Rothenfluh-Member

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Representation and status

Color CMYK
siehe Passwang-Fm.
Color RGB
R: 170 G: 120 B: 70
Rank
lithostratigraphic Member (Subformation)
Validity
Unit is in Use
Status
valid formal name
Scs Note

Beschluss

Scs Date
01.01.2004
Status discussion

Nomenclature

Deutsch
Rothenfluh-Member
Français
Membre de la Rothenfluh
Italiano
Membro della Rothenfluh
English
Rothenfluh Member
Origin of the Name

Roti Flue, nördlich von Rothenfluh (BL)

Historical Variants

Rothenfluh-Schichten (Lusser 1980), Rothefluh-Member, Rothenfluh Beds = Rothenfluh Schichten = Couches de Rothenfluh (Gonzalez & Wetzel 1996)

Nomenclatorial Remarks

«Blaue Kalke» (sensu Quenstedt 1856/57), «Blagdeni-Schichten» auct. (Moesch 1867, Mühlberg 1900, Strübin 1901, Schmassmann 1945)

Description

Description

An der Basis des Members lokal mit Crinoiden-Brekzie ("Pentacrinitenbreccie" des Staffeleggebietes ; Mühlberg 1900).

Thickness
Ca. 25 m im Westen, 10 m im Osten (Gonzalez & Wetzel 1996).

Components

Fossil Content
  • crinoids

Hierarchy and sequence

Superordinate unit
Upper boundary

Im Übergang zum Hauptrogenstein (Untere Acuminata-Schichten im Osten, Grenchenberg-Member im Westen) nimmt der Ooidgehalt der Kalke zu und die Mergellagen setzen aus.

Lower boundary

Hartgrund im Dach der Humphriesi-Schichten.

Stratigraphic discussion

Lokal mit Korallen (horizon à coraux supérieur de Cornol).

Age

Age at top
  • middle Bajocian
Age at base
  • middle Bajocian
Dating Method

Biostratigraphie: Ammoniten

Geography

Geographical extent
Delsberg – Ostrand der Burgunder Plattform (Linie Gansingen (AG) – Schinznach (AG)).
Type locality

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
Conditions of formation

Gegen Osten zunehmend distaleres, epikontinentales Meer (Gonzalez 1993).

Metamorphism
non metamorphic

References

Definition
Lusser C. (1980) : Sedimentologie und Paläogeographie des unteren Doggers im zentralen und nördlichen Jura. Diss. Univ. Basel
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.707: The Rothenfluh Beds occur throughout the Jura (synonyms: "Blagdeni Schichten", "Blaue Kalke" sensu Quenstedt 1856/57). They consist of marly, bioclastic mud- and wackestones interbedded with fine-grained, often quartz-bearing (up to 25%). nodular limestones. The unit is approximately 25 m thick in the western and 10 m in the eastern Jura.

The Rothenfluh Beds can be considered a member of the Hauptrogenstein Formation, if the Hauptrogenstein Formation is defined in a genetic sense as an alloformation. However, in a strictly lithostratigraphic sense the Rothenfluh Beds should not be included in the Hauptrogenstein Formation.

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