The origin of deep-water, coral-topped mounds in the northern Rockall Trough, Northeast Atlantic

Author:

Masson D.G,Bett B.J,Billett D.S.M,Jacobs C.L,Wheeler A.J,Wynn R.B

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference48 articles.

1. Armishaw, J.E., Holmes, R.W., Stow, D.A.V., 1998. Morphology and sedimentation on the Hebrides slope and Barra Fan, NW UK continental margin. In: Stoker, M.S., Evans, D., Cramp, A. (Eds.), Geological Processes on Continental Margins: Sedimentation, Mass-Wasting and Stability. Spec. Publication 129, The Geological Society, London, pp. 81–104.

2. An empirical model for the development and equilibrium morphology of current ripples in fine sand;Baas;Sedimentology,1999

3. Berndt, C., Bunz, S., Mienert, J., in press. Polygonal fault systems on the mid-Norwegian margin: a long-term source for fluid flow. In: van Rensbergen, P., Morley, C. (Eds.), Subsurface Sediment Mobilisation. Spec. Publication, The Geological Society, London.

4. Bett, B.J., 1999. RRS Charles Darwin Cruise 112C. Atlantic Margin Environmental Survey: Seabed Survey of deep-water areas (17th Round Tranches) to the north and west of Scotland. Southampton Oceanography Centre Cruise Rpt. 26, Southampton Oceanography Centre, 172 pp.

5. Bett, B.J., 2001a. RRS Charles Darwin cruise 123C legs C and D. 2000. White Zone (WhiZ) Environmental Survey: Seabed survey of the deep-waters to the north and west of Scotland. Unpublished cruise report to Department of Trade and Industry.

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