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Geological Society, London, Special Publications

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Timing and style of crustal extension N of the Scottish mainland

S. R. Kirton and K. Hitchen
Geological Society, London, Special Publications, 28, 501-510, 1 January 1987, https://doi.org/10.1144/GSL.SP.1987.028.01.32
S. R. Kirton
British Geological Survey 19 Grange Terrace, Edinburgh EH9 2LF
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K. Hitchen
British Geological Survey 19 Grange Terrace, Edinburgh EH9 2LF
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Summary

The region immediately to the N of the Scottish mainland and W of Orkney and Shetland may be divided into two areas on grounds of structural style. The two areas are separated by a well-defined NE-SW-trending horst, the Solan Bank High. The northwestern area is dominated by listric normal faults downthrowing to the NW. These faults were initiated at two main stages: late, or post Permo-Triassic (but pre-middle Jurassic) and middle Jurassic. A well-defined NW-SE-trending transfer (strike-slip) fault, termed here the Judd fault, is associated with the middle Jurassic faults. The southeastern area is dominated by listric normal faults down-throwing to the SE. These faults were initially Caledonian thrusts which subsequently relaxed during the Permo-Triassic.

  • © 1987 The Geological Society

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In this volume

Geological Society, London, Special Publications: 28 (1)
Geological Society, London, Special Publications
Volume 28
1987
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Timing and style of crustal extension N of the Scottish mainland

S. R. Kirton and K. Hitchen
Geological Society, London, Special Publications, 28, 501-510, 1 January 1987, https://doi.org/10.1144/GSL.SP.1987.028.01.32
S. R. Kirton
British Geological Survey 19 Grange Terrace, Edinburgh EH9 2LF
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K. Hitchen
British Geological Survey 19 Grange Terrace, Edinburgh EH9 2LF
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Timing and style of crustal extension N of the Scottish mainland

S. R. Kirton and K. Hitchen
Geological Society, London, Special Publications, 28, 501-510, 1 January 1987, https://doi.org/10.1144/GSL.SP.1987.028.01.32
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