Stress orientation, pore pressure and least principal stress in the Norwegian sector of the North Sea

We have compiled data on stress orientation, pore pressure and least principal stress from over 300 wells in the Norwegian sector of the North Sea. Well-defined regional variations are observed in all three parameters. Incorporation of precise stress orientation data from drilling-induced tensile borehole wall fractures shows that the orientation of maximum horizontal stress is approximately E–W between 60°N and 62°N but tends to be NNW–SSE south of 58°N, similar to the average stress direction seen throughout Great Britain and continental NW Europe. We believe this rotation is due to the superposition of plate-driving stresses with those associated with lithospheric flexure caused by deglaciation. Regional variations of the magnitude of the least principal stress and pore pressure also appear to support the hypothesis that the stress field in this region has been strongly affected by deglaciation.

[1]  Roger Hansen,et al.  Seismicity and seismotectonics of Norway and nearby continental shelf areas , 1991 .

[2]  L. Gaarenstroom,et al.  Overpressures in the Central North Sea: implications for trap integrity and drilling safety , 1993 .

[3]  O. T. Jones,et al.  The Dynamics of Faulting and Dyke Formation: with Applications to Britain , 1942, Nature.

[4]  S. Stein,et al.  Passive Margin Earthquakes, Stresses and Rheology , 1989 .

[5]  H. Bungum,et al.  Crustal stress and tectonics in Norwegian regions determined from earthquake focal mechanisms , 2000, Geological Society, London, Special Publications.

[6]  Larry G. Mastin,et al.  Regional patterns of tectonic stress in Europe , 1992 .

[7]  E. V. Artyushkov Stresses in the lithosphere caused by crustal thickness inhomogeneities , 1973 .

[8]  Daniel Moos,et al.  Utilization of observations of well bore failure to constrain the orientation and magnitude of crustal stresses: Application to continental, Deep Sea Drilling Project, and Ocean Drilling Program boreholes , 1990 .

[9]  T. Engelder,et al.  Influence of poroelastic behavior on the magnitude of minimum horizontal stress, Sh in overpressured parts of sedimentary basins , 1994 .

[10]  M. Brudy,et al.  Orientation of crustal stresses in the North Sea and Barents Sea inferred from borehole breakouts , 1996 .

[11]  M. Zoback,et al.  High Horizontal Stress in the Visund Field, Norwegian North Sea: Consequences For Borehole Stability and Sand Production , 1998 .

[12]  A. Doré The Base Tertiary Surface of southern Norway and the northern North Sea , 1992 .

[13]  M. Ekman,et al.  Recent postglacial rebound, gravity change and mantle flow in Fennoscandia , 1996 .

[14]  M. Zoback,et al.  Fluid flow along potentially active faults in crystalline rock: Geology , 1995 .

[15]  M. Zoback First‐ and second‐order patterns of stress in the lithosphere: The World Stress Map Project , 1992 .