Baden-Irchel-Herdern Lineament
Représentation et statut
- Couleur RGB
- R: 250 G: 50 B: 50
- Rang
- accident tectonique
- Usage
- Ce terme n'est pas en usage.
- Status
- terme local (informel)
Nomenclature
- Deutsch
- Baden-Irchel-Herdern-Störung
- English
- Baden-Irchel-Herdern Lineament
- Origine du nom
-
Linie Baden (AG) - Irchel (ZH) - Herdern (TG)
- Variantes historiques
-
Baden-Irchel-Herdern Lineament (Naef et al. 1995, Malz et al. 2016, Gouffon et al. 2024)
Paléogéographie et tectonique
- Type de protolithe
-
- tectonique
- Métamorphisme
- non métamorphique
Références
- Révision
-
(2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
p.22: Towards the southeast, the Neuhausen Fault intersects the WSW– ENE trending Baden-Irchel-Herdern Lineament (Naef et al. 1995, Malz et al. 2016; see § 3.2). It is thus presumed that this intersection results in an accordingly trending bend in the graben system, as similarly observed further to the north according to the interpretation of 3D seismic data (Birkhäuser et al. 2001). However, the precise continuation of the graben bounding fault system towards the southeast remains unclear.