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- W2183636769 abstract "dominantly NE-SW to E-W trending dykes, post-dates the N-MORB and lAT, and suggests formation in a fore-are setting. The occurrence of a few MORB-type dykes cutting boninite dykes may indicate formation of new oceanie erust, possibly associated with are splitting. The rare occurrence of post-MORB cale-alkaline magmatic aetivity may indicate a maturing stage of are magmatie activity." @default.
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- W2183636769 date "1994-01-01" @default.
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- W2183636769 title "The geochemical evolution of the Gulfjellet Ophiolite Complex, west Norwegian Caledonides" @default.
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