Add to ORKGThe Schneeberg Complex is a part of the austroalpine nappe stack system and is located west of the Tauern Window (Fig. 1). While the surrounding nappe units experienced a polymetamorphic history, the Schneeberg Complex is basically a monometamorphic sedimentary sequence which experienced its main deformation phase during the late cretaceous (Frisch, Kuhlemann, Dunkl, &
The Turňa Unit (Turnaicum, Tornaicum) is one of the three nappe systems involved in the geological s...
The Mont Morion complex of the Dent Blanche nappe is interpreted as a multi-stadial Alpine km-scale ...
New structural, thermobarometric and geochronological data allow integrating kinematics, timing and ...
The Ötztal Nappe in the Eastern Alps is a thrust sheet of Variscan metamorphic basement rocks and th...
The Scheiblingkirchen window, a Lower Austroalpine tectonic window at the eastern margin of the East...
The Schneeberg Complex (Merano, NE Italy) was traditionally distinguished from the surrounding Aust...
The Penninic nappes in the Swiss Alps formed during continental collision between the Adriatic and E...
The classica! methods of structural analysis were applied in the Texel Gruppe (upper Spronsertal, Ea...
Continental collision during alpine orogeny entailed a thrust and fold belt system. The Penninic nap...
solidated in late Precambrian time) to the south and the Rhenohercynian zone to the north. It is cha...
Fold-and-thrust belts are prominent structures that occur at the front of compressional orogens. To ...
International audienceDuring Cretaceous time, the area of the future Helvetic nappes (Central Alps, ...
The structural analysis of the Austroalpine units in Graubunden reveals the existence of two orogeni...
The Dorozsma Complex (DC) is defined and its main lithologies are described. The complex makes up th...
AbstractRechnitz window group represents a Cordilleran-style metamorphic core complex, which is almo...
The Turňa Unit (Turnaicum, Tornaicum) is one of the three nappe systems involved in the geological s...
The Mont Morion complex of the Dent Blanche nappe is interpreted as a multi-stadial Alpine km-scale ...
New structural, thermobarometric and geochronological data allow integrating kinematics, timing and ...
The Ötztal Nappe in the Eastern Alps is a thrust sheet of Variscan metamorphic basement rocks and th...
The Scheiblingkirchen window, a Lower Austroalpine tectonic window at the eastern margin of the East...
The Schneeberg Complex (Merano, NE Italy) was traditionally distinguished from the surrounding Aust...
The Penninic nappes in the Swiss Alps formed during continental collision between the Adriatic and E...
The classica! methods of structural analysis were applied in the Texel Gruppe (upper Spronsertal, Ea...
Continental collision during alpine orogeny entailed a thrust and fold belt system. The Penninic nap...
solidated in late Precambrian time) to the south and the Rhenohercynian zone to the north. It is cha...
Fold-and-thrust belts are prominent structures that occur at the front of compressional orogens. To ...
International audienceDuring Cretaceous time, the area of the future Helvetic nappes (Central Alps, ...
The structural analysis of the Austroalpine units in Graubunden reveals the existence of two orogeni...
The Dorozsma Complex (DC) is defined and its main lithologies are described. The complex makes up th...
AbstractRechnitz window group represents a Cordilleran-style metamorphic core complex, which is almo...
The Turňa Unit (Turnaicum, Tornaicum) is one of the three nappe systems involved in the geological s...
The Mont Morion complex of the Dent Blanche nappe is interpreted as a multi-stadial Alpine km-scale ...
New structural, thermobarometric and geochronological data allow integrating kinematics, timing and ...