Abstract The North Atlantic, extending from the Charlie Gibbs Fracture Zone to the north
Norway-Greenland-Svalbard margins, is regarded as both a classic case of structural …

The breakup of Pangaea was accompanied by extensive, episodic, magmatic activity.
Several Large Igneous Provinces (LIPs) formed, such as the Central Atlantic Magmatic …

Abstract The Norwegian-Greenland Sea (NGS) in the NE Atlantic comprises diverse tectonic
regimes and structural features including sub-oceanic basins of different ages …

The breakup of Laurasia to form the Northeast Atlantic Realm disintegrated an
inhomogeneous collage of cratons sutured by cross-cutting orogens. Volcanic rifted margins …

The Møre and Vøring basins of the mid-Norwegian volcanic passive margin are
characterized by thick accumulations of Cretaceous to Paleocene sedimentary strata. They …

The formation of the NE Atlantic conjugate margins is the result of multiple rifting phases
spanning from the Late Paleozoic and culminating in the early Eocene when breakup was …

The mechanisms responsible for the formation of extremely thinned continental crust (< 10
km thick) and lithosphere during rifting remains debated. Observations from present-day and …

Passive margins are the locus of tectonic and magmatic processes leading to the formation
of highly variable along-strike and conjugate margins structures. Using extensive new …

The NE Atlantic volcanic rifted margins include vast underexplored basin areas
neighbouring mature petroleum-producing regions. We appraise the cross-border …

During the terminal stages of Wilson cycles, remnants of magma‐poor margins may be
incorporated into the orogens, whereas the magma‐rich margins often are lost in subduction …