Soja-Decke

Représentation et statut

Variantes historiques: --- (Argand 1915, Jenny 1923, Egli 1966), Sojateildecke (Heydweiller 1918), Sojadecke = Sojalappen = Sojazug (Bosshard 1925), Valsojadecke (Staub 1920), Sojamulde (Kündig 1926a), Soia-Decke (Niggli et al. 1936), Sojaschuppe (Egli 1966), Sinclinale di Soja (Bianconi 1971), Soja nappe = nappe de Soja = soja unit s.str. (Galster et al. 2010), Soja unit (Galster et al. 2012), Soi-Decke, falda della Val Soi, falda della Val Soja

Unités hiérarchiquement subordonnées

Unités sus-jacentes

Unités sous-jacentes

Extension géographique: Val Soi, Val Mavaglia, Val Combra, Val Pontirone (+ Pizzo di Claro?) [kommt auf den GA25-Blättern XXX_Biasca, XXX_Grono, XXX_Mesocco, XXX_Olivone und XXX_Osogna vor].

Révision: Gouffon Yves (Editor) (2024) : Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern

p.53: The small Soja Nappe includes a polycyclic crystalline basement covered by Permian to Jurassic sediments. It is located below the Adula Nappe in its frontal part, where it is wedged between this latter nappe and the Simano Nappe. To the north, it extends into the Garzott Slices located in the core of the Lunschania Antiform and surrounded by the Piz Terri-Lunschania Nappe. Due to this structural position, Galster et al. (2012) attached the Garzott Slices to the Piz Terri-Lunschania Nappe, but the facies analogies bring them closer to the Soja Nappe (Vögeli et al. 2013). A paleogeographic origin of the Soja Nappe between the Piz Terri-Lunschania Nappe and the Adula Nappe is plausible.