This article reviews the geology of the Sveconorwegian orogen in south Scandinavia and
existing tectonic models for the Mesoproterozoic to Neoproterozoic Sveconorwegian …

Abstract Interpretations of the pre-Caledonian rifted margin of Baltica commonly reconstruct
it as a simple, tapering, wedge-shaped continental margin dissected by half graben, with …

Smeaheia, a prominent fault block located on the Horda Platform, northern North Sea is
identified as a potential subsurface CO 2 storage site. We utilise the GN1101 3D seismic …

The evolution of Fennoscandia following the early Devonian collapse of the Caledonian
mountains is a matter of debate, due largely to the scarcity of post-Caledonian cover rocks …

The origin of the Norwegian mountains (the Scandes) is a key controversy in modern
geoscience. Are they remnants from the Caledonian Orogeny, modified shoulders of late …

Three‐dimensional surface visualization models derived from high‐resolution LiDAR data
provide new information about the type and scale of erosional processes below Late …

The Earth's cratons are traditionally regarded as tectonically stable cores that were
episodically buried by thin sedimentary covers. Cratonic crust in southern Finland holds …

Abstract The Mesoproterozoic (Jotnian) Dala Sandstone, western Sweden, is investigated
using zircon U-Pb SIMS. The Dala Sandstone was deposited in a gentle sag basin and …

Caledonian collision of continents Laurentia and Baltica, with at least 1000 km of lateral
shortening, dominates the bedrock along the northern margins of the North Atlantic Ocean …

Lower Cambrian shallow marine quartz arenite records a transgressive regime related to a
global basal Cambrian eustatic sea-level rise. Six sections from southern Norway, southern …