
The stratigraphic architecture of marginal marine successions records the interplay of autogenic and...
The process regime of low-gradient coastal plains, delta plains and shorelines can change during tra...
The Neslen Formation of the Mesaverde Group (eastern Book Cliffs, Utah) accumulated along the wester...
The Neslen Formation of the Mesaverde Group (eastern Book Cliffs, Utah) accumulated along the wester...
The Upper Cretaceous Ferron Sandstone of east-central Utah is an important source of coal and contai...
Integration of facies and trace-fossil evidence tests and refines depositional models constructed so...
Integration of facies and trace-fossil evidence tests and refines depositional models constructed so...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
The backwater zone of a river is its distal reach downstream of the point at which the streambed ele...
The Ferron Sandstone Member of the Cretaceous Mancos Shale is composed of three fluvio-deltaic wedge...
A recent, revised regional sequence stratigraphic correlation indicates that outcrop belts along the...
Discerning the roles of autogenic and allogenic controls on the deposition, accumulation and preserv...
The Campanian (Upper Cretaceous) Neslen Formation which crops out in the Book Cliffs, Utah (USA) has...
The process regime of low-gradient coastal plains, delta plains and shorelines can change during tra...
The Campanian (Upper Cretaceous) Neslen Formation which crops out in the Book Cliffs, Utah (USA) has...
The stratigraphic architecture of marginal marine successions records the interplay of autogenic and...
The process regime of low-gradient coastal plains, delta plains and shorelines can change during tra...
The Neslen Formation of the Mesaverde Group (eastern Book Cliffs, Utah) accumulated along the wester...
The Neslen Formation of the Mesaverde Group (eastern Book Cliffs, Utah) accumulated along the wester...
The Upper Cretaceous Ferron Sandstone of east-central Utah is an important source of coal and contai...
Integration of facies and trace-fossil evidence tests and refines depositional models constructed so...
Integration of facies and trace-fossil evidence tests and refines depositional models constructed so...
Shorefaces can display strong facies variability and integration of sedimentology and ichnology prov...
The backwater zone of a river is its distal reach downstream of the point at which the streambed ele...
The Ferron Sandstone Member of the Cretaceous Mancos Shale is composed of three fluvio-deltaic wedge...