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Frontal and lateral submarine lobe fringes: comparing sedimentary facies, architecture and flow processes
Submarine lobe-fringe deposits form heterolithic successions that may include a high
proportion of hybrid beds. The identification of lobe-fringe successions aids interpretation of …
proportion of hybrid beds. The identification of lobe-fringe successions aids interpretation of …
Structural classification, discharge statistics, and recession analysis from the springs of the Gran Sasso (Italy) carbonate aquifer; comparison with selected analogues …
The relative importance of karst conduits and fractures in driving groundwater flow affects
the discharge of springs and the long-term availability of water resources. Applying statistics …
the discharge of springs and the long-term availability of water resources. Applying statistics …
Transitional flow deposits on submarine lobe flank (Veřovice and Lhoty Fms, Albian–Cenomanian, Polish Outer Carpathians)
Abstract The Zagórnik-Rzyki studied section includes the upper part of the Veřovice Fm and
the lower part of the Lhoty Fm (Aptian–Albian), which are small fragments of the much …
the lower part of the Lhoty Fm (Aptian–Albian), which are small fragments of the much …
Hybrid event bed character and distribution linked to turbidite system sub‐environments: The North Apennine Gottero Sandstone (north‐west Italy)
This study documents the character and occurrence of hybrid event beds (HEBs) deposited
across a range of deep‐water sub‐environments in the Cretaceous–Palaeocene Gottero …
across a range of deep‐water sub‐environments in the Cretaceous–Palaeocene Gottero …
The thick-bedded tail of turbidite thickness distribution as a proxy for flow confinement: Examples from tertiary basins of central and northern Apennines (Italy)
This study reviews the thickness statistics of non-channelized turbidites from four tertiary
basins of Central-Northern Apennines (Italy), where bed geometry and sedimentary …
basins of Central-Northern Apennines (Italy), where bed geometry and sedimentary …
Depositional processes and stratigraphic architecture within a coarse-grained rift-margin turbidite system: The Wollaston Forland Group, east Greenland
Abstract The Wollaston Forland Basin, NE Greenland, is a half-graben with a Middle
Jurassic to Lower Cretaceous basin-fill. In this outcrop study we investigate the facies …
Jurassic to Lower Cretaceous basin-fill. In this outcrop study we investigate the facies …
Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina
Inherited rift topography controls the sediment routing, timing of sand supply, and
sedimentary linkage of early post‐rift depocentres. Exhumed examples of early post‐rift …
sedimentary linkage of early post‐rift depocentres. Exhumed examples of early post‐rift …
Deep-water channel-lobe transition zone dynamics: Processes and depositional architecture, an example from the Karoo Basin, South Africa
Submarine channel-lobe transition zones separate well-defined channels from well-defined
lobes and form morphologically complicated areas, commonly located at breaks in slope …
lobes and form morphologically complicated areas, commonly located at breaks in slope …
[HTML][HTML] Estimating reactivation times and velocities of slow-moving landslides via PS-InSAR and their relationship with precipitation in Central Italy
Monitoring slow-moving landslides is a crucial task for socioeconomic risk prevention and/or
mitigation. Persistent scatterer interferometric synthetic aperture radar (PS-InSAR) is an …
mitigation. Persistent scatterer interferometric synthetic aperture radar (PS-InSAR) is an …
Spatial variability in depositional reservoir quality of deep-water channel-fill and lobe deposits
Initial porosity and permeability in deep-water systems are controlled by primary
sedimentary texture and mineralogy. Therefore, understanding the sedimentary processes …
sedimentary texture and mineralogy. Therefore, understanding the sedimentary processes …