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- W2149702456 abstract "The contemporaneous extrusion of basalts in the Oslo Graben and intrusion of dolentes in northern Britain and southern Sweden at ~ 295 Ma calls for a common explanation. Two hypotheses are investigated: (1) the Graben and dykes resulted from extensional stresses associated with progressive lithosphere separation to the northwest of Europe in the late Carboniferous. (2) the dykes, and therefore the Graben, were related in some way to oblique collision of plates in the Hercynian orogeny which was developing to the south. The Oslo Graben was conceived in mid-Carboniferous times and born towards the end of the Carboniferous as the thin lithosphere failed and allowed the extrusion of basalt magma. It was then abandoned as the two collinear oceanic rifts to the west and northwest joined up, but the Graben carried on a life of its own, as the mafic magma cushion caught in the density trap beneath the crust continued to differentiate, and alkali magma pods rose buoyantly to freeze in the upper crust or extrude on the Graben floor." @default.
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- W2149702456 date "1983-05-01" @default.
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- W2149702456 title "Origin of the Oslo Graben in relation to the Hercynian-Alleghenian orogeny and lithospheric rifting in the North Atlantic" @default.
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- W2149702456 doi "https://doi.org/10.1016/0040-1951(83)90029-x" @default.
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