Late Palaeozoic palaeomagnetic and tectonic constraints for amalgamation of Pangea supercontinent in the European Variscan belt
This paper provides a review of the evolution of palaeomagnetic directions and sequence of
tectonic events in the European Variscan belt during Late Palaeozoic times. These data are …
tectonic events in the European Variscan belt during Late Palaeozoic times. These data are …
The Atlas-East Variscan-Elbe shear system and its role in the formation of the pull-apart Late Palaeozoic basins
The Variscan orogeny occurred as a result of the Late Devonian to Late Carboniferous
collision and accretion of Gondwana-derived microcontinents and continental masses with …
collision and accretion of Gondwana-derived microcontinents and continental masses with …
Pre‐Alpine (Variscan) inheritance: a key for the location of the future Valaisan Basin (Western Alps)
The boundary between the Helvetic and the Penninic (= Briançonnais) Zones has long been
recognized as a major fault (“Penninic Front”) in the Western Alps. A narrow oceanic domain …
recognized as a major fault (“Penninic Front”) in the Western Alps. A narrow oceanic domain …
[PDF][PDF] The Calabria-Peloritani Orogen, a composite terrane in Central Mediterranean; its overall architecture and geodynamic significance for a pre-Alpine scenario …
R Cirrincione, E Fazio, P Fiannacca… - Periodico di …, 2015 - researchgate.net
Abstract The Calabria-Peloritani Orogen is an arcuate segment of the peri-Mediterranean
orogenic Alpine nappe system that comprises the whole Calabria and the north-eastern …
orogenic Alpine nappe system that comprises the whole Calabria and the north-eastern …
Transpressive deformation in the southern european variscan belt: new insights from the aiguilles rouges massif (Western Alps)
Despite the Mediterranean sector of the Variscan Belt being fragmented and reworked
during Alpine orogenesis, evidence for the activity of a right‐lateral strike‐slip shear zone …
during Alpine orogenesis, evidence for the activity of a right‐lateral strike‐slip shear zone …
Constraining the timing of evolution of shear zones in two collisional orogens: fusing structural geology and geochronology
In recent decades, constraining the timing of shear activity has been one of the main topics
of research about the tectono-metamorphic evolution of orogenic belts. We present a review …
of research about the tectono-metamorphic evolution of orogenic belts. We present a review …
Late‐orogenic Evolution of the Southern European Variscan Belt Constrained by Fabric Analysis and Dating of the Camarat Granitic Complex and Coeval Felsic …
Abstract The Camarat Granitic Complex (CGC), emplaced in the migmatitic Internal Zone of
the Maures–Tanneron Massif (MTM), SE Variscides, consists of the Gigaro granodiorite and …
the Maures–Tanneron Massif (MTM), SE Variscides, consists of the Gigaro granodiorite and …
HTLP metamorphism and fluid‐fluxed melting during multistage anatexis of continental crust (N Sardinia, Italy)
The Variscan high‐grade metamorphic basement of northern Sardinia and southern Corsica
record lower Carboniferous anatexis related to post‐collisional decompression of the …
record lower Carboniferous anatexis related to post‐collisional decompression of the …
Unfolding the arc: The use of pre-orogenic constraints to assess the evolution of the Variscan belt in Western Europe
We present a pre-orogenic, early Paleozoic, palinspastic reconstruction of the northern
Gondwana margin that was subsequently involved in the Late Paleozoic Variscan orogeny …
Gondwana margin that was subsequently involved in the Late Paleozoic Variscan orogeny …
Timing and kinematics of flow in a transpressive dextral shear zone, Maures Massif (Southern France)
Abstract The Maures–Tanneron Massif and the Corsica–Sardinia Block are two segments of
the southern European Variscan belt that separated during the Late Oligocene–Miocene …
the southern European Variscan belt that separated during the Late Oligocene–Miocene …