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• W2007332617 abstract "Recent detailed field studies in several anorthosite complexes have shown that anorthosites are frequently associated with weakness zones in the crust which may have favoured their emplacement at mid‐crust levels. Recent experimental data have shown that the parent magma compositions of various anorthosite massifs lie on thermal highs in the relevant phase diagrams at 10–13 kbar, indicating that these magmas cannot be derived by fractionation of peridotitic mantle melts but by melting of gabbronoritic sources in the lower crust at 40–50 km depths. In the Sveconorwegian Province terne boundaries have been traced in deep seismic profiles to Moho offsets or to tongues of lower crustal material underthrust to depths higher than 40 km. In Southern Norway, we suggest that a lithospheric‐scale weakness zone (the Feda transition zone?) has channelled the Rogaland anorthosites through linear delamination, asthenospheric uprise and melting of a mafic lower crustal tongue." @default.
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• W2007332617 date "1999-04-01" @default.
• W2007332617 modified "2023-10-17" @default.
• W2007332617 title "The crustal tongue melting model and the origin of massive anorthosites" @default.
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• W2007332617 doi "https://doi.org/10.1046/j.1365-3121.1999.00232.x" @default.
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