«Knorri-Ton»

Representation and status

Color CMYK
siehe Klingnau-Fm.
Color RGB
R: 175 G: 145 B: 115
Rank
lithostratigraphic Member (Subformation)
Validity
Unit is in Use
Status
incorrect name (though informally used)
Status discussion

Bei Gonzalez (1993) als Formationsglied [= Member] des Hauptrogensteins definiert.

Nomenclature

Deutsch
«Knorri-Ton»
Français
«Argile à Knorri»
Italiano
«Argilla di Knorri»
English
«Knorri Clay»
Origin of the Name

Namengebendes Fossil (Bivalvia): Ostrea (Catinulla) knorri (Voltz 1828/Zieten).

Historical Variants

---- (Mühlberg 1898), Knorri-Tone (Müller et al. 1984, Gonzalez 1993), Knorri Clays = Knorri Tone = Argiles à Ostrea knorri (Gonzalez & Wetzel 1996)

Description

Description

Dunkler Tonstein im Dach der Klingnau-Formation mit dünnen Lagen aus knolligem, feinkörnigem Kalk. Lokal tritt die Auster Ostrea Knorri im Gestein auf.

Thickness
Einige Meter (Gonzalez & Wetzel 1996).

Components

Fossil Content
  • ostreids

Age

Age at top
  • middle Bathonian
Age at base
  • early Bathonian

Geography

Geographical extent
Ersetzt den Spatkalk östlich der Lägeren.

Palaenography and tectonic

  • Dogger of the Jura Mountains
Paleogeography
Swabian Basin
Tectonic unit (resp. main category)
Kind of protolith
  • sedimentary
Metamorphism
non metamorphic

References

Definition
Gonzalez R., Wetzel A. (1996) : Stratigraphy and paleogeography of the Hauptrogenstein and Klingnau Formations (middle Bajocian to late Bathonian), northern Switzerland Eclogae geol. Helv. 89/2, 695-720

p.705: The Knorri Clays replace the Spatkalk of the Hauptrogenstein Formation (see below) east of the Lägern Chain. They are a few meters thick and consist of dark clays with occasional layers of fine-grained, nodular limestone, locally with accumulations of the oyster Ostrea knorri.

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