Add to ORKGParticipants: Ansorge Jörg (ETHZ) den Brok Bas (EAWAG-EMPA) Dèzes Pierre (SANW) Gonzalez Laura (University of Bern) Herwegh Marco (University of Bern) Hürzeler Jean-Pierre (University of Basel) Imper David (GeoPark) Mancktelow Neil (ETHZ) Mullis Josef (University of Basel) Nyffenegger Franziska (Fachhochschule Burgdorf, University of Bern) Pfiffner Adrian (University of Bern) Schreurs Guido (University of Bern) Schmalholz Stefan (ETHZ) Schmid Stefan (University of Basel) Wiederkehr Michael (University of Basel) Wilson Christopher (Melbourne University) Wilson Lilian (Melbourne University
New stratigraphic data along a profile from the Helvetic Gotthard Massif to the remnants of the Nort...
The Pennine Basal Thrust (PBT) is an exhumed megathrust developed during continental collision from ...
The aim of this thesis was to develop a comprehensive tectonic model of the Helvetic zone of Vorarlb...
We present a geological map, profiles and the results of a detailed structural analysis of the Early...
lowed a pre-existing Miocene age erosional angular unconformity (Fig. 1; German: "Reliefübersc...
The Glarus thrust is a prominent tectonic feature in the eastern Helvetic Alps that has been investi...
Thrust-related fluid flow coupled with isotopic exchange between fluid and rock is simulated in a th...
The purpose of the 1979 excursion of the Swiss Geological Society was to show the recent interpretat...
Along the Glarus thrust different lithologies that are part of the footwall are in contact with one ...
International audienceSince two centuries the European Alps are a natural laboratory to study contin...
The Upper Rhine Graben (URG) is an area with a great geological potential, in relation with many top...
The formation and structural evolution of the Jungfrau syncline is described, based on excellent out...
This study is devoted to the analysis of a prominent concentration of earthquakes whose epicenters d...
In the Western Alps, some recent scarps were previously interpreted as surface ruptures of tectonic ...
The article examines the organizational patterns of nineteenth-century Swiss Alpine geology. It argu...
New stratigraphic data along a profile from the Helvetic Gotthard Massif to the remnants of the Nort...
The Pennine Basal Thrust (PBT) is an exhumed megathrust developed during continental collision from ...
The aim of this thesis was to develop a comprehensive tectonic model of the Helvetic zone of Vorarlb...
We present a geological map, profiles and the results of a detailed structural analysis of the Early...
lowed a pre-existing Miocene age erosional angular unconformity (Fig. 1; German: "Reliefübersc...
The Glarus thrust is a prominent tectonic feature in the eastern Helvetic Alps that has been investi...
Thrust-related fluid flow coupled with isotopic exchange between fluid and rock is simulated in a th...
The purpose of the 1979 excursion of the Swiss Geological Society was to show the recent interpretat...
Along the Glarus thrust different lithologies that are part of the footwall are in contact with one ...
International audienceSince two centuries the European Alps are a natural laboratory to study contin...
The Upper Rhine Graben (URG) is an area with a great geological potential, in relation with many top...
The formation and structural evolution of the Jungfrau syncline is described, based on excellent out...
This study is devoted to the analysis of a prominent concentration of earthquakes whose epicenters d...
In the Western Alps, some recent scarps were previously interpreted as surface ruptures of tectonic ...
The article examines the organizational patterns of nineteenth-century Swiss Alpine geology. It argu...
New stratigraphic data along a profile from the Helvetic Gotthard Massif to the remnants of the Nort...
The Pennine Basal Thrust (PBT) is an exhumed megathrust developed during continental collision from ...
The aim of this thesis was to develop a comprehensive tectonic model of the Helvetic zone of Vorarlb...