True polar wander would be recognized paleomagnetically as identical apparent polar wander paths for all surface elements. The apparent polar wander paths for the Late Ordovician-Late Devonian interval for Laurentia, Baltica and Gondwana have nearly identical looping shapes that can be brought into superposition. The paths of these continents are well documented, but even the less well known paths of South China and Siberia reveal similar lengths. The resulting reconstruction places the northern Andean margin of South America opposite the Appalachian margin of Laurentia, with Baltica and Laurentia adjoined in the fit of Bullard and colleagues. Siberia and South China would be to the north of Africa, if their paleopoles are taken at face val...
From the Late Carboniferous until the Middle Jurassic, continents were assembled in a quasi-rigid su...
The Carboniferous to early Permian apparent polar wander (APW) path for Eurasia is not well constrai...
Hotspot tracks represent plate motions relative to mantle sources, and paleomagnetic data from magma...
Paleomagnetically determined apparent polar wander (APW) paths should contain components of individu...
A significant number of new palaeomagnetic poles have become available since the last time a compila...
A significant number of new palaeomagnetic poles have become available since the last time a compila...
true polar wander (TPW) occurred during the Cambrian (520 to 535 Ma). This con-clusion is based on (...
The recognition of wide-spread remagnetization events during the Palaeozoic has greatly added to the...
Utilizing marine magnetic anomalies and paleomagnetic pole positions, paleogeographic maps were cons...
Abstract: Neoproterozoic to Late Palaeozoic times saw the break-up of the supercontinent Rodinia, an...
International audienceA new apparent polar wander path (APWP) from the beginning of the Paleocene (6...
Many of the controversies that arise in global reconstructions for Permian-Triassic time could be re...
propose new apparent polar wander paths for Baltica during the Early-Mid Palaeozoic and discuss thei...
International audienceWe have constructed new apparent polar wander paths (APWPs) for major plates o...
The recognition of wide-spread remagnetization events during the Palaeozoic has greatly added to the...
From the Late Carboniferous until the Middle Jurassic, continents were assembled in a quasi-rigid su...
The Carboniferous to early Permian apparent polar wander (APW) path for Eurasia is not well constrai...
Hotspot tracks represent plate motions relative to mantle sources, and paleomagnetic data from magma...
Paleomagnetically determined apparent polar wander (APW) paths should contain components of individu...
A significant number of new palaeomagnetic poles have become available since the last time a compila...
A significant number of new palaeomagnetic poles have become available since the last time a compila...
true polar wander (TPW) occurred during the Cambrian (520 to 535 Ma). This con-clusion is based on (...
The recognition of wide-spread remagnetization events during the Palaeozoic has greatly added to the...
Utilizing marine magnetic anomalies and paleomagnetic pole positions, paleogeographic maps were cons...
Abstract: Neoproterozoic to Late Palaeozoic times saw the break-up of the supercontinent Rodinia, an...
International audienceA new apparent polar wander path (APWP) from the beginning of the Paleocene (6...
Many of the controversies that arise in global reconstructions for Permian-Triassic time could be re...
propose new apparent polar wander paths for Baltica during the Early-Mid Palaeozoic and discuss thei...
International audienceWe have constructed new apparent polar wander paths (APWPs) for major plates o...
The recognition of wide-spread remagnetization events during the Palaeozoic has greatly added to the...
From the Late Carboniferous until the Middle Jurassic, continents were assembled in a quasi-rigid su...
The Carboniferous to early Permian apparent polar wander (APW) path for Eurasia is not well constrai...
Hotspot tracks represent plate motions relative to mantle sources, and paleomagnetic data from magma...