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[HTML][HTML] Cenozoic uplift and erosion of the Norwegian Barents Shelf–A review
Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …
timing and exact magnitude. The intricate relationship between different geodynamic …
Deep-water depositional systems supplied by shelf-incising submarine canyons: Recognition and significance in the geologic record
It is well established that sedimentary margins grow by sediments bypassing through shelf-
and slope-incising canyons onto the basin floor and by sediments being deposited …
and slope-incising canyons onto the basin floor and by sediments being deposited …
Deciphering Earth's natural hourglasses: perspectives on source-to-sink analysis
Production, transport, and deposition of siliciclastic sediments takes place across changing
altitudes, physical processes, environments, and controls en route from source to sink …
altitudes, physical processes, environments, and controls en route from source to sink …
Stratigraphic expression of the Paleocene-Eocene Thermal Maximum climate event during long-lived transient uplift—An example from a shallow to deep-marine …
Seismic geomorphology and stratigraphic analysis can reveal how source-to-sink systems
dynamically respond to climatic and tectonic forcing. This study uses seismic reflection data …
dynamically respond to climatic and tectonic forcing. This study uses seismic reflection data …
Source‐to‐sink analysis of ancient sedimentary systems using a subsurface case study from the Møre‐Trøndelag area of southern Norway: Part 2–sediment dispersal …
The composition, volume and stratigraphic organisation of submarine fan systems deposited
along continental margins are expected to reflect the landscape from which the sediment …
along continental margins are expected to reflect the landscape from which the sediment …
Multi‐scale constraints of sediment source to sink systems in frontier basins: a forward stratigraphic modelling case study of the Levant region
N Hawie, R Deschamps, D Granjeon, FH Nader… - Basin …, 2017 - earthdoc.org
Recent scientific work has highlighted the presence of an up to 12 km thick Cenozoic
siliclastic and carbonate infill in the Levant Basin. Since the Late Eocene, several regional …
siliclastic and carbonate infill in the Levant Basin. Since the Late Eocene, several regional …
Linking an Early Triassic delta to antecedent topography: Source-to-sink study of the southwestern Barents Sea margin
Present-day catchments adjacent to sedimentary basins may preserve geomorphic
elements that have been active through long intervals of time. Relicts of ancient catchments …
elements that have been active through long intervals of time. Relicts of ancient catchments …
Geological controls on the geometry of incised‐valley fills: Insights from a global dataset of late‐Quaternary examples
Incised valleys that develop due to relative sea‐level change are common features of
continental shelves and coastal plains. Assessment of the factors that control the geometry …
continental shelves and coastal plains. Assessment of the factors that control the geometry …
Crustal taper and topography at passive continental margins
Terra Nova, 23, 349–361, 2011 Abstract The long‐term evolution of kilometre (s) high,
seaward‐facing escarpments at passive margins is linked directly to the crustal thinning …
seaward‐facing escarpments at passive margins is linked directly to the crustal thinning …
Mass-balance constraints on stratigraphic interpretation of linked alluvial–coastal–shelfal deposits from source to sink: example from Cretaceous Western Interior …
Experimental work suggests that the rate of upstream-to-downstream loss of sediment from
an active depositional system to permanent storage exerts a fundamental control on …
an active depositional system to permanent storage exerts a fundamental control on …