1887
Volume 26, Issue 4
  • E-ISSN: 1365-2117

Abstract

Abstract

The impact of a pre‐existing rift fabric on normal fault array evolution during a subsequent phase of lithospheric extension is investigated using 2‐D and 3‐D seismic reflection, and borehole data from the northern Horda Platform, Norwegian North Sea. Two fault populations are developed: (i) a population comprising relatively tall (>2 km), N‐S‐striking faults, which have >1.5 km of throw. These faults are up to 60 km long, penetrate down into crystalline basement and bound the eastern margins of 6–15 km wide half‐graben, which contain >3 km of pre‐Jurassic, likely Permo–Triassic, but possibly Devonian syn‐rift strata; and (ii) a population comprising vertically restricted (<1 km), NW‐SE‐striking faults, which are more closely spaced (0.5–5 km), have lower displacements (30–100 m) and not as long (2–10 km) as those in the N–S‐striking population. The NW‐SE‐striking population typically occurs between the N‐S‐striking population, and may terminate against or cross‐cut the larger structures. NW–SE‐striking faults do not bound pre‐Jurassic half‐graben and are largely restricted to the Jurassic‐to‐Cretaceous succession. Seismic‐stratigraphic observations, and the stratigraphic position of the fault tips in both fault populations, allow us to reconstruct the Late Jurassic‐to‐Early Cretaceous growth history of the northern Horda Platform fault array. We suggest the large, N‐S‐striking population was active during the Permo–Triassic and possibly earlier (Devonian?), before becoming inactive and buried during the Early and Middle Jurassic. After a period of relative tectonic quiescence, the N‐S‐striking, pre‐Jurassic fault population propagated through the Early‐Middle Jurassic cover and individual fault systems rapidly (within <10 Ma) established their maximum length in response to Late Jurassic extension. These fault systems became the dominant structures in the newly formed fault array and defined the locations of the main, Late Jurassic‐to‐Early Cretaceous, syn‐rift depocentres. Late Jurassic extension was also accommodated by broadly synchronous growth of the NW‐SE‐striking fault population; the eventual death of this population occurred in response to the localization of strain onto the N–S‐striking fault population. Our study demonstrates that the inheritance of a pre‐existing rift fabric can influence the geometry and growth of individual fault systems and the fault array as a whole. On the basis of observations made in this study, we present a conceptual model that highlights the influence of a pre‐existing rift fabric on fault array evolution in polyphase rifts.

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References

  1. Bartholomew, I.D., Peters, J.M. & Powell, C.M. (1993) Regional structural evolution of the North Sea: oblique slip and the reactivation of basement lineaments. In: Petroleum Geology of Northwest Europe: Proceedings of the 4th Conference (Ed. by R.J.Parker ), pp. 1109–1122. Geological Society, London.
    [Google Scholar]
  2. Bellahsen, N. & Daniel, J.M. (2005) Fault reactivation control on normal fault growth: an experimental study. J. Struct. Geol., 27, 769–780.
    [Google Scholar]
  3. Bonini, M., Souriot, T., Boccaletti, M. & Brun, J.P. (1997) Successive orthogonal and oblique extensional episodes in a rift zone: laboratory experiments with application to the Ethiopian Rift. Tectonics, 16, 347–362.
    [Google Scholar]
  4. Brun, J.P. & Tron, V. (1993) Development of the North Viking Graben: inferences from laboratory modelling. Sed. Geol., 86, 31–51.
    [Google Scholar]
  5. Buck, R.W. (1991) Modes of continental lithospheric extension. J. Geophys. Res., 96, 20161–20178.
    [Google Scholar]
  6. Byerlee, J. (1978) Friction of rocks. Pure Appl. Geophys., 116, 615–626.
    [Google Scholar]
  7. Cartwright, J.A., Trudgill, B.D. & Mansfield, C.S. (1995) Fault growth by segment linkage: an explanation for scatter in maximum displacement and trace length data from the Canyon lands grabens of SE Utah. J. Struct. Geol., 17, 1319–1326.
