[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 …
salient geological characteristics and correlations among the main and relatively minor …
Tectonic evolution of Variscan Iberia: gondwana–Laurussia collision revisited
An integrated interpretation of the late Paleozoic structural and geochronological record of
the Iberian Massif is presented and discussed under the perspective of a Gondwana …
the Iberian Massif is presented and discussed under the perspective of a Gondwana …
İŞ TATMİNİNİ ETKİLEYEN İŞLETME İÇİ FAKTÖRLERİN EĞİTİM SEKTÖRÜ AÇISINDAN DEĞERLENDİRİLMESİNE YÖNELİK BİR ALAN ARAŞTIRMASI
Geleceğin nitelikli iş gücünü yetiştiren eğitim kurumlarının istenilen özellikte faaliyet
göstermelerinin sağlanabilmesi için bu insan gücünü yetiştiren eğitimcilerin işlerinden …
göstermelerinin sağlanabilmesi için bu insan gücünü yetiştiren eğitimcilerin işlerinden …
Pre-Mesozoic Alpine basements—their place in the European Paleozoic framework
JF Von Raumer, F Bussy, U Schaltegger… - …, 2013 - pubs.geoscienceworld.org
Prior to their Alpine overprinting, most of the pre-Mesozoic basement areas in Alpine
orogenic structures shared a complex evolution, starting with Neoproterozoic sediments that …
orogenic structures shared a complex evolution, starting with Neoproterozoic sediments that …
The birth of the Rheic Ocean—Early Palaeozoic subsidence patterns and subsequent tectonic plate scenarios
JF von Raumer, GM Stampfli - Tectonophysics, 2008 - Elsevier
New plate-tectonic reconstructions of the Gondwana margin suggest that the location of
Gondwana-derived terranes should not only be guided by the models, but should also …
Gondwana-derived terranes should not only be guided by the models, but should also …
Cambrian ensialic rift-related magmatism in the Ossa-Morena Zone (Évora–Aracena metamorphic belt, SW Iberian Massif): Sm–Nd isotopes and SHRIMP zircon U–Th …
The Late Ediacaran (c. 560–550 Ma) Série Negra sediments of the Évora–Aracena
metamorphic belt, Ossa-Morena Zone, SW Iberian Massif, preserve a record of the erosion …
metamorphic belt, Ossa-Morena Zone, SW Iberian Massif, preserve a record of the erosion …
The missing Rheic Ocean magmatic arcs: provenance analysis of Late Paleozoic sedimentary clastic rocks of SW Iberia
Early Carboniferous turbiditic sedimentary rocks in synorogenic basins located on both
sides of the Rheic suture in SW Iberia were studied for provenance analysis. An enigmatic …
sides of the Rheic suture in SW Iberia were studied for provenance analysis. An enigmatic …
Variscan intra-orogenic extensional tectonics in the Ossa-Morena Zone (Évora-Aracena-Lora del Rı́o metamorphic belt, SW Iberian Massif): SHRIMP zircon U-Th-Pb …
Abstract Following a Middle–Late Devonian (c. 390–360 Ma) phase of crustal shortening
and mountain building, continental extension and onset of high-medium-grade metamorphic …
and mountain building, continental extension and onset of high-medium-grade metamorphic …
Early carboniferous wrenching, exhumation of high-grade metamorphic rocks and basin instability in SW Iberia: Constraints derived from structural geology and U–Pb …
New U–Pb and 40Ar–39Ar geochronology and structural data from high-to medium grade
metamorphic shear zones of the Ossa-Morena Zone, and structural data from Early …
metamorphic shear zones of the Ossa-Morena Zone, and structural data from Early …
Time-space distribution of silicic plutonism in a gneiss dome of the Iberian Variscan Belt: The Évora Massif (Ossa-Morena Zone, Portugal)
Abstract In the Iberian Variscan Belt, polyphasic deformation has been recognized as
comprising an early phase of crustal thickening, followed by an intermediate phase of crustal …
comprising an early phase of crustal thickening, followed by an intermediate phase of crustal …