The last phase of the Storegga Slide: Simulation of retrogressive slide dynamics and comparison with slide-scar morphology

Ormen Lange - An Integrated Study for Safe Field Development in the Storegga Submarine Area

Volumn , Issue , 2005, Pages 171-178

  Gauer, Peter ^a   Kvalstad, Tore J ^a   Forsberg, Carl Fredrik ^a   Bryn, Petter ^b   Berg, Kjell ^b  

^a NORWEGIAN GEOTECHNICAL INSTITUTE   (Norway)

^b STATOIL   (Norway)

Author keywords

[No Author keywords available]

Indexed keywords

RETROGRESSIVE SLIDE DYNAMICS; SLIDE SCAR; STOREGGA SLIDE;

MORPHOLOGY;

EID: 84903034555     PISSN: None     EISSN: None     Source Type: Book    
DOI: 10.1016/j.marpetgeo.2004.10.004     Document Type: Chapter

References (20)

1. Balmforth N.J., Craster R.V. Geophysical aspects of non-Newtonian fluid mechanics. Geomorphological Fluid Mechanics Lecture Notes in Physics 582 2001, Springer, Berlin. N.J. Balmforth, A. Provenzale (Eds.).
2. Berg, K., Solheim, A., Bryn, P., 2005. The Pleistocene to recent geological development of the Ormen Lange area.
3. Bryn, P., Østmo, S.R., Lien, R., Berg, K., Tjelta, T.L., 1998. Slope stability in the deep waters off Mid-Norway. Proceedings of 1998 Offshore Technology Conference, Houston, Texas, May 1998.
4. Bryn P., Berg K., Solheim K., Kvalstad T.J., Forsberg C.F. Explaining the Holocene Storegga Slide. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.12.003.
5. CFX-4.3 Flow Solver User Guide, 1999: ANSYS CFX.
6. De Blasio F.V., Eleverhoi A., Issler D., Harbitz C.B., Bryn P., Lien R. On the dynamics of subaqueous clay rich gravity mass flows-the giant Storegga Slide. Marine and Petroleum Geology 2005, this issue, doi:10.1016/j.marpetgeo.2004.10.014.
7. Forsberg C.F., Locat J. Mineralogical and microstructural development of sediments on the Mid-Norwegian margin. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.12.002.
8. Gauer P. Numerical modelling of blowing and drifting snow in Alpine terrain. Journal of Glaciology 2001, 47(156):97-110.
9. Haflidason H., Lien R., Sejrup H.P., Forsberg C.F., Bryn P. The dating and morphometry of the Storegga Slide. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.10.008.
10. Hermann F., Issler D., Keller S. Towards a Numerical Model of Powder Snow Avalanches, ECCOMACS 94 1994, 948-955. Wiley, New York.
11. Kvalstad T.J., Nadim F., Kaynia A.M., Mokkelbost K.H., Bryn P. Soil conditions and slope stability in the Ormen Lange. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.10.021.
12. Kvalstad T.J., Andresen L., Forsberg C.F., Berg K., Bryn P., Wangen M. The Storegga Slide: evaluation of triggering sources and slide mechanics. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.10.019.
13. Locat J., Demers D. Viscosity, yield stress, remoulded strength, and liquidity index relationships for sensitive. Canadian Geotechnical Journal 1988, 25:799-806.
14. Locat J., Lee H.J. Submarine landslides: advances and challenges. Canadian Geotechnical Journal 2002, 39:193-212.
15. Løvholt F., Harbitz C.B., Haugen K.B. A parametric study of tsunamis generated by submarine slides in the Ormen Lange/Storegga area of western Norway. Marine and Petroleum Geology 2005, this issue, doi:10.1016/j.marpetgeo.2004.10.019.
16. NGI, 2001. Ormen Lange site investigation 2000, Geotechnical and Geological report, NGI report no. 20001147-2, 20 August 2001.
17. NGI, 2002. Ormen Lange slope stability assessment. Task 4: In situ conditions, NGI report No. 993016-5, 29 April 2002.
18. Norem H., Locat J., Schieldrop B. An approach to the physics and modelling of submarine flow slides. Marine Geotechnology 1990, 9:93-111.
19. Rodi W. Turbulence Models and their Application in Hydraulics-A State of the Art Review 1980, IAHR Book Publication, Delft, The Netherlands.
20. Strout J.M., Tjelta T.I. In situ pore pressures: what is their significance and how can they be reliably measured. Marine and Petroleum Geology 2005, this issue, doi: 10.1016/j.marpetgeo.2004.10.024.