1887
Volume 1, Issue 3
  • ISSN: 1354-0793
  • E-ISSN:

Abstract

The Tiffany and Toni fields lie at the western margin of the South Viking Graben in the Northern North Sea in UK Block 16/17. The reservoirs are composed of coarse clastic sediments of the Upper Jurassic Brae Formation, which were deposited by turbidity currents and debris flows in a submarine fan setting. The Brae Formation accumulated adjacent to the graben margin fault scarp and abuts pre-Jurassic rocks of the Fladen Ground Spur to the west. The Kimmeridge Clay Formation provides both the source of hydrocarbons and the seal for the reservoir.

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/content/journals/10.1144/petgeo.1.3.279
1995-08-01
2024-04-28
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  • Article Type: Other

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