The large Palaeozoic continent of Laurentia was largely in North America, but included parts
of modern Europe. It was independent from late Neoproterozoic times at about 570Ma until it …

We present a new model of the crustal and tectonic structure of the Arctic region north of 60°
N latitude, constrained as a part of the international Atlas of Geological Maps of the …

Using full-colour palaeogeographical maps from the Cambrian to the present, this
interdisciplinary volume explains how plate motions and surface volcanism are linked to …

Palaeogeographic and tectono-stratigraphic considerations in the greater Barents Sea show
that the distribution of reservoirs and hydrocarbon source rocks from the Late Palaeozoic to …

Mafic igneous rocks of Cretaceous age (80–130 Ma) scattered around the Arctic Ocean are
commonly referred to as the High Arctic Large Igneous Province (HALIP). We have mapped …

A sequence stratigraphic framework of the Triassic on the Norwegian Barents shelf is
presented. The Triassic succession was subdivided into five second-order sequences based …

Aim I re‐evaluate the specific biogeographical significance of each of the land bridges
(Beringia, Thulean and De Geer) in the Northern Hemisphere during the latest Cretaceous …

Uplift and erosion are complex phenomena in terms of their governing processes, precise
timing and exact magnitude. The intricate relationship between different geodynamic …

A new generation of aeromagnetic data documents the post‐Caledonide rift evolution of the
southwestern Barents Sea (SWBS) from the Norwegian mainland up to the continent‐ocean …

Abstract The Eocene-Oligocene Transition (EOT), approximately 34 Ma ago, marks a period
of major global cooling and inception of the Antarctic ice sheet. Proxies of deep circulation …