[HTML][HTML] The Mid-Variscan Allochthon: Keys from correlation, partial retrodeformation and plate-tectonic reconstruction to unlock the geometry of a non-cylindrical belt

JRM Catalan, K Schulmann, JF Ghienne - Earth-Science Reviews, 2021 - Elsevier
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 …

Metamorphic remnants of the Variscan Orogeny across the alps and their tectonic significance

M Roda, MI Spalla, M Filippi, JM Lardeaux, G Rebay… - Geosciences, 2023 - mdpi.com
Lithospheric slices preserving pre-Alpine metamorphic imprints are widely described in the
Alps. The Variscan parageneses recorded in continental, oceanic, and mantle rocks suggest …

Early Paleozoic or Early-Middle Triassic collision between the South China and Indochina blocks: The controversy resolved? Structural insights from the Kon Tum …

M Faure, LTT Hoai, C Lepvrier - Journal of Asian Earth Sciences, 2018 - Elsevier
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 …

Magmatism during continental collision, subduction, exhumation and mountain collapse in collisional orogenic belts and continental net growth: A perspective

SG Song, MJ Wang, C Wang, YL Niu - Science China Earth Sciences, 2015 - Springer
Continental orogens on Earth can be classified into accretionary orogen and collisional
orogen. Magmatism in orogens occurs in every periods of an orogenic cycle, from oceanic …

Flow of partially molten crust controlling construction, growth and collapse of the Variscan orogenic belt: the geologic record of the French Massif Central

O Vanderhaeghe, O Laurent… - Bulletin de la …, 2020 - pubs.geoscienceworld.org
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 …

Post-collisional magmatism: Consequences of UHPM terrane exhumation and orogen collapse, N. Qaidam UHPM belt, NW China

M Wang, S Song, Y Niu, L Su - Lithos, 2014 - Elsevier
Exhumation of subducted slabs and extensional collapse of orogens are the main tectonic
processes in ancient and modern continental collisional zones. Magmatism during these two …

Topography of the Variscan orogen in Europe: failed–not collapsed

W Franke - International Journal of Earth Sciences, 2014 - Springer
The Variscan orogenic collage consists of three subduction-collision systems (Rheno-
Hercynian, Saxo-Thuringian and Massif Central-Moldanubian). Devonian to early …

Pre-Cadomian to late-Variscan odyssey of the eastern Massif Central, France: formation of the West European crust in a nutshell

C Chelle-Michou, O Laurent, JF Moyen, S Block… - Gondwana …, 2017 - Elsevier
Abstract The East Massif Central (EMC), France, is part of the internal zone of the Variscan
belt where late Carboniferous crustal melting and orogenic collapse have largely obliterated …

Sedimentary response to the paleogeographic and tectonic evolution of the southern North China Craton during the late Paleozoic and Mesozoic

DB Yang, HT Yang, JP Shi, WL Xu, F Wang - Gondwana Research, 2017 - Elsevier
With the aim of constraining the influence of the surrounding plates on the Late Paleozoic–
Mesozoic paleogeographic and tectonic evolution of the southern North China Craton …

Evolution of the Corsica–Sardinia Batholith and late-orogenic shearing of the Variscides

L Casini, S Cuccuru, A Puccini, G Oggiano, P Rossi - Tectonophysics, 2015 - Elsevier
Abstract The Corsica–Sardinia Batholith formed in the late Carboniferous–Permian along
the northern Gondwana margin. One or more of the following processes may have raised …