    [Google Scholar]
  8. Contreas, J., Anders, M.H. & Scholz, C.H. (2000) Growth of a normal fault system: observations from the Lake Malawi basin of the East African rift. J. Struct. Geol., 22, 159–168.
    [Google Scholar]
  9. Cowie, P.A. (1998) A healing–reloading feedback control on the growth rate of seismogenic faults. J. Struct. Geol., 20, 1075–1087.
    [Google Scholar]
  10. Cowie, P.A. & Scholz, C.H. (1992a) Displacement‐length scaling relationships for faults: data synthesis and discussion. J. Struct. Geol., 14, 1149–1156.
    [Google Scholar]
  11. Cowie, P.A. & Scholz, C.H. (1992b) Physical explanation for the displacement‐length relationship of faults using a post‐yield fracture mechanics model. J. Struct. Geol., 14, 1133–1148.
    [Google Scholar]
  12. Cowie, P.A., Gupta, S. & Dawers, S. (2000) Implications of fault array evolution on syn‐rift depocentre development: insights from a numerical fault growth model. Basin Res., 12, 241–261.
    [Google Scholar]
  13. Cowie, P.A., Underhill, J.R., Behn, M.D., Lin, J. & Gill, C. (2005) Spatio‐temporal evolution of strain accumulation derived from multi‐scale observations of Late Jurassic rifting in the northern North Sea: a critical evaluation of models of lithospheric extension. Earth Planet. Sci. Lett., 234, 401–419.
    [Google Scholar]
  14. Cowie, P.A., Roberts, G.P. & Mortimer, E. (2007) Strain localisation with fault arrays over timescales of 100‐107 years – observations, explanations, debates. In: Tectonic Faults: Agents of Change on a Dynamic Earth (Ed. by M.R Handy , G.Hirth , G. & N.Hovius ). Dahlem Workshop Report 95, pp. 48–77. MIT Press: Cambridge MA.
    [Google Scholar]
  15. Dawers, N.H. & Anders, M.H. (1995) Displacement‐length scaling and fault linkage. J. Struct. Geol., 17, 607–614.
    [Google Scholar]
  16. Dawers, N.H. & Underhill, J.R. (2000) The role of fault interaction and linkage in controlling syn‐rift stratigraphic sequences: Statfjord East area, northern North Sea. Am. Assoc. Petr. Geol. Bull., 84, 45–64.
    [Google Scholar]
  17. Doré, A.G., Lundin, E.R., Fichler, C. & Olesen, O. (1997) Patterns of basement structure and reactivation along the NE Atlantic margin. J. Geol. Soc., 154, 85–92.
    [Google Scholar]
  18. Dreyer, T., Whitaker, M., Dexter, J., Flesche, H. & Larsen, E. (2005) From spit system to tide‐dominated delta: intergrated reservoir model for the upper Jurassic Sognefjord Formation on the Troll West Field. In: Petroleum Geology: North‐West Europe and Global Perspectives – Proceedings of the 6th Petroleum Geology Conference (Ed. by A.G.Doré & B.A.Vining ), pp. 423–448. Geological Society, London
    [Google Scholar]
  19. Færseth, R.B. (1996) Interaction of Permo–Triassic and Jurassic extensional fault‐blocks during development of the North Sea. J. Geol. Soc., 153, 931–944.
    [Google Scholar]
  20. Færseth, R.B. & Ravnås, R. (1998) Evolution of the Oseberg fault‐block in the context of the northern North Sea structural framework. Mar. Petrol. Geol., 15, 467–490.
    [Google Scholar]
  21. Færseth, R.B., Gabrielsen, R.H. & Hurich, C.A. (1995) Influence of basement in structuring of the North Sea basin, offshore southwest Norway. Nor. Geol. Tidsskr., 75, 105–119.
    [Google Scholar]
  22. Færseth, R.B., Knudsen, B.E., Liljedahl, T., Midboe, P.S. & Soderstrom, B. (1997) Oblique rifting and sequential faulting in the Jurassic development of the northern North Sea. J. Struct. Geol., 19, 1285–1302.
