Gerstenhübel-Bank
Back to Effingen-MemberRepresentation and status
- Color CMYK
- cf. Effingen-Member
- Color RGB
- R: 190 G: 195 B: 185
- Rank
- lithostratigraphic Bed
- Validity
- Unit is in Use
- Status
- informal term
- Status discussion
Nomenclature
- Deutsch
- Gerstenhübel-Bank
- Français
- Banc du Gerstenhübel
- Italiano
- Strato del Gerstenhübel
- English
- Gerstenhübel Bed
- Origin of the Name
-
Gerstenhübel, Veltheim (AG)
- Historical Variants
- Gerstenhübelkalk (Jäckli 1966, Hantke 1967), Gerstenhübel-Schicht (Gygi 1969), Gerstenhübel Beds (Gygi 2000b, Gygi 2000c), Gerstenhübel-Kalkschicht
- Nomenclatorial Remarks
- Schon von F. Mühlberg ausgeschieden. Hübel = Hügel, Berg, Erhebung
Description
- Description
- Wohlgeschichtete (in Bänken von 20 cm bis 30 cm), leicht mergelige Kalksteine mit spärlichem Vorkommen von Fossilien. Eine rund 10 m mächtige, feingeschichtete Mergelkalkbankabfolge wird im Steinbruch Jakobsberg von Gygi (1969) als Gerstenhübel-Bank 1) bezeichnet und mit dem Riffgürtel der Günsberg-Formation weiter im Westen korreliert (Gygi 2000). Innerhalb des insgesamt 230 m mächtigen Effingen-Members der Bohrung Küttigen-1 (Ref. 3) identifizieren Albert et al. (2007) eine 28 m mächtige Kalkbankabfolge, welche rund 88 m über der Basis einsetzt, als Gerstenhübel-Bank.
- Geomorphology
- Prominente morphologische Rippe innerhalb des Effingen-Members.
- Thickness
- Bis 12 m; 16 m (Wetzel & Strasser 2001) ; 13,4 m an der Typlokalität (Gygi 1973)
Components
Fossil Content
- protists
Hierarchy and sequence
- Superordinate unit
- Units at roof
- Units at floor
Age
- Age at top
-
- middle Oxfordian
- Age at base
-
- middle Oxfordian
- Dating Method
- Bifurcatus-Zone : Amoeboceras cf. serratum (Sowerby) (Atrops et al. 1993, Gygi 2000b)
Geography
- Geographical extent
- Erlinsbach - Holderbank - Chestenberg - Villigen (AG).
- Type area
- Nördlicher Kt. Aargau
- Type locality
-
-
Gerstenhübel (AG)
Site particularities- Obergrenze
- Untergrenze
- typische Fazies
- Steinbruch, Tongrube
- (2654100 / 1252500)
- Steinbruch Jakobsberg, N von Wildegg (Gygi 1969 S.66 Pl.17 Profil RG37, Gygi 2000c)
-
Gerstenhübel (AG)
- Type profile
-
-
Gerstenhübel (AG)
Site particularities- Obergrenze
- Untergrenze
- typische Fazies
- Steinbruch, Tongrube
- (2654100 / 1252500)
- Steinbruch Jakobsberg, N von Wildegg (Gygi 1969 S.66 Pl.17 Profil RG37, Gygi 2000c)
-
Gerstenhübel (AG)
Palaenography and tectonic
-
- Malm of the Jura Mountains
- Paleogeography
- Argovian Basin
- Tectonic unit (resp. main category)
-
-
Jura
:
Juragebirge
-
Jura
:
- Kind of protolith
-
- sedimentary
- Sequence
- The onset of the 16 m thick limestone deposits of the Gerstenhübel Beds represents a flooding followed by highstand sedimentation with increased carbonate production. A few metres above the top of the Gerstenhübel Beds, a 5 - 10 cm thick mudstone bed is capped by a limonite/pyrite crust up to 3 mm thick. Burrows and borings in this hardground suggest a multiphase formation. The sequence-stratigraphic significance of this horizon is debatable; Pittet (1996) interepreted it as maximum-flooding surface, whereas Allenbach (2001c) suggested a type II sequence boundary (SB Ox6) and sediment by-passing. (Wetzel & Strasser 2001)
- Metamorphism
- non metamorphic
References
- Definition
- 1969) : Geologische Beschreibung des Aargauer-Jura und der nördlichen Gebiete des Kantons Zürich. (
- Definition
-
2000) :
Annotated index of lithostratigraphic units currently used in the Upper Jurassic of northern Switzerland. Eclogae geol. Helv. 93/1, 125-146
(
p.130: Gerstenhübel Beds (Gygi 1969) ; Thick limestone succession within the Effingen Member of the Wildegg Formation The Gerstenhübel Beds (Gerstenhübel-Schicht) were named by Gygi (1969. p. 66). The type locality is the hill called Gerstenhübel (coordinates 654.100/252.500) 2 km south-southeast of Veltheim. Canton Aargau. LK 1089. Aarau. where the unit was quarried for some time. The names Veltheim and Gerstenhübel are not indicated on the map LK 1089, Aarau. The Gerstenhübel Beds are the succession no. 37 in section RG 37 of Gygi (1969. Pl. 17). This is the type section. The Gerstenhübel Beds are a well-bedded succession of