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The tectonic phases were mostly extensional in nature, and the pre-drift extension across the M\u00f8re and V\u00f8ring basins since mid-Permian time has been estimated to be of the order of 200\u2013250\u2005km. The pre-Cretaceous basin configuration is poorly constrained due to limited seismic resolution at great depths and a lack of borehole control. A fundamental change occurred in the crustal deformation regime: from Late Jurassic distributed stretching of the upper crust to Early Cretaceous thinning at lower-crustal levels located along the axis of the M\u00f8re and V\u00f8ring basins. A westward migration of Late Cretaceous\u2013Paleocene depocentres in the V\u00f8ring Basin reflects the focus of deformation towards the time and line of break-up. The basin architecture and evolution are summarized in relation to tectono-sedimentary elements corresponding to the main tectonic and depositional phases, and represent characteristic megasequences in the seismic data. 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