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The thrust structures of southern Assynt, Moine thrust zone

Published online by Cambridge University Press:  01 May 2009

M. P. Coward
M. P. Coward
Affiliation:
Geology Department, Imperial College, Prince Consort Road, London SW7 2BP, U.K.
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Abstract

The Moine thrust zone of southern Assynt forms part of the northwest margin of the Caledonide belt and has aroused controversy concerning amounts and timing of thrust displacement and sequence of thrust development. Recent mapping shows it to have been a foreland propagating thrust sequence; the uppermost ductile Moine thrust formed first, followed by sequences of imbricates, a major thrust (the Ben More thrust) and then several lower duplex zones. This sequence is clear from new observations that many of the earlier thrusts were folded and/or breached during the development of the underlying structures. A displacement of over 54 km has been estimated for the zone as a whole. An alkaline igneous complex, including the large Borrolan syenite, was intruded during the development of the thrust zone and much of it was carried some 30 km to the west-northwest onto the foreland. Late extensional structures in southern Assynt are an integral part of the Caledonide thrust sequence and probably developed from the collapse of the thrust wedge as it climbed from stronger basement rocks on to a weaker cover sequence on the foreland.

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Articles
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Geological Magazine , Volume 122 , Issue 6 , November 1985, pp. 595 - 607
Copyright
Copyright © Cambridge University Press 1985

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