Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

Finn Mørk; Tove Nielsen; Francisca Staines-Urias; Antoon Kuijpers

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

Finn Mørk, Tove Nielsen, Francisca Staines-Urias, Antoon Kuijpers

Publikation: Bidrag til bog/rapport/konferenceproceedings › Konferenceartikel i proceedings

Resumé

NSOW flowing through the Faroe-Shetland Channel has a complex flowing pattern into the Iceland Basin. One branch flows across the Wyville-Thomson Ridge, along the southern flanks of the Faroe, Bill Bailey and Lousy Banks before turning north along the western flank of Lousy Bank. A general increase in the Norwegian Sea
Overflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.

Originalsprog	Engelsk
Titel	Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010
Redaktører	F. Javier Hernández-Molina, Dorrik A.V. Stow, Estefanía Llave, Michele Rebesco, Gemma Ercilla, David van Rooij, Anxo Mena, Juan T. Vázquez, Antje Voelker
Forlag	Sociedad Geologica de Espana
Sider	127-128
Antal sider	2
Status	Udgivet - 2010
Begivenhed	Deep-water circulation: Processes & products. International Congress - Baiona, Spanien Varighed: 16 jun. 2010 → 18 jun. 2010

Publikationsserier

Navn	Geo-Temas
Vol/bind	11

Konference

Konference	Deep-water circulation: Processes & products. International Congress
Land/Område	Spanien
By	Baiona
Periode	16/06/10 → 18/06/10

Programområde

Programområde 5: Natur og klima

Adgang til dokumentet

https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdfLicens: Ikke-specificeret

Citationsformater

Mørk, F., Nielsen, T., Staines-Urias, F., & Kuijpers, A. (2010). Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. I F. J. Hernández-Molina, D. A. V. Stow, E. Llave, M. Rebesco, G. Ercilla, D. van Rooij, A. Mena, J. T. Vázquez, & A. Voelker (red.), Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010 (s. 127-128). Sociedad Geologica de Espana. https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdf

Mørk, Finn ; Nielsen, Tove ; Staines-Urias, Francisca et al. / Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. red. / F. Javier Hernández-Molina ; Dorrik A.V. Stow ; Estefanía Llave ; Michele Rebesco ; Gemma Ercilla ; David van Rooij ; Anxo Mena ; Juan T. Vázquez ; Antje Voelker. Sociedad Geologica de Espana, 2010. s. 127-128 (Geo-Temas, Bind 11).

@inproceedings{c358a74fe2764c9abfa41cf4ae31d845,

title = "Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin",

abstract = "NSOW flowing through the Faroe-Shetland Channel has a complex flowing pattern into the Iceland Basin. One branch flows across the Wyville-Thomson Ridge, along the southern flanks of the Faroe, Bill Bailey and Lousy Banks before turning north along the western flank of Lousy Bank. A general increase in the Norwegian SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.",

author = "Finn M{\o}rk and Tove Nielsen and Francisca Staines-Urias and Antoon Kuijpers",

year = "2010",

language = "English",

series = "Geo-Temas",

publisher = "Sociedad Geologica de Espana",

pages = "127--128",

editor = "Hern{\'a}ndez-Molina, {F. Javier} and Stow, {Dorrik A.V.} and Estefan{\'i}a Llave and Michele Rebesco and Gemma Ercilla and {van Rooij}, David and Anxo Mena and V{\'a}zquez, {Juan T.} and Antje Voelker",

booktitle = "Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010",

address = "Spain",

note = "Deep-water circulation: Processes & products. International Congress ; Conference date: 16-06-2010 Through 18-06-2010",

}

Mørk, F , Nielsen, T, Staines-Urias, F & Kuijpers, A 2010, Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. i FJ Hernández-Molina, DAV Stow, E Llave, M Rebesco, G Ercilla, D van Rooij, A Mena, JT Vázquez & A Voelker (red), Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. Sociedad Geologica de Espana, Geo-Temas, bind 11, s. 127-128, Deep-water circulation: Processes & products. International Congress, Baiona, Spanien, 16/06/10. <https://sge.usal.es/archivos/GEO_TEMAS/Geo_temas11.pdf>

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. / Mørk, Finn ; Nielsen, Tove; Staines-Urias, Francisca et al.
Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. red. / F. Javier Hernández-Molina; Dorrik A.V. Stow; Estefanía Llave; Michele Rebesco; Gemma Ercilla; David van Rooij; Anxo Mena; Juan T. Vázquez; Antje Voelker. Sociedad Geologica de Espana, 2010. s. 127-128 (Geo-Temas, Bind 11).

Publikation: Bidrag til bog/rapport/konferenceproceedings › Konferenceartikel i proceedings

TY - GEN

T1 - Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

AU - Mørk, Finn

AU - Nielsen, Tove

AU - Staines-Urias, Francisca

AU - Kuijpers, Antoon

PY - 2010

Y1 - 2010

N2 - NSOW flowing through the Faroe-Shetland Channel has a complex flowing pattern into the Iceland Basin. One branch flows across the Wyville-Thomson Ridge, along the southern flanks of the Faroe, Bill Bailey and Lousy Banks before turning north along the western flank of Lousy Bank. A general increase in the Norwegian SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.

AB - NSOW flowing through the Faroe-Shetland Channel has a complex flowing pattern into the Iceland Basin. One branch flows across the Wyville-Thomson Ridge, along the southern flanks of the Faroe, Bill Bailey and Lousy Banks before turning north along the western flank of Lousy Bank. A general increase in the Norwegian SeaOverflow Water intensity in the area north of Bill Bailey Bank is shown, based on sediment cores.

M3 - Conference article in proceedings

T3 - Geo-Temas

SP - 127

EP - 128

BT - Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010

A2 - Hernández-Molina, F. Javier

A2 - Stow, Dorrik A.V.

A2 - Llave, Estefanía

A2 - Rebesco, Michele

A2 - Ercilla, Gemma

A2 - van Rooij, David

A2 - Mena, Anxo

A2 - Vázquez, Juan T.

A2 - Voelker, Antje

PB - Sociedad Geologica de Espana

T2 - Deep-water circulation: Processes & products. International Congress

Y2 - 16 June 2010 through 18 June 2010

ER -

Mørk F , Nielsen T, Staines-Urias F, Kuijpers A. Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin. I Hernández-Molina FJ, Stow DAV, Llave E, Rebesco M, Ercilla G, van Rooij D, Mena A, Vázquez JT, Voelker A, red., Deep-water circulation: Processes & products. International Congress. Baiona, Pontevedra, Spain. 16, 17 & 18 June 2010. Sociedad Geologica de Espana. 2010. s. 127-128. (Geo-Temas, Bind 11).

Geological evidence of Norwegian Sea Overflow pathways into the Iceland Basin

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