Zobrazeno 1 - 7
of 7
pro vyhledávání: '"J. S. Laberg"'
Publikováno v:
Climate of the Past, Vol 19, Pp 1321-1343 (2023)
The Greenland Ice Sheet (GrIS) responds rapidly to the present climate; therefore, its response to the predicted future warming is of concern. To learn more about the impact of future climatic warming on the ice sheet, decoding its behavior during pa
Externí odkaz:
https://doaj.org/article/a35a741f832e4283a49fc24ff7fb65f8
Publikováno v:
The Cryosphere, Vol 14, Pp 4475-4494 (2020)
The presence of a grounded Greenland Ice Sheet on the northeastern part of the Greenland continental shelf during the Last Glacial Maximum is supported by new swath bathymetry and high-resolution seismic data, supplemented with multi-proxy analyses o
Externí odkaz:
https://doaj.org/article/9eaccadedaeb4991a8f4b45429f461e5
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 11, Pp n/a-n/a (2020)
Abstract The onset and evolution of the middle to late Cenozoic “icehouse” world was influenced by the development of the global ocean circulation linking the Norwegian–Greenland Sea‐Arctic Ocean to the Atlantic Ocean. The evolution of the ea
Externí odkaz:
https://doaj.org/article/6969dc743bf749bf841572cfc8dd3d5e
Publikováno v:
Scopus-Elsevier
Three-dimensional seismic data from the Sorvestsnaget Basin, south-western Barents Sea continental margin are used to investigate a Middle Eocene depositional system. It is composed of sandstones interbedded with mudstones inferred to have accumulate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e2e7b19ae9d56871fc5fefbbada35f2e
https://doi.org/10.3997/2214-4609.201401348
https://doi.org/10.3997/2214-4609.201401348
Autor:
T. O. Vorren, J. S. Laberg
Publikováno v:
European Margin Sediment Dynamics ISBN: 9783642626890
The Traenadjupet Slide is located on the continental slope of Norway immediately NE of the Voring Plateau (Dowdeswell et al. 1996). The slide-affected area extends from the shelf break to >3,000 m water depth in the Lofoten Basin, implying a run-out
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::412a50a7382435ce5e370fb32081b290
https://doi.org/10.1007/978-3-642-55846-7_9
https://doi.org/10.1007/978-3-642-55846-7_9
Publikováno v:
Scopus-Elsevier
Three-dimensional, two-dimensional seismic data and well 7216/11-1S data from the Sorvestsnaget Basin south-western Barents Sea continental margin are used to investigate areal distribution, architectures and provenance of the Middle Eocene sand-bear
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4738bb2bb47296b14fdf7b721a2a7f96
http://www.scopus.com/inward/record.url?eid=2-s2.0-80052485117&partnerID=MN8TOARS
http://www.scopus.com/inward/record.url?eid=2-s2.0-80052485117&partnerID=MN8TOARS
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