Studies conducted in present‐day magma‐poor rifted margins reveal that the transition from
weakly thinned continental crust (∼ 30 km) in proximal margins to hyper‐extended crust (≤ …

A prominent lower crustal high-velocity layer observed in the Vøring Basin, NE Atlantic, has
been investigated with regard to composition and spatial link to crustal-scale lineaments. In …

Eocene magmatic breakup along the mid‐Norway rifted margin was preceded by extreme
Jurassic‐Cretaceous crustal thinning in a magma‐poor environment. Along the SE borders …

The sub-basalt domain of the Norwegian continental shelf (NCS) is one of the last remaining
hydrocarbon exploration frontiers in Europe. While there is an established geological and …

In this contribution, we present a model of microcontinent architecture within a system that
involves a complex rifted margin setting and different phases of deformation and continental …

The thermal evolution of continental rifted margins is key to understanding margin
subsidence and hydrocarbon prospectivity. Observed heat-flow values, however, do not …

A model of the thermal, compositional, density, and seismological structure of the
lithospheric and sublithospheric mantle along a 500-km transect across the Namibian …

Transform marginal plateaus (TMPs) are large and flat structures commonly found in deep
oceanic domains, but their origin and relationship to adjacent oceanic lithosphere remain …

The aim of this study is to investigate the shallow thermal field differences for two differently
aged passive continental margins by analyzing regional variations in geothermal gradient …

D gravity models that consider the highly complex density structure of the Norwegian
passive volcanic continental margin require a significantly lower density in the mantle below …