The making of Pangea is the result of large-scale amalgamation of continents and micro-
continents, which started at the end of the Neoproterozoic with the formation of Gondwana …

The non-cylindrical character of the Variscan Belt is established via a description of its most
salient geological characteristics and correlations among the main and relatively minor …

The Rheic Ocean, which separated Laurussia from Gondwana following the closure of
Iapetus, is arguably the most important ocean of the Palaeozoic. Its suture extends from …

Abstract The European Variscan belt is a unique orogen that is covered by comprehensive
sets of seismic and potential field data from the Iberian Peninsula in the west to the Polish …

The Rheic Ocean was one of the most important oceans of the Paleozoic Era. It lay between
Laurentia and Gondwana from the Early Ordovician and closed to produce the vast Ouachita …

The tectonics, dynamics, and biogeographic landscape of the early Paleozoic were
dominated by the opening and expansion of one large ocean—the Rheic—and the …

Terra Nova, 23, 241–247, 2011 Abstract Early Variscan structures and magnetic anomalies
delineate four oroclines along the Variscan belt. The arcs bend the lithostratigraphic zones …

U‐Pb (zircon) crystallization ages of 52 late‐Variscan granitoid intrusions from NW Iberia (19
from new data, 33 from previous studies) constrain the lithospheric evolution of this realm of …

Abstract In Central Vietnam, the Kontum massif is subdivided from North to South into:(i)
Kham Duc,(ii) Ngoc Linh,(iii) Kan Nack complexes. The Kham Duc complex consists of …

Abstract The Late Paleozoic Variscan Orogen of Europe and North Africa comprises
reworked Neoproterozoic to Early Paleozoic crust of the northern Gondwanan shelf that …