In this study we compare three pairs of conjugate rifted margins that are often referred to as
archetypes of rift systems. Despite numerous differences, a remarkable first-order structural …

Accurate spatial models of tectonic plates and geological terranes are important for
analyzing and interpreting a wide variety of geoscientific data and developing compositional …

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 …

Passive‐margin salt basins are classified as prerift, syn‐stretching, syn‐thinning, and syn‐
exhumation. Prerift salt, such as the Triassic Keuper in the Western Pyrenees, undergoes …

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

An updated magnetic anomaly grid of the NE Atlantic and an improved database of
magnetic anomaly and fracture zone identifications allow the kinematic history of this region …

The idea of a simple linear boundary between continental and oceanic crust at extended
continental margins is widely recognized to be an oversimplification. Despite this, such …

The fossil rift in the North Pyrenean Zone, which underwent high temperature‐low pressure
metamorphism and alkaline magmatism during Early Cretaceous hyperextension, was …

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 …

This study describes the distribution and stratigraphic range of the Upper Palaeozoic–
Mesozoic succession in the NE Atlantic region, and is correlated between conjugate …