«Spatkalk» (des Hauptrogensteins)

Representation and status

Color CMYK
siehe Hauptrogenstein
Color RGB
R: 210 G: 185 B: 135
Rank
lithostratigraphic Member (Subformation)
Validity
Unit is in Use
Status
incorrect name (though informally used)
Status discussion

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

Nomenclature

Deutsch
«Spatkalk» (des Hauptrogensteins)
Français
«Spatkalk» (Hauptrogenstein)
Italiano
«Spatkalk» (Hauptrogenstein)
English
«Spatkalk» (Hauptrogenstein)
Historical Variants

Spatkalk (Moesch 1867, Mühlberg 1898, Gonzalez 1993, Gonzalez & Wetzel 1996), Spatkalk mit Ostrea Knorri = Knorri-Spatkalk (Mühlberg 1900), Knorri-Spathkalk (Tobler 1905 Tab.6b)

Links

Non-synonyms

Description

Description

Der oft grobe, bioklastische und ausschliesslich aus Echinodermentrümmern (hauptsächlich Crinoidenstielgliedern) mit Nester von Limonit ("eisenschüssige Spatkalke") bestehende Kalk ist dünnplattig und hart.

Thickness
2-12 m (Gonzalez & Wetzel 1996), Weniger als 1 m bis 22 m.

Components

Fossil Content
  • echinoderms

Hierarchy and sequence

Superordinate unit
Upper boundary

angebohrte Regressionsfläche

Age

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

Biostratigraphie: Ammoniten

Geography

Geographical extent
Aargauer Jura. Der Spatkalk geht nach Westen in den «Ferrugineus-Oolith» und nach Osten in den «Knorri-Ton» (Klingnau-Fm.) über.
Type area
Aargauer Jura
Type profile
Point of interest

Palaenography and tectonic

  • Dogger of the Jura Mountains
Paleogeography
Northern Tethyan Carbonate Platform :
Plateforme de Bourgogne, ... = Northern Tethyan Carbonate Platform (NTCP)
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.709: The "Spatkalk" dominates the top of the Hauptrogenstein Formation from the eastern Jura to the Lägern Chain (Fig. 4). Its thickness varies between 2 and 12 m (values included in Fig. 5c). Characteristic are bioclastic (usually coarse echinoderm fragments), often strongly limonitic pack- to grainstones with mm to dm thick marls as background sediments.

  • «Obere Crinoiden-Schichten»

    Name Origin

    Namengebendes Fossil (Crinoid): Pentacrinus leuthardti De Loriol.

    Rank
    lithostratigraphic Bed
    Status
    local name (informal)
    In short

    Graubrauner, gelb und lehmig anwitternder Kalk im Dach des Hauptrogensteins (bzw. an der Basis der Ifenthal-Fm.). Besteht zur Hälfte aus Crinoidentrümmern.

    Age
    Bathonian
Back to top
This site or embedded third-party content uses cookies.
This site or embedded third-party content uses cookies, but we respect your 'Do Not Track' browser setting, which is currently enabled!
Close menu