Evidence for current-controlled morphology along the western slope of Hatton Bank (Rockall Plateau, NE Atlantic Ocean)-Reference-Cited by-同舟云学术

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Evidence for current-controlled morphology along the western slope of Hatton Bank (Rockall Plateau, NE Atlantic Ocean)

Published:2009-09-04 Issue:2 Volume:30 Page:99-111
ISSN:0276-0460
Container-title:Geo-Marine Letters
language:en
Short-container-title:Geo-Mar Lett

Author:

Sayago-Gil Miriam,Long David,Hitchen Kenneth,Díaz-del-Río Víctor,Fernández-Salas Luis Miguel,Durán-Muñoz Pablo

Publisher

Springer Science and Business Media LLC

Subject

Earth and Planetary Sciences (miscellaneous),Geotechnical Engineering and Engineering Geology,Environmental Science (miscellaneous),Oceanography

Link

http://link.springer.com/content/pdf/10.1007/s00367-009-0163-5.pdf

Reference41 articles.

1. Bailey W, Shannon PM, Walsh JJ, Unnithan V (2003) The spatial distribution of faults and deep sea carbonate mounds in the Porcupine Basin, offshore Ireland. Mar Petrol Geol 20:509–522

2. Bianchi GG, McCave IN (2000) Hydrography and sedimentation under the deep western boundary current on Björn and Gardar Drifts, Iceland Basin. Mar Geol 165:137–169

3. Due L, Van Aken HM, Boldreel LO, Kuijpers A (2006) Seismic and oceanographic evidence of the present-day bottom-water dynamics in the Lousy Bank-Hatton Bank area, NE Atlantic. Deep Sea Res I 53:1729–1741

4. Faugères JC, Mézerais ML, Stow DAV (1993) Contourite drift types and their distribution in the North and South Atlantic Ocean Basins. Sed Geol 82:189–203

5. Faugères JC, Stow DAV, Imbert P, Viana AR (1999) Seismic features diagnostic of contourite drifts. Mar Geol 162:1–38

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