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- W3120490592 abstract "Abstract Mafic dykes, related to the Central Scandinavian Dolerite Group, changed their geometry during the Caledonian orogeny from flat-lying bodies in the Autochthon to steeply inclined in the thrusted and stacked Lower Allochthon units. During tectonic transport a remagnetisation occured and the post-Jotnian paleomagnetic signature was completely obliterated. In the Bangonaive window this remagnetisation occurred at a deeper crustal level probably during metamorphism and deformation under amphibolite-facies conditions, while in the Borgefjell window it was caused by alteration in a more shallow crustal level. In both tectonic windows the remanence direction is influenced by the structure, and in the strongly anisotropic samples of the Bangonainve window a distinct refraction of the remanence direction (up to 15°) towards the magnetic lineation is observed." @default.
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- W3120490592 date "2000-01-01" @default.
- W3120490592 modified "2023-09-26" @default.
- W3120490592 title "Remagnetisation and magnetic refraction in Proterozoic dykes from central Scandinavia during Caledonian deformation" @default.
- W3120490592 hasPublicationYear "2000" @default.
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