Peio-Linie
Rappresentazione e statuto
- Colore CMYK
- N/A
- Colore RGB
- R: 250 G: 50 B: 50
- Rango
- tettonica
- Uso
- Unità in uso.
- Status
- termine informale
Nomenclatura
- Deutsch
- Peio-Linie
- Français
- Faille de Peio
- Italiano
- Falda di Peio
- English
- Pejo Fault
- Origine del nome
-
(Val di) Peio (Italia)
- Varianti storiche
-
Peio-Linie (Bockemühl & Pfister 1985), Peio line (Hoinkes & Thöni 1993), Pejo Fault (TK500 / Gouffon et al. 2024)
- Nota sul nome
-
Pejo-Quarzite (Hammer ----) = Quarzphyllit der Catena Orobica und der Oetztaleralpen (in: Knoblauch & Reinhard 1939 S.79)
Descrizione
- Descrizione
-
major tectonic line separating the Scarl-Campo basement from the Ulten basement
... zwischen Cima-Rovaia-Glimmerschiefer (Campo-Decke) im Norden und Tonale-Schiefer im Süden).
Referenze
- Revisione
-
(2024) :
Tectonic Map of Switzerland 1:500000, Explanatory notes. Federal Office of Topography swisstopo, Wabern
p.99: Further east, a second Late Cretaceous normal fault, the SE-dipping Pejo Normal Fault, accommodates top-E extension combined with a sinistral strike-slip component in the present-day map view (Werling 1992, Viola et al. 2003). The amount of displacement across the Pejo Normal Fault seems to be substantial since this fault juxtaposes the Tonale Nappe that lacks Alpine metamorphic overprint with the southernmost Campo Nappe Complex that was at least locally metamorphosed under upper greenschist-facies conditions during the Alpine cycle (Werling 1992).