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The minor intrusions of Assynt, NW Scotland : early development of magmatism along the Caledonian Front

By K.M. Goodenough, B.N. Young and I. Parsons


The Assynt Culmination of the Moine Thrust Belt, in the northwest Scottish Highlands, contains a variety of Caledonian alkaline and calc-alkaline intrusions that are mostly of Silurian age. These include a significant but little-studied suite of dykes and sills, the Northwest Highlands Minor Intrusion Suite. We describe the structural relationships of these minor intrusions and suggest a classification into seven swarms. The majority of the minor intrusions can be shown to pre-date movement in the Moine Thrust Belt, but some appear to have been intruded during the period of thrusting. A complex history of magmatism is thus recorded within this part of the Moine Thrust Belt. New geochemical data provide evidence of a subduction-related component in the mantle source of the minor intrusions. \u

Topics: Earth Sciences
Publisher: Mineralogical Society of Great Britain and Ireland
Year: 2004
DOI identifier: 10.1180/0026461046840207
OAI identifier:

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