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Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
At geologic timescales, a significant proportion of the sediment eroded from continents is transferred from rivers to littoral cells, then through submarine canyons to deep ocean basins. Accumulation and occasional discharge of sediment from canyon h
Externí odkaz:
https://doaj.org/article/5b996fe2d3904d52a0226c5996aec611