The assembly of the Gondwana supercontinent during the waning stages of the Proterozoic
provides a tectonic backdrop for the myriad biological, climatological, tectonic and …

The Brunovistulian terrane represents a microcontinent of enigmatic Proterozoic provenance
that was located at the southern margin of Baltica in the early Paleozoic. During the Variscan …

We present two alternative sets of global palaeogeographical reconstructions for the time
interval 615–530 Ma using competing high and low-latitude palaeomagnetic data subsets …

Paleomagnetic results obtained from rocks of Ediacaran age in several localities in
Laurentia and Baltica persistently display co-existence of two magnetization components …

The paleoposition of Baltica at the end of Neoproterozoic is of utmost importance for global
paleogeography, but paleomagnetic data of Ediacaran age are very controversial …

The time-averaged geomagnetic field is generally purported to be uniformitarian across
Earth history—close to a geocentric axial dipole, with average strength within one order of …

Changes in the geomagnetic field over geologic timescales can be used to study the
evolution and processes of its sources in Earth's deep interior. As a stark contrast to the …

Volume 2 provides an overview of the Mesozoic and Cenozoic evolution of Central Europe.
This period commenced with the destruction of Pangaea and ended with the formation of the …

This contribution summarizes selected results of the “Palaeozoic Accretion of Poland”
Project. Emphasis is placed on geochronological, geochemical and palaeomagnetic …

Thick Neoproterozoic rift sequences along the western margin of the East European Craton
(EEC) are classically attributed to rifting leading to break-up of super-continent …