Abstract
Postrift domal uplift patterns are a distinct feauture of northern North Atlantic
margins. On the basis of apatite fission-track data, offshore seismic stratigraphy,
geomorphology, gravity and seismic tomography, we argue that southern Norway is
characterized by predominantly Neogene domal uplift. Currently available data suggest similar processes for other uplifted regions
such as Spitsbergen, northern
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