Recent progress in plate tectonic reconstructions has seen models move beyond the
classical idea of continental drift by attempting to reconstruct the full evolving configuration of …

Neoproterozoic tectonic geography was dominated by the formation of the supercontinent
Rodinia, its break-up and the subsequent amalgamation of Gondwana. The Neoproterozoic …

The extent and nature of the Archaean–Palaeoproterozoic craton of Río de la Plata of
southern South America, a major but poorly understood crustal component in …

Abstract The Pan-African Damara orogenic system records Gondwana amalgamation
involving serial suturing of the Congo–São Francisco and Río de la Plata cratons (North …

The southernmost outcrops of the Río de la Plata cratonic region are exposed in the Tandilia
System in eastern Argentina. The geological evolution comprises mainly an igneous …

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 …

Constraining the paleogeography of the Ediacaran is crucial for understanding the extensive
tectonic, biological and geochemical changes that occurred during that epoch …

Previous studies have proposed that a major suture resulted from the collision between the
Amazonian and São Francisco-Congo cratons during the Cambrian, following the closure of …

The Ediacaran apparent polar wander path (APWP) for the Rio de la Plata Craton was
analyzed and a new alternative path is presented. This revised path was constructed …

Central Gondwana was assembled by three continental collisions in relatively quick
succession: late Cryogenian East Africa Orogen, early Ediacaran West Antarctica Orogen …