Frontal and lateral submarine lobe fringes: comparing sedimentary facies, architecture and flow processes

YT Spychala, DM Hodgson, A Prélat… - Journal of …, 2017‏ - pubs.geoscienceworld.org
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 …

Structural classification, discharge statistics, and recession analysis from the springs of the Gran Sasso (Italy) carbonate aquifer; comparison with selected analogues …

G Medici, V Lorenzi, C Sbarbati, M Manetta, M Petitta - Sustainability, 2023‏ - mdpi.com
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 …

Transitional flow deposits on submarine lobe flank (Veřovice and Lhoty Fms, Albian–Cenomanian, Polish Outer Carpathians)

P Łapcik - Sedimentary Geology, 2023‏ - Elsevier
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 …

Hybrid event bed character and distribution linked to turbidite system sub‐environments: The North Apennine Gottero Sandstone (north‐west Italy)

M Fonnesu, F Felletti, PDW Haughton… - …, 2018‏ - Wiley Online Library
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 …

The thick-bedded tail of turbidite thickness distribution as a proxy for flow confinement: Examples from tertiary basins of central and northern Apennines (Italy)

M Marini, F Felletti, S Milli, M Patacci - Sedimentary Geology, 2016‏ - Elsevier
This study reviews the thickness statistics of non-channelized turbidites from four tertiary
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

GA Henstra, SA Grundvåg, EP Johannessen… - Marine and Petroleum …, 2016‏ - Elsevier
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 …

Evolving fill‐and‐spill patterns across linked early post‐rift depocentres control lobe characteristics: Los Molles Formation, Argentina

AMLJ Privat, J Peakall, DM Hodgson… - …, 2024‏ - Wiley Online Library
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 …

Deep-water channel-lobe transition zone dynamics: Processes and depositional architecture, an example from the Karoo Basin, South Africa

HL Brooks, DM Hodgson, RL Brunt… - GSA …, 2018‏ - pubs.geoscienceworld.org
Submarine channel-lobe transition zones separate well-defined channels from well-defined
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

E Ghaderpour, C Masciulli, M Zocchi, F Bozzano… - Remote Sensing, 2024‏ - mdpi.com
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 …

Spatial variability in depositional reservoir quality of deep-water channel-fill and lobe deposits

D Bell, IA Kane, ASM Pontén, SS Flint… - Marine and Petroleum …, 2018‏ - Elsevier
Initial porosity and permeability in deep-water systems are controlled by primary
sedimentary texture and mineralogy. Therefore, understanding the sedimentary processes …