Results 281 to 290 of about 2,368,102 (348)
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How submarine channels (re)shape continental margins

Journal of Sedimentary Research, 2020
ABSTRACTSubmarine landscapes, like their terrestrial counterparts, are sculpted by autogenic sedimentary processes toward morphologies at equilibrium with their allogenic controls. While submarine channels and nearby, inter-channel continental-margin areas share boundary conditions (e.g., terrestrial sediment supply, tectonic deformation), there are ...
Luke A. Pettinga, Zane R. Jobe
openaire   +2 more sources

Curvature-induced secondary flow in submarine channels

Environmental Fluid Mechanics, 2014
The curvature-driven secondary flow in sinuous submarine channels has been a subject of considerable interest and controversy. Here, results from numerical model studies involving saline flow in laboratory-scale channels are presented. A 3D finite volume model of density and turbidity currents is used and simulations are run with different inflow ...
Hesham Ezz, Jasim Imran
openaire   +2 more sources

Initiation and evolution of fault‐controlled slope‐parallel submarine channels: Miocene eastern slope of Yinggehai Basin, South China Sea

Basin Research, 2022
Submarine channels act as the main conduits for the transport of sediment to deep‐water basins by sediment gravity flows. The interplay between fault‐related deformation and the initiation and development of the channels is poorly known. Here, we present
Zhen Wang   +11 more
semanticscholar   +1 more source

Flow structure in sinuous submarine channels: Velocity and turbulence structure of an experimental submarine channel

Marine Geology, 2006
Submarine channels have long been considered analogous to meandering fluvial channels due to their similar planform geometry, and this has given rise to strong analogies in terms of the fluid dynamics of these channel types. However, there is a paucity of direct measurements detailing the structure of velocity or sediment concentration, and nothing is ...
Keevil, G.   +3 more
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Two-channel submarine carrier telegraph system

Electrical Engineering, 1950
ANEW 2-channel carrier telegraph system for short submarine telegraph cables has been developed for the Western Union Key West-Havana cables, about 100 nautical miles in length and with attenuations up to 80 decibels at 1,000 cycles per second. It utilizes standard land-line frequency-modulation channel terminal equipment and provides 50-cycle ...
E. L. Newell, G. H. Cramer
openaire   +1 more source

Submarine channel response to intrabasinal tectonics: The influence of lateral tilt

AAPG Bulletin, 2010
Lateral tilting is a common deformation style in extensional basins; its influence on subaerial channels is, to a degree, understood and may be significant, controlling the style of channel development and the resultant sand-body architecture. Growth faulting and lateral tilting in turbidite channel systems have been demonstrated from three-dimensional
Kane, Ian A.   +3 more
openaire   +1 more source

Submarine lava tubes and channels

Bulletin of Volcanology, 1986
High-resolution, side-looking sonar surveys of the East Pacific rise and seamounts in the eastern Pacific have revealed the common presence of lava tubes and channels in seafloor volcanic terrains. Tube and channel systems commonly issue from small volcanic cones or domes, are continuous for distances of 1–3 km, and are considered to be important in ...
openaire   +1 more source

Submarine channel evolution: active channels in fjords, British Columbia, Canada

Geo-Marine Letters, 2012
Seafloor channel systems are well developed in several British Columbia (Canada) fjords, including Knight, Bute and Toba inlets. The channels are active conduits for turbidity currents during episodic failures of delta fronts at the fjord heads. Recently acquired swath multibeam bathymetric data enabled a complete and detailed assessment of the form of
Kim W. Conway   +3 more
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Controls on sinuosity evolution within submarine channels

Geology, 2008
The planform geometry of submarine channels commonly exhibits a spatio-temporal stability generally not observed in fluvial channels. As such, submarine channels tend to lack the meander loop cutoffs and frequent avulsion history typical of fluvial channels. fluvial sinuosity develops through inner-bend deposition and outer-bend erosion.
Kane, Ian A.   +2 more
openaire   +2 more sources

LATITUDINAL CHANGES IN THE MORPHOLOGY OF SUBMARINE CHANNELS: REEVALUATING THE EVIDENCE FOR THE INFLUENCE OF THE CORIOLIS FORCE

LATITUDINAL CONTROLS ON STRATIGRAPHIC MODELS AND SEDIMENTARY CONCEPTS, 2017
Published in "Latitudinal Controls on Stratigraphic Models and Sedimentary Concepts", SEPM Special Publication 108, September 2017, DOI: 10.2110/sepmsp.108.02.
Z. Sylvester
semanticscholar   +1 more source

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