Abstract
In sandstones of the Intra-Carpathian Paleogene in central areas of the Inner West Carpathians (the Liptov depression) the magnetic fabric is essentially sedimentary in origin. Towards the margin of the West Carpathians (the Skorus̆inské vrchy Hills) the magnetic fabric indicates an influence of deformation on the sedimentary magnetic fabric. The effect of deformation is very strong at the very margin (the Zázrivá depression). This is interpreted as the effect of closure of the basins of the neighbouring klippen and flysch belts; the post-Paleogene deformation associated with the closing probably propagated into the Inner Carpathians.
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