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pro vyhledávání: '"S. W. Funke"'
Publikováno v:
Geoscientific Model Development, Vol 10, Iss 3, Pp 1051-1068 (2017)
Turbidity currents are one of the main drivers of sediment transport from the continental shelf to the deep ocean. The resulting sediment deposits can reach hundreds of kilometres into the ocean. Computer models that simulate turbidity currents and t
Externí odkaz:
https://doaj.org/article/dc043343a5bf47f8b2757c7e02fb0d7a