    [Google Scholar]
  23. Frankowicz, E. & McClay, K.R. (2010) Extensional fault segmentation and linkages, Bonaparte Basin, outer North West Shelf Australia. AAPG Bull., 94, 977–1010.
    [Google Scholar]
  24. Gabrielsen, R.H., Færseth, R., Steel, R.J., Idil, S. & Kløvjan, O.S. (1990) Architectural styles of basin fill in the northern Viking Graben. In: Tectonic evolution of the North Sea Rifts (Ed. by D.J.Blundell & A.D.Gibbs ), pp. 158–179. Clarendon, Oxford.
    [Google Scholar]
  25. Gabrielsen, R.H., Kyrkebø, R., Faleide, J.I., Fjeldskaar, W. & Kjennerud, T. (2001) The Cretaceous post‐rift configuration of the northern North Sea. Petrol. Geosci., 7, 137–154.
    [Google Scholar]
  26. Gawthorpe, R.L. & Leeder, M.R. (2000) Tectono‐sedimentary evolution of active extensional basins. Basin Res., 12, 195–218.
    [Google Scholar]
  27. Gawthorpe, R.L., Sharp, I.R., Underhill, J.R. & Gupta, S. (1997) Linked sequence stratigraphic and structural evolution of propagating normal faults. Geology, 25, 795–798.
    [Google Scholar]
  28. Gawthorpe, R.L., Jackson, C.A.L., Young, M.J., Sharp, I.R., Moustafa, A.R. & Leppard, C.W. (2003) Normal Fault Growth, displacement localisation and the evolution of normal fault populations: the Hamman Faraun fault block, Suez rift, Egypt. J. Struct. Geol., 25, 883–895.
    [Google Scholar]
  29. Giba, M., Walsh, J.J. & Nicol, A. (2012) Segmentation and growth of an obliquely reactivated normal fault. J. Struct. Geol., 39, 253–267.
    [Google Scholar]
  30. Glennie, K.W. (1987) Outline of North Sea History and structural framework. In: Introduction to the Petroleum Geology of the North Sea. 3rd edn (Ed. by K.W.Glennie ), pp. 34–77. Blackwell Scientific Publications, Oxford.
    [Google Scholar]
  31. Gupta, S., Cowie, P.A., Dawers, N.H. & Underhill, J.R. (1998) A mechanism to explain rift‐basin subsidence and stratigraphic patterns through fault‐array evolution. Geology, 26, 595–598.
    [Google Scholar]
  32. Gupta, A. & Scholz, C.H. (2000) A model of normal fault interaction based on observations and theory. J. Struct. Geol., 22, 865–879.
    [Google Scholar]
  33. Gradstein, F., Ogg, J. & Smith, A. (2004) A Geologic Time Scale, pp. 610. Cambridge University Press, Cambridge, UK.
    [Google Scholar]
  34. Helland‐Hansen, W., Ashton, M., Lomo, L. & Steel, R. (1992) Advance and retreat of the Brent Delta; recent contributions to the depositional model. In: Geology of the Brent Group (Ed. by A.C.Morton , R.S.Haszeldine & M.R.Giles ), Geol. Soc. Spec. Publ., 61, 109–127.
    [Google Scholar]
  35. Henza, A.A., Withjack, M.O. & Schlische, R.W. (2010) Normal‐fault development during two‐phase non‐coaxial extension: an experimental study. J. Struct. Geol., 32, 1656–1667.
    [Google Scholar]
  36. Holdsworth, R.E., Butler, C.A. & Roberts, A.M. (1997) The recognition of reactivation during continental deformation. J. Geol. Soc., 154, 73–78.
    [Google Scholar]
  37. Hospers, J., Finnstrøm, E.G. & Rathore, J.S. (1985) A regional gravity study of the northern North Sea. Geophys. Prospect., 33, 543–566.
