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- W1982542334 abstract "Abstract The dense tholeiitic Koster dyke swarm, west Sweden, has undergone progressive deformation under amphibolite facies metamorphic conditions. The varying influence of this event on the dyke rock forms the basis for a regional division of the swarm into three sectors: the sectors of igneous dolerites, partly recrystallised metadolerites, and lineated amphibolites, respectively. Systematic measurements of the magnetic susceptibility in the dykes have demonstrated a correlation between the regional pattern of recrystallisation and the pattern of mean susceptibility given as mean susceptibility per 0.5 km2. The transformation of dolerites to metadolerites and finally to lineated amphibolites is accompanied by a marked decrease in the susceptibility, which is related essentially to the degree of alteration of titanomagnetite to sphene + Fe-ions incorporated in the silicates." @default.
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- W1982542334 date "1984-10-01" @default.
- W1982542334 modified "2023-09-26" @default.
- W1982542334 title "Magnetic susceptibility used in mapping of amphibolite facies recrystallisation in basic dykes" @default.
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- W1982542334 doi "https://doi.org/10.1016/0040-1951(84)90243-9" @default.
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