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Main structural elements of the South Viking Graben and its flanks. The extent of the thick Middle-Upper Jurassic graben fill is defined by the limits of the KCF-Draupne Formation. Unshaded areas on the Fladen Ground Spur and Utsira High have pre-Upper...
Main structural elements of the South Viking Graben and its flanks. The extent of the thick Middle-Upper Jurassic graben fill is defined by the limits of the KCF-Draupne Formation. Unshaded areas on the Fladen Ground Spur and Utsira High have pre-Upper Jurassic rocks beneath Cenozoic or Cretaceous strata (with very thin, <approximately 2 m [6.6 ft], KCF-Draupne Formation in a few wells). The locations of Upper Jurassic oil and gas condensate fields within the graben are shown with solid fill. Fields with Cenozoic reservoirs are shown with black outlines; fields and discoveries with Middle Jurassic and older reservoirs are shown with orange outlines. Most faults shown are derived from mapping by some of the [[South Viking Graben|current authors]], but a few in the southeast portion of the map are from [[South Viking Graben|Zanella et al. (2003)]]. Bi = Birch; Br = Braemar; CB = Central Brae; D = Devenick; EB = East Brae; G = Gudrun; JS = John Sverdrup; K = Kingfisher; L = Larch; M = Miller; NB = North Brae; SB = South Brae; S = Sycamore; Th = Thelma; Ti = Tiffany; To = Toni. From AAPG Memoir 115—Rift-Related Coarse-Grained Submarine Fan Reservoirs: The Brae Play, South Viking Graben, North Sea, [http://store.aapg.org/detail.aspx?id=1301 Chapter 2].