Proposal for a terrane-based nomenclature for the Lewisian Gneiss Complex of NW Scotland
MetadataShow full item record
Copyright 2005 The Geological Society of London
The current nomenclature for the Lewisian Gneiss Complex has evolved from lithological and structural correlations made prior to any dating. Initial (flawed) geochronological studies gave some names an apparent chronological standing but, as work advanced, fitting events into a coherent regional framework became increasingly difficult. Modern dating studies have shown that the Lewisian Gneiss Complex was progressively assembled from disparate blocks of Archaean continental crust and juvenile Proterozoic arcs, which satisfy the definition of terranes. Each terrane had its own separate accretionary and metamorphic history followed by a common history once juxtaposed against other terranes. Based on a new compilation of modern geochronology allied to the many detailed structural and metamorphic studies, this paper proposes a new systematic terminology for the Lewisian Gneiss Complex that is more applicable to this new tectonic framework.
Showing items related by title, author, creator and subject.
Goodenough, K.; Park, R.; Krabbendam, M.; Myers, J.; Wheeler, J.; Loughlin, S.; Crowley, Q.; Friend, C.; Beach, A.; Kinny, Peter; Graham, R. (2010)The Lewisian Gneiss Complex of northwestern Scotland consists of Archaean gneisses, variably reworked during the Proterozoic. It can be divided into three districts – a central granulitefacies district between districts ...
U-Pb zircon dating of basement inliers within the Moine Supergroup, Scottish Caledonides: implications of Archaean protolith ages.Friend, C.; Strachan, R.; Kinny, Peter (2008)Basement gneiss inliers within the Scottish Caledonides have been conventionally correlated with the Archaean Lewisian Gneiss Complex of the Caledonian foreland. Alternatively, the inliers could represent allochthonous ...
Subduction or sagduction? Ambiguity in constraining the origin of ultramafic–mafic bodies in the Archean crust of NW ScotlandJohnson, Tim; Brown, M.; Goodenough, K.; Clark, Christopher; Kinny, Peter; White, R. (2016)The Lewisian Complex of NW Scotland is a fragment of the North Atlantic Craton. It comprises mostly Archean tonalite–trondhjemite–granodiorite (TTG) orthogneisses that were variably metamorphosed and reworked in the late ...