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 …

Abstract The Reykjanes Ridge is a key setting to study plate boundary processes overlaid
on a regional mantle melting anomaly. The ridge originated as one arm of a ridge-ridge …

An overview of the distribution of volcanic facies units was compiled over the North Atlantic
region. The new maps establish the pattern of volcanism associated with breakup and the …

Mantle convection is the principal mechanism by which heat is transferred from the deep
Earth to the surface. Cold subducting slabs sink into the mantle and steadily warm, whilst …

Injection of CO 2 into basaltic formations provides significant benefits including permanent
storage by mineralisation and large storage volume. The largest geological storage potential …

Modelled primary magma compositions of Palaeogene basalts from the North Atlantic
Igneous Province (NAIP) require melting at mantle potential temperatures (TP) in the range …

Seismic refraction data and results from receiver functions were used to compile the depth to
the basement and Moho in the NE Atlantic Ocean. For interpolation between the unevenly …

Modeled primary magma compositions for flood basalts from the Central Atlantic magmatic
province and the Ferrar large igneous province (Antarctica) require mantle potential …

Hotspot tracks are thought to originate when mantle plumes impinge moving plates.
However, many observed cases close to mid‐ocean ridges do not form a single age …

Results of a 3D modeling study inspired by recent seismic tomography of the Northern
Atlantic mantle suggest that a complex pattern of hot mantle distribution with long horizontal …