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The Faroe–Shetland Basin and adjacent areas

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Published:
January 01, 2016

Abstract

The Faroe-Shetland Basin (FSB) is a narrow but deep-rifted structure, trending NE-SW, with its orientation controlled by Caledonian basement thrusts. It lies between the Precambrian and Paleozoic Caledonian basement of the West Shetland Platform (part of the Orkney-Shetland Platform) and the Faroe Platform. It corresponds approximately to the topographical deep-water Faroe-Shetland Channel. It is bounded to the SW by the Sula Sgeir High and the Wyville-Thomson Ridge. The western margin lies under the flood basalts of the Faroe Platform and is imperfectly delimited. The NE margin is formed by the Erlend Central Complex (forming the Erlend Platform) (Figs 171 & 176).

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Geological Society, London, Special Reports

A revised correlation of Tertiary rocks in the British Isles and adjacent areas of NW Europe

C. King
C. King
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A. S. Gale
A. S. Gale
School of Earth & Environmental Sciences, University of Portsmouth, Burnaby Building, Burnaby Road, Portsmouth PO1 3QL, UK
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T. L. Barry
T. L. Barry
Department of Geology, University of Leicester, University Road, Leicester LE1 7RH, UK
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Geological Society of London
Volume
27
ISBN electronic:
9781862397071
Publication date:
January 01, 2016

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