The architecture and tectono-magmatic evolution of the lithosphere of Europe are the result of a succession of subduction, rifting and inputs from plumes that have modified the …
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 …
We provide a thorough review of the literature on peraluminous magmatism of Late Neoproterozoic and Early Palaeozoic (mostly Late Cambrian-Middle Ordovician) age …
The Velay anatectic dome in the Variscan French Massif Central exposes a low-pressure– high-temperature metamorphic sequence, which represents an ideal natural laboratory for …
Heterogenous isotopic ratios in magmatic rocks have been variously interpreted to be a result of magma mixing or inheritance from the source rock. Isotopic heterogeneities in …
The continental crust of Europe west of the Trans-European Suture Zone (TESZ), is mostly a collage of Peri-Gondwana Cadomian and Avalonian terranes that were formed on the late …
The Earth is unique in the Solar System due to significant volumes of granite in the lithosphere. However, the origins of granites are still highly debated, especially sediment …
Anatectic magmas form plutons or accumulate in the core of anatectic domes. Both scenarios have distinct implications on the behaviour of the continental crust during …
M Bosq, P Bertran, JP Degeai, A Queffelec, O Moine - Aeolian Research, 2020 - Elsevier
Pleistocene loess of the Rhône Valley and Provence region, disconnected from the two main European aeolian systems (North European Loess Belt and Danube basin), are of …