Zobrazeno 1 - 10
of 47
pro vyhledávání: '"Channel-Lobe Transition Zone"'
Akademický článek
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Publikováno v:
The Depositional Record, Vol 8, Iss 2, Pp 829-868 (2022)
Abstract Channel‐lobe transition zones are dynamic areas located between deepwater channels and lobes. Presented here is a rare example of an exhumed channel‐lobe transition zone from an active‐margin setting, in the Kazusa forearc Basin, Boso
Externí odkaz:
https://doaj.org/article/830d0b1563e54b618db812cc33c40b1d
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Observations from the modern seafloor that suggest turbidity currents tend to erode as they lose channel-levee confinement, rather than decelerating and depositing their sediment load, has driven investigations into sediment gravity flow behaviour at
Externí odkaz:
https://doaj.org/article/a809607c23334784aee94b99b101df1b
Autor:
L. A. S. Hansen, R. S. Healy, L. Gomis-Cartesio, D. R. Lee, D. M. Hodgson, A. Pontén, R. J. Wild
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Scours, and scour fields, are common features on the modern seafloor of deep-marine systems, particularly downstream of submarine channels, and in channel-lobe-transition-zones. High-resolution images of the seafloor have improved the documentation o
Externí odkaz:
https://doaj.org/article/d4af0ca7d2104c0db44f9392aa1a731d
Autor:
Rice, Trezevant Adair
The Mancos Shale is a marine stratigraphic unit deposited in the Western Interior Seaway during Late Cretaceous time (~80 Ma). While dominated by offshore shale/siltstone deposits, anomalous sand-rich intervals within the Aberdeen and Kenilworth Memb
Akademický článek
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Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Observations from the modern seafloor that suggest turbidity currents tend to erode as they lose channel-levee confinement, rather than decelerating and depositing their sediment load, has driven investigations into sediment gravity flow behaviour at
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::bc89edaf567621d551948fb14f7e9490
https://www.frontiersin.org/articles/10.3389/feart.2022.790320/full
https://www.frontiersin.org/articles/10.3389/feart.2022.790320/full
Autor:
David M. Hodgson, R. J. Wild, Luz E. Gomis-Cartesio, Anna Pontén, D. R. Lee, R. S. Healy, Larissa Hansen
Publikováno v:
Frontiers in Earth Science, Vol 9 (2021)
Scours, and scour fields, are common features on the modern seafloor of deep-marine systems, particularly downstream of submarine channels, and in channel-lobe-transition-zones. High-resolution images of the seafloor have improved the documentation o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4d9a7d0067ff72147556aa7be0d32650
https://www.frontiersin.org/articles/10.3389/feart.2021.737932/full
https://www.frontiersin.org/articles/10.3389/feart.2021.737932/full
Akademický článek
Tento výsledek nelze pro nepřihlášené uživatele zobrazit.
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Publikováno v:
Sedimentology : the journal of the International Association of Sedimentologists 68 (2021), Nr. 4
Sedimentology : the journal of the International Association of Sedimentologists
Sedimentology : the journal of the International Association of Sedimentologists
Jets that expand from an orifice into an ambient water body represent a basic flow model for depositional environments related to expanding flows. Momentum-dominated jets evolve into gravity-dominated density flows. To understand this transition and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6096327b0c1ba7c35c76b04ca8ba2324
https://www.repo.uni-hannover.de/handle/123456789/13943
https://www.repo.uni-hannover.de/handle/123456789/13943