The late stages of the Variscan orogeny are characterized by middle to lower crustal melting
and intrusion of voluminous granitoids throughout the belt, which makes it akin to “hot” …

Convergent plate boundaries are characterized by the development of crustal orogenic
wedges and orogenic plateaus but also by gravitational collapse of previously thickened …

Experiments were conducted to explore the behavior of Li, Rb, Nb, Sn, Cs, Ta, W during
crustal melting and test the anatectic origin of rare metal-bearing peraluminous granites …

Flow of partially molten crust controlling construction, growth and collapse of the Variscan
orogenic belt: the geologic record of the French Massif CentralImpact du fluage de la croûte …

Abstract The Ongole Domain in the southern Eastern Ghats Belt of India formed during the
final stages of Columbia amalgamation at ca. 1600 Ma. Yet very little is known about the …

Abstract In the Variscan French Massif Central and Armorican Massif, the tectonic
significance of a widespread NW–SE-trending stretching lineation, coeval with medium …

In France, the Devonian–Carboniferous Variscan orogeny developed at the expense of
continental crust belonging to the northern margin of Gondwana. A Visean–Serpukhovian …

Abstract Sikinos and Ios Islands, located in the Southern Cyclades, represent part of a
Cenozoic metamorphic core complex system that exposes subduction‐related metamorphic …

Age constraints on the protoliths, deformation, metamorphism and melting events are key
parameters when correlating different continental lithospheric remnants among each other …

Abstract In the northern Variscan French Massif Central, the Sioule metamorphic series
exposes from top to bottom the tectonic superposition of the Upper Gneiss Unit (UGU) …