[HTML][HTML] Orogenic architecture of the Mediterranean region and kinematic reconstruction of its tectonic evolution since the Triassic
The basins and orogens of the Mediterranean region ultimately result from the opening of
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
oceans during the early break-up of Pangea since the Triassic, and their subsequent …
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 …
Deformation and temperature variation along thrust-sense shear zones in the hinterland-foreland transition zone of collisional settings: A case study from the Barbagia …
Abstract In the Internal Zone of a continental collisional orogen, first-order contractional
shear zones accommodate crustal shortening. Structural investigations at different scales …
shear zones accommodate crustal shortening. Structural investigations at different scales …
Kinematics and timing constraints in a transpressive tectonic regime: The example of the Posada-Asinara Shear Zone (NE Sardinia, Italy)
Detailed geological field mapping, integrated with meso-and microstructural investigations,
kinematic of the flow and finite strain analyses, combined with geochronology, are …
kinematic of the flow and finite strain analyses, combined with geochronology, are …
Evolution of the Corsica–Sardinia Batholith and late-orogenic shearing of the Variscides
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 …
the northern Gondwana margin. One or more of the following processes may have raised …
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 …
The Late Palaeozoic-Early Mesozoic from the Catalan Pyrenees (Spain): 60 Myr of environmental evolution in the frame of the western peri-Tethyan palaeogeography
Abstract The Eastern Catalan Pyrenees form the southernmost segment of the Pyrenean
Axial Zone. They experienced complex multistage process as the result of both the Variscan …
Axial Zone. They experienced complex multistage process as the result of both the Variscan …
Stratigraphic evolution in the Ligurian Alps between Variscan heritages and the Alpine Tethys opening: A review
A Decarlis, G Dallagiovanna, A Lualdi, M Maino… - Earth-Science …, 2013 - Elsevier
Abstract The Ligurian Alps are the southernmost segment of the Alpine orogenic belt. Their
formation is the result of a multistage process that comprises two orogenic cycles: the …
formation is the result of a multistage process that comprises two orogenic cycles: the …
Early Permian 90° clockwise rotation of the Maures–Estérel–Corsica–Sardinia block confirmed by new palaeomagnetic data and followed by a Triassic 60° clockwise …
Palaeomagnetic investigations of the Corso-Sardinian block and Maures–Estérel show that
there has been a change in their magnetic orientation during the Late Carboniferous–Early …
there has been a change in their magnetic orientation during the Late Carboniferous–Early …