    [Google Scholar]
  38. Jackson, C.A.L. & Rotevatn, A. (2013) 3D seismic analysis of the structure and evolution of a salt‐influenced normal fault zone: a test of competing fault growth models. J. Struct. Geol., 54, 215–234.
    [Google Scholar]
  39. Jackson, C.A.‐L., Gawthorpe, R.L. & Sharp, I.R. (2002) Growth and linkage of the East Tanka fault zone, Suez rift: structural style and syn‐rift stratigraphic response. J. Geol. Soc., 159, 175–187.
    [Google Scholar]
  40. Keep, M. & McClay, K.R. (1997) Analogue Modelling of multiphase rift systems. Tectonophysics, 273, 239–270.
    [Google Scholar]
  41. Korme, T., Acocella, V. & Abebe, B. (2004) The role of pre‐existing structures in the Origin, Propagation and Architecture of faults in the main Ethiopian Rift. Gondwana Res., 7, 467–479.
    [Google Scholar]
  42. Lepercq, J.Y. & Gaulier, J.M. (1996) Two‐stage rifting in the North Viking Graben area (North Sea): inferences from a new three‐dimensional subsidence analysis. Mar. Petrol. Geol., 13, 129–148.
    [Google Scholar]
  43. Madritsch, H., Kounov, A., Schmid, S.M. & Fabbri, O. (2009) Multiple fault reactivations within the intra‐continental Rhine‐Bresse Transfer Zone (La Serre Horst, eastern France). Tectonophyscis, 471, 297–318.
    [Google Scholar]
  44. Maerten, L., Gillespie, P. & Pollard, D.D. (2002) Effects of local stress perturbation on secondary fault development. J. Struct. Geol., 24, 145–153.
    [Google Scholar]
  45. McLeod, A.E., Dawers, N.H. & Underhill, J.R. (2000) The propagation and linkage of normal faults: insights from the Strathspey‐Brent–Statfjord fault array, northern North Sea. In: Processes and Controls in the Stratigraphic Development of Extensional Basins (Ed. by S.Gupta & P.A.Cowie ) Basin Res., 12, 263–284.
    [Google Scholar]
  46. Meyer, V., Nicol, A., Childs, C., Walsh, J.J. & Watterson, J. (2002) Progressive localisation of strain during the evolution of a normal fault population. J. Struct. Geol., 24, 1215–1231.
    [Google Scholar]
  47. Michon, L. & Sokoutis, D. (2005) Interaction between structural inheritance and extension direction during graben and depocentre formation: an experimental approach. Tectonophysics, 409, 125–146.
    [Google Scholar]
  48. Morley, C.K., Harayana, C., Phoosonsee, W., Pongwapee, S., Kornsawan, A. & Wonganan, N. (2004) Activation of rift oblique and rift‐parallel pre‐existing fabrics during extension and their effect on deformation style: examples from the rifts of Thailand. J. Struct. Geol., 26, 1803–1829.
    [Google Scholar]
  49. Morley, C.K., Gabdi, S. & Seusurrhiya, K. (2007) Fault superimposition and linkage resulting from stress changes during rifting: examples from 3D seismic data, Phitsanulok Basin, Thailand. J. Struct. Geol., 29, 646–663.
    [Google Scholar]
  50. Nøttvedt, A., Gabrielsen, R.H. & Steel, R.J. (1995) Tectonostratigraphy and sedimentary architecture of rift basins, with reference to the northern North Sea. Mar. Petrol. Geol., 12, 881–901.
    [Google Scholar]
  51. Odinsen, T., Christiansson, P., Gabrielsen, R.H., Faleide, J.I. & Berge, A.M. (2000) The geometries and deep structure of the northern North Sea rift system. In: Dynamics of the Norwegian Margin (Ed. by A.Nottvedt ) Geol. Soc. London Spec. Publ., 167, 41–57.
    [Google Scholar]
  52. Paton, D.A. (2006) Influence of crustal heterogeneity on normal fault dimensions and evolution: southern South Africa extensional system. J. Struct. Geol., 28, 868–886.
