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- W2010052913 abstract "Synopsis Lamprophyre dykes intruding Gala Group (Upper Llandovery) metagreywackes in the Central Belt of the Southern Uplands commonly contain a few xenoliths, usually of quartzite or vein quartz. However, on the coast south of Glenluce, one dyke contains a suite of incognate xenoliths of foliated and non-foliated meta-igneous rocks in addition to quartz, meta-greywacke and cognate xenoliths. These incognate xenoliths may represent samples either of the basement underlying the Southern Uplands or dioritic/tonalitic intrusions emplaced at depth into the sedimentary cover." @default.
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- W2010052913 date "1999-06-01" @default.
- W2010052913 modified "2023-09-23" @default.
- W2010052913 title "Xenoliths of Southern Uplands ‘basement?’ in a lamprophyre dyke, Central Belt, Glenluce, SW Scotland" @default.
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- W2010052913 doi "https://doi.org/10.1144/sjg35010057" @default.
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