Gondwana is reviewed from the unification of its several cratons in the Late Neoproterozoic,
through its combination with Laurussia in the Carboniferous to form Pangea and up to its …

The Variscides of Europe and N-Africa are the result of the convergence of the plates of
Gondwana and Laurussia in the Paleozoic. This orogen is characterized by the juxtaposition …

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

The Portscatho Formation, within the allochthonous unit of the Middle and Upper Devonian
Gramscatho Group, is a thick sequence of deep-water sandstones and interbedded slates …

We review the highlights of the 1988 symposium on Palaeozoic Biogeography and
Palaeogeography, and present a revised set of 20 Palaeozoic base maps that incorporate …

The earth's history is traced through the tectonic evolution of the continental crust from the
very beginning of the geological record, rather than by studying the stratigraphy of a …

New palaeogeographical reconstructions are presented at 10 myr intervals from the Lower
Cambrian at 540 Ma to the Lower Devonian at 400 Ma, showing continental crustal …

This review focuses on the tectonics and sedimentation of major sedimentary basins and
orogenic belts (Late Proterozoic–Neogene) in the Korean peninsula. The Korean peninsula …

The mid-European segment of the Variscides is a tectonic collage consisting of (from north
to south): Avalonia, a Silurian–early Devonian magmatic arc, members of the Armorican …

The geological record preserves evidence for two fundamental stages in the evolution of
Earth's biosphere, a microbial stage from~ 3.5 to 0.65 Ga, and a metazoan stage evident by …