    [Google Scholar]
  53. Paton, D.A. & Underhill, J.R. (2004) Role of crustal anisotropy in modifying the structural and sedimentological evolution of extensional basins: the Gamtoos Basin, South Africa. Basin Res., 16, 339–359.
    [Google Scholar]
  54. Peacock, D.C.P. & Sanderson, D.J. (1991) Displacements, segment linkage and relay ramps in normal fault zones. J. Struct. Geol., 13, 721–733.
    [Google Scholar]
  55. Pickering, G., Peacock, D.C.P., Sanderson, D.J. & Bull, J.M. (1997) Modelling tip zones to predict the throw and length characteristics of faults. AAPG Bull., 81, 82–99.
    [Google Scholar]
  56. Rattey, R.P. & Hayward, A.B. (1993) Sequence stratigraphy of a failed rift system: the Middle Jurassic to Early Cretaceous basin evolution of the Central and Northern North Sea. In: Petroleum Geology of Northwest Europe, Proceedings of the 4th Conference (Ed. by J.R.Parker ), pp. 215–249. Geological Society, London
    [Google Scholar]
  57. Ravnås, R. & Bondevik, K. (1997) Architecture and controls on Bathonian‐Kimmeridgian shallow‐marine synrift wedges of the Oseberg‐Brage area, northern North Sea. Basin Res., 9, 197–226.
    [Google Scholar]
  58. Ravnås, R. & Steel, R.J. (1998) Architecture of Marine Rift‐Basin Successions. AAPG Bull., 82, 110–146.
    [Google Scholar]
  59. Ravnås, R., Nottvedt, A., Steel, R.J. & Windelstad, J. (2000) Syn‐rift sedimentary architectures in the Northern North Sea. In: Dynamics of the Norwegian Margin (Ed. by A.Nottvedt ) Geol. Soc. London Spec. Pub., 167, 133–177.
    [Google Scholar]
  60. Roberts, A.M., Yielding, G. & Badley, M.E. (1990) A kinematic model for the orthogonal opening of the late Jurassic North Sea rift system, Denmark‐Mid Norway. In: Tectonic Evolution of the North Sea Rifts (Ed. by D.J.Blundell , A.D.Gibbs ), pp. 180–199. Oxford University Press, Oxford.
    [Google Scholar]
  61. Roberts, A.M., Yielding, G., Kusznir, N.J., Walker, I. & Dorn‐Lopez, D. (1993) Mesozoic extension in the North Sea: constraints from flexural Backstripping, forward modelling and fault populations. In: Petroleum Geology of Northwest Europe, Proceedings of the 4th Conference (Ed. by J.R.Parker ), pp. 1123–1136. Geological Society, London
    [Google Scholar]
  62. Roberts, A.M., Yielding, G., Kusznir, N.J., Walker, I.M. & Dorn‐Lopez, D. (1995) Quantitative analysis of Triassic extension in the northern Viking Graben. J. Geol. Soc., 152, 15–26.
    [Google Scholar]
  63. Schlische, R.W. (1995) Geometry and origin of fault‐related folds in extensional settings. AAPG Bull., 79, 1661–1678.
    [Google Scholar]
  64. Scholz, C.H. & Contreras, J. (1998) Mechanics of continental rift architecture. Geology, 26, 967–970.
    [Google Scholar]
  65. Sibson, R.H. (1985) A note on fault reactivation. J. Struct. Geol., 7, 751–754.
    [Google Scholar]
  66. Sinclair, I.K. (1995) Transpressional inversion due to episodic rotation of extensional stress regimes in Jeanne d'Arc Basin, offshore Newfoundland. In: Basin Inversion (Ed. by J.G.Buchanan & P.G.Buchanan ) Geol. Soc. London Spec. Publ., 88, 249–271.
    [Google Scholar]
  67. Smethurst, M.A. (2000) Land‐offshore tectonic links in western Norway and the northern North Sea. J. Geol. Soc., 157, 769–781.
