Wolhusen-Bentonit
Torna a bacino molassicoRappresentazione e statuto
- Colore CMYK
- (0%,4%,0%,0%)
- Colore RGB
- R: 255 G: 245 B: 255
- Rango
- Strato litostratigrafico
- Uso
- Unità in uso.
- Status
- termine locale (informale)
Nomenclatura
- Deutsch
- Wolhusen-Bentonit
- Français
- Bentonite de Wolhusen
- Italiano
- Bentonite di Wolhusen
- English
- Wolhusen Bentonite
- Origine del nome
- Varianti storiche
- Bentonitvorkommen von Wolhusen (Pavoni & Schindler 1981), Wolhusen bentonite (Kälin & Kempf 2009)
Geografia
- Estensione geografica
- E-Teil des Napf-Schuttfächers.
- Regione-tipo
- E Napf-Gebiet
- Località-tipo
-
-
Vorder Ämsere, 600 m südlich der Kirche Wolhusen
Caratteristiche del sito- Obergrenze
- Untergrenze
- typische Fazies
- Bohrkern
- (2648000 / 1211330)
- M. Freimoser in: Pavoni & Schindler 1981
-
Vorder Ämsere, 600 m südlich der Kirche Wolhusen
Referenze
- Revisione
-
2009) :
High-resolution stratigraphy from the continental record of the Middle Miocene Northern Alpine Foreland Basin of Switzerland. N. Jb. Geol. Paläont. Abh. 254/1-2, 177-235
On the eastern side of the Napf alluvial fan, near Wolhusen, a bentonite horizon has been described by PAVONI & SCHINDLER (1981). A correlation to the bentonite levels of the Zürich region is not yet established, however, given its lithostratigraphic position the Wolhusen bentonite is most probably equivalent to the Urdorf bentonite.
(