A continental rift is a nascent plate boundary where the lithosphere is thinned by tectonic
activity. Some continental rifts undergo extension to the point that they generate a new …

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 …

We present an updated oceanic crustal age grid and a set of complementary grids including
spreading rate, asymmetry, direction, and obliquity. Our data set is based on a selected set …

We present GlobSed, a new global 5‐arc‐minute total sediment thickness grid for the world's
oceans and marginal seas. GlobSed covers a larger area than previously published global …

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

The evolution of the Northern Hemisphere oceanic gateways has facilitated ocean
circulation changes and may have influenced climatic variations in the Cenozoic time (66 …

Movements of tectonic plates often induce oblique deformation at divergent plate
boundaries. This is in striking contrast with traditional conceptual models of rifting and rifted …

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

A seismic stratigraphic framework and basin fill geohistory for Arctic Ocean basins is
presented based on data collected by several Russian Government organized expeditions …

The incompleteness of the stratigraphical record is well documented, and the concept of
“missing time” has attracted renewed attention in recent years. However, the importance of …