    [Google Scholar]
  68. Smith, M. & Mosley, P. (1993) Crustal heterogeneity and basement influence on the development of the Kenyan rift, East Africa. Tectonics, 12, 591–606.
    [Google Scholar]
  69. Steel, R. (1993) Triassic‐Jurassic megasequence stratigraphy in the Northern North Sea: Rift to post‐rift evolution. In: Petroleum Geology of Northwest Europe, Proceedings of the 4th Conference (Ed. by J.R.Parker ), pp. 299–315. Geological Society, London.
    [Google Scholar]
  70. Stewart, I.J., Rattey, R.P. & Vann, I.R. (1992) Structural style and the habit of hydrocarbons in the North Sea. In: Structural and Tectonic Modelling and its Application to Petroleum Geology (Ed. by R.M.Larsen , H.Brekke , B.T.Larsen & E.Talleraas ) NPF Spec. Publ., 1, 197–220.
    [Google Scholar]
  71. Taylor, S.K., Nicol, A. & Walsh, J.J. (2008) Displacement loss on growth faults due to sediment compaction. J. Struct. Geol., 30, 394–405.
    [Google Scholar]
  72. Tomasso, M., Underhill, J.R., Hodgkinson, R.A. & Young, M.J. (2008) Structural styles and depositional architecture in the Triassic of the Ninian and Alwyn North fields: implications for basin development and prospectivity in the Northern North Sea. Mar. Petrol. Geol., 25, 588–605.
    [Google Scholar]
  73. Underhill, J.R. & Partington, M.A. (1993) Jurassic thermal doming and deflation in the North Sea; implications of the sequence stratigraphic evidence. In: Petroleum Geology of Northwest Europe, Proceedings of the 4th Conference (Ed. by J.R.Parker ), pp. 337–345. Geological Society, London.
    [Google Scholar]
  74. Versfelt, J. & Rosendahl, B.R. (1989) Relationship between pre‐rift structure and rift architecture in Lake Tananyika and Malawi, East Africa. Nature, 337, 354–356.
    [Google Scholar]
  75. Walsh, J.J. & Watterson, J. (1988) Analysis of the relationship between displacements and the dimensions of faults. J. Struct. Geol., 10, 239–247.
    [Google Scholar]
  76. Walsh, J.J., Nicol, A. & Childs, C. (2002) An alternative model for the growth of faults. J. Struct. Geol., 24, 1669–1675.
    [Google Scholar]
  77. Withjack, M.O., Olson, J. & Peterson, E. (1990) Experimental models of extensional forced folds: America Association of Petroleum Geologists. Bulletin, 74, 1038–1054.
    [Google Scholar]
  78. Wojtal, S.F. (1996) Changes in fault displacement populations correlated to linkage between faults. J. Struct. Geol., 18, 265–279.
    [Google Scholar]
  79. Young, M.J., Gawthorpe, R.L. & Hardy, S. (2001) Growth and linkage of a segmented normal fault zone; the Late Jurassic Murchison‐Statfjord North Fault, northern North Sea. J. Struct. Geol., 23, 1933–1952.
    [Google Scholar]
  80. Young, M.J., Gawthorpe, R.L. & Sharp, I.R. (2003) Normal fault growth and early syn‐rift sedimentology and sequence stratigraphy: Thal Fault, Suez Rift, Egypt. Basin Res., 15, 479–502.
    [Google Scholar]
  81. Zervos, F. (1987) A compilation and regional interpretation of the northern North Sea gravity map. In: Continental Extension Tectonics(Ed. by M.P.Coward , J.F.Dewey & P.L.Hancock ) Geol. Soc. Spec. Publ., 28, 477–493.
    [Google Scholar]
  82. Ziegler, P.A. (1990) Tectonic and palaeogeographic development of the North Sea rift system. In: Tectonic Evolution of the North Sea Rifts (Ed. by D.J.Blundell & A.D.Gibbs ), pp. 1–36. Oxford University Press, Oxford.
    [Google Scholar]
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