In this contribution, we will describe examples from the subducted continental crust of the Western Alps, Austroalpine domain. We will integrate results from structural geology, petrology/geochemistry, and modelling, at different scales from lithosphere to atomic scale, emphasising the roles of contrasting tectono-metamorphic evolutions versus the efficiency of rocks to memorize their promenade along the subduction plate interface or close to it. We will compare the evolution of continental crust slices found at different positions within the subduction architecture and recording specific structural features and metamorphic parageneses. We emphasise that the combined use of structural and metamorphic criteria is the only nowadays reliable m...
We report on the structural architecture and metamorphic evolution of a m\ue9lange, developed origin...
International audienceConvergence zones present very different morphologies depending on the type of...
A survey is given of the dimensions and composition of the present continental crust. The abundances...
In the Alpine continental crust structural, metamorphic, sedimentary and igneous signatures indicate...
In the Sesia-Lanzo Zone, Western Alps, the Rocca Canavese Thrust Sheets (RCT) subunit is characteriz...
In the Sesia-Lanzo Zone (SLZ), the subunit Rocca Canavese Thrust Sheet (RCT) is characterised by a m...
Geological mapping, multiscale structural analysis, and estimations of the degree of fabric evolutio...
In metamorphic basements, 3D geological modelling, based on multiscale correlation of superposed str...
Detailed mapping of superposed fabrics and their mineral support allows for reconstruction of the te...
The geological structure of continental lithosphere shows complex variety that is inherited into oro...
International audienceIn this paper we review and discuss, in a synthetic historical way, the main r...
The concept of 'metamorphic field gradient' applied to the lithologically homogeneous deep crust of ...
Preservation of stratigraphic settings in continents is mostly confined to uppermost crustal levels,...
The narrow axial zone of collisional belts, where ocean closure apparently generates the highest tec...
In the Southern Apennines and Calabria outcrop metamorphic slices of hercynian and/or alpine age. Th...
We report on the structural architecture and metamorphic evolution of a m\ue9lange, developed origin...
International audienceConvergence zones present very different morphologies depending on the type of...
A survey is given of the dimensions and composition of the present continental crust. The abundances...
In the Alpine continental crust structural, metamorphic, sedimentary and igneous signatures indicate...
In the Sesia-Lanzo Zone, Western Alps, the Rocca Canavese Thrust Sheets (RCT) subunit is characteriz...
In the Sesia-Lanzo Zone (SLZ), the subunit Rocca Canavese Thrust Sheet (RCT) is characterised by a m...
Geological mapping, multiscale structural analysis, and estimations of the degree of fabric evolutio...
In metamorphic basements, 3D geological modelling, based on multiscale correlation of superposed str...
Detailed mapping of superposed fabrics and their mineral support allows for reconstruction of the te...
The geological structure of continental lithosphere shows complex variety that is inherited into oro...
International audienceIn this paper we review and discuss, in a synthetic historical way, the main r...
The concept of 'metamorphic field gradient' applied to the lithologically homogeneous deep crust of ...
Preservation of stratigraphic settings in continents is mostly confined to uppermost crustal levels,...
The narrow axial zone of collisional belts, where ocean closure apparently generates the highest tec...
In the Southern Apennines and Calabria outcrop metamorphic slices of hercynian and/or alpine age. Th...
We report on the structural architecture and metamorphic evolution of a m\ue9lange, developed origin...
International audienceConvergence zones present very different morphologies depending on the type of...
A survey is given of the dimensions and composition of the present continental crust. The abundances...