Pre-Alpine tectonic evolution of the Eastern Alps: from prototethys to paleotethys
In all reconstructions published during the last two decades, the Austroalpine and the
correlative Southalpine basement units of the Eastern Alps were considered to represent a …
correlative Southalpine basement units of the Eastern Alps were considered to represent a …
[HTML][HTML] The Northern Calcareous Alps revisited: Formation of a hyperextended margin and mantle exhumation in the Northern Calcareous Alps sector of the Neo …
Abstract The Neo-Tethys margin evolution is preserved in the Northern Calcareous Alps
(Eastern Alps), from Late Permian crustal stretching to Late Triassic oceanization. The …
(Eastern Alps), from Late Permian crustal stretching to Late Triassic oceanization. The …
Carboniferous–Triassic tectonic and thermal evolution of the middle crust section of the Dervio–Olgiasca Zone (Southern Alps)
C Real, K Fassmer, R Carosi… - Journal of …, 2023 - Wiley Online Library
A well‐preserved remnant of the middle crust of the former Adriatic passive margin is
exposed in the Southern Alps (Italy). The Dervio–Olgiasca Zone is located south of the …
exposed in the Southern Alps (Italy). The Dervio–Olgiasca Zone is located south of the …
[HTML][HTML] The role of structural inheritance in continental break-up and exhumation of Alpine Tethyan mantle (Canavese Zone, Western Alps)
Abstract The Canavese Zone (CZ) in the Western Alps represents the remnant of the distal
passive margin of the Adria microplate, which was stretched and thinned during the Jurassic …
passive margin of the Adria microplate, which was stretched and thinned during the Jurassic …
Metamorphic remnants of the Variscan Orogeny across the alps and their tectonic significance
Lithospheric slices preserving pre-Alpine metamorphic imprints are widely described in the
Alps. The Variscan parageneses recorded in continental, oceanic, and mantle rocks suggest …
Alps. The Variscan parageneses recorded in continental, oceanic, and mantle rocks suggest …
What drives A lpine T ethys opening? Clues from the review of geological data and model predictions
Permo‐Triassic remnants (300–220 Ma) of high‐temperature metamorphism associated
with large gabbro bodies occur in the Alps and indicate a high thermal regime compatible …
with large gabbro bodies occur in the Alps and indicate a high thermal regime compatible …
Metamorphic facies and deformation fabrics diagnostic of subduction: Insights from 2D numerical models
We developed a 2D numerical model that simulates the evolution of a subduction in order to
analyze which different metamorphic facies and deformation fabrics can be recorded within …
analyze which different metamorphic facies and deformation fabrics can be recorded within …
[HTML][HTML] How many subductions in the Variscan orogeny? Insights from numerical models
We developed a 2D numerical model to simulate the evolution of two superposed ocean-
continent-ocean subduction cycles with opposite vergence, both followed by continental …
continent-ocean subduction cycles with opposite vergence, both followed by continental …
3D reconstruction of fabric and metamorphic domains in a slice of continental crust involved in the Alpine subduction system: The example of Mt. Mucrone (Sesia …
Geological map**, multiscale structural analysis, and estimations of the degree of fabric
evolution and of reaction progress allow the construction of a 3D quantitative model of …
evolution and of reaction progress allow the construction of a 3D quantitative model of …
Cld-St-And-bearing assemblages in the central Southalpine Basement: Markers of an evolving thermal regime during Variscan convergence
Multiscale structural analysis is carried out to explore the sequence of superposed pre-
Alpine chloritoid–staurolite–andalusite metamorphic assemblages in the polydeformed …
Alpine chloritoid–staurolite–andalusite metamorphic assemblages in the polydeformed …