By James G. Buchanan, Peter G. Buchanan
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Tectonophysics, 173,163-174. WATSON, J. 1985. Northern Scotland as an AtlanticNorth Sea divide. Journal of the Geological Society, London, 142,221-243. WHITE, R. S. 1992. Crustal structure and magmatism of North Atlantic continental margins. Journal of the Geological Society, London, 149,841-854. & MCKENZtE, D. 1989. Magmatism at rift zones: The generation of volcanic continental margins and flood basalts. Journal of Geophysical Research, 94, 7685-7729. --, SPENCE, G. , FOWLER, S. , MCKENZlE, D.
Flood basalts are associated with some of these centres but are more widely distributed in the Rockall Trough, Antrim (Northern Ireland) and in the vicinity of the Faeroe Islands. Minor intrusive bodies and dyke swarms are common both onshore and offshore, as far south as Lundy Island in the Bristol Channel (Thorpe et al. 1990), as far east as the western margin of the North Sea basin, and as far west as the Porcupine basin (Tate & Dobson 1988). Further northwest, along the continental margin, the results of wide-angle seismic experiments have indicated the presence of substantial volumes of underplated igneous rock (up to 15 km in thickness) within the lower crust of the Hatton-Rockall margin and the Veering Plateau (Hinz et al.
Basin inversion by James G. Buchanan, Peter G. Buchanan