Zobrazeno 1 - 10
of 66
pro vyhledávání: '"mega‐scale glacial lineations"'
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 89, Iss 2, Pp 100-120 (2017)
The SIS (Scandinavian Ice Sheet) became divided into several active, semi-independent ice lobes during the last deglaciation ca 13 000–10 000 years ago. The largest of them, the North Karelian/Oulu Ice Lobe (NKIL/OIL), covered vast areas in central
Externí odkaz:
https://doaj.org/article/168f7874f1164ec094c76eb597d1c4c4
Autor:
Kristin M. M. Rohr, Scott R. Dallimore, Young Keun Jin, Gary Taylor, Michael Wamsteeker, Jong Kuk Hong, Edward L. King, Michael Riedel
Mega‐scale glacial lineations formed by the raking of ice shelves across the seafloor have been reported from multiple polar regions. Here, we present the first evidence of continental slope situated buried lineations in the southern Canadian Beauf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::07136f27a758cdfbce0b86bfda67c158
https://doi.org/10.1002/esp.5125
https://doi.org/10.1002/esp.5125
Publikováno v:
Bulletin of the Geological Society of Finland, Vol 89, Iss 2, Pp 100-120 (2017)
The SIS (Scandinavian Ice Sheet) became divided into several active, semi-independent ice lobes during the last deglaciation ca 13 000–10 000 years ago. The largest of them, the North Karelian/Oulu Ice Lobe (NKIL/OIL), covered vast areas in central
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8b75f1a40e6479d575e15e5498d532de
http://www.geologinenseura.fi/bulletin/Volume89/Bulletin_vol89_2_100-120_2017_Nikarmaa-etal.pdf
http://www.geologinenseura.fi/bulletin/Volume89/Bulletin_vol89_2_100-120_2017_Nikarmaa-etal.pdf
Akademický článek
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Akademický článek
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Publikováno v:
Marine Geology
Accepted manuscript version. Published version available at https://doi.org/10.1016/j.margeo.2018.03.002. Accepted manuscript version, licensed CC BY-NC-ND 4.0. Recent developments in seismic acquisition systems and seismic data visualization have co
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::de57ee07f819080104e4d029663dbb0e
https://hdl.handle.net/1956/18586
https://hdl.handle.net/1956/18586
Publikováno v:
Marine geology, 2018, Vol.402, pp.153-164 [Peer Reviewed Journal]
Submitted manuscript version: Published version available in Relationship between mega-scale glacial lineations and iceberg ploughmarks on the Bjørnøyrenna Palaeo-Ice Stream bed, Barents Sea (2017). Mega-scale glacial lineations (MSGLs) are ridge-g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::739f0a8d23ea68ccc921f85c433fcdc0
https://hdl.handle.net/10037/13124
https://hdl.handle.net/10037/13124
Publikováno v:
Bellwald, B., Planke, S., Piasecka, E.D., Matar, M.A. & Andreassen, K. (2018). Ice-stream dynamics of the SW Barents Sea revealed by high-resolution 3D seismic imaging of glacial deposits in the Hoop area. Marine Geology, 402, 165-183.
Externí odkaz:
https://hdl.handle.net/10037/13354
Publikováno v:
Piasecka, E.D., Stokes, C.R., Winsborrow, M.C.M. & Andreassen, K. (2018). Relationship between mega-scale glacial lineations and iceberg ploughmarks on the Bjørnøyrenna Palaeo-Ice Stream bed, Barents Sea. Marine Geology.
Externí odkaz:
https://hdl.handle.net/10037/13124
Autor:
Spagnolo, M., Bartholomaus, T.C., Clark, C.D., Stokes, C.R., Atkinson, N., Dowdeswell, J.A., Ely, J., Graham, A.G.C., Hogan, K.A., King, E.C., Larter, R.D., Livingstone, S.J., Pritchard, H.D.
Publikováno v:
Journal of geophysical research : earth surface, 2017, Vol.122(7), pp.1355-1373 [Peer Reviewed Journal]
Ice stream bed topography contains key evidence for the ways ice streams interact with, and are potentially controlled by, their beds. Here we present the first application of two-dimensional Fourier analysis to 22 marine and terrestrial topographies
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::41b666fd8e1482f9d801b9d54bafb56f
https://doi.org/10.1002/2016JF004154
https://doi.org/10.1002/2016JF004154