Results 221 to 230 of about 535,744 (290)
Estimating the benthic efflux of dissolved iron on the Ross Sea continental shelf
Peter N Sedwick +2 more
exaly +2 more sources
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New Zealand Journal of Geology and Geophysics, 2018
This paper provides new maps of the surficial sediment distribution on the continental shelf (0∼150 m water depth) of New Zealand based on a new database – nzSEABED. The maps of percent mud, sand, gravel and carbonate, are compared with previous research
H. Bostock +7 more
semanticscholar +1 more source
This paper provides new maps of the surficial sediment distribution on the continental shelf (0∼150 m water depth) of New Zealand based on a new database – nzSEABED. The maps of percent mud, sand, gravel and carbonate, are compared with previous research
H. Bostock +7 more
semanticscholar +1 more source
Modeling the carbon fluxes of the northwest European continental shelf: Validation and budgets
Sarah Wakelin, Jason Holt, J I Allen
exaly +2 more sources
2019
In the next two chapters, we will take a tour aboard an imaginary hover car to visit the world’s continental shelves and the deep ocean. The continental shelf (as the name suggests) is the submerged part of the continents, and the features we see underwater are comparable to those we see today along the coast.
openaire +2 more sources
In the next two chapters, we will take a tour aboard an imaginary hover car to visit the world’s continental shelves and the deep ocean. The continental shelf (as the name suggests) is the submerged part of the continents, and the features we see underwater are comparable to those we see today along the coast.
openaire +2 more sources
New Zealand Journal of Geology and Geophysics, 1966
Abstract Explorations of the structure of the piles of sediment underlying parts of the continental shelf, or terrace, have confirm the theory that in general this ubiquitous feature has been formed by up‐ and out‐growth due to the deposition on the shelf (as topsets beds) and on the continental slope (as foreset beds) during a ...
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Abstract Explorations of the structure of the piles of sediment underlying parts of the continental shelf, or terrace, have confirm the theory that in general this ubiquitous feature has been formed by up‐ and out‐growth due to the deposition on the shelf (as topsets beds) and on the continental slope (as foreset beds) during a ...
openaire +1 more source
Freshwater Peat on the Continental Shelf
Science, 1967Freshwater peats from the continental shelf off northeastern United States contain the same general pollen sequence as peats from ponds that are above sea level and that are of comparable radiocarbon ages. These peats indicate that during glacial times of low sea level terrestrial vegetation covered the region that is now the continental shelf in an ...
K O, Emery +4 more
openaire +2 more sources
2010
The Aegean continental shelf dispute involves the delimitation of the respective sovereign rights of the two countries in the Aegean seabed and its subsoil.
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The Aegean continental shelf dispute involves the delimitation of the respective sovereign rights of the two countries in the Aegean seabed and its subsoil.
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The Continental Shelf Hypothesis
Nutrition and Health, 2002Marc, Verhaegen, Stephen, Munro
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