Scisti di Biò
Darstellung und Status
- Farbe CMYK
- (0%,0%,0%,100%)
- Rang
- lithostratigraphische Einheit
- Gebrauch
- Element ist in Gebrauch
- Status
- lokaler Begriff (informell)
Nomenklatur
- Deutsch
- Biò-Schiefer
- Français
- Schistes de Biò
- Italiano
- Scisti di Biò
- English
- Biò Schist
- Herkunft des Namens
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Biò (Italia), E Ivrea
- Historische Varianten
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Bio' schists = Scisti di Bìo' (Biino & Compagnoni 1989), Scisti di Biò (Dal Piaz et al. 1992a)
Alter
- Alter Top
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- Später Jura
- Alter Basis
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- Später Jura
Referenzen
- Erstdefinition
-
(1989) :
The Canavese Zone between the Serra d*Ivrea and the Dora Baltea River (Western Alps). Eclogae geol. Helv. 82/2, 413-417
p.418: The Bio' Schists
A small slice of metasedimentary rocks is exposed north of Bio', close to the contact with the Sesia Zone. The Bio' Schists have been interpreted in various ways in the Canavese geological literature. They are composed of a continous sequence of folded pelite, siltite and arenite with interbedded arkose and impure limestone. The Bio' Schists are considered to be Malm in age (Biino & Compagnoni 1989a) such as the Lago Pistono Schists.