Psilonotenton-Formation
Back to Southern GermanyRepresentation and status
- Index
- juPT
- Color CMYK
- (17%,33%,0%,41%)
- Color RGB
- R: 125 G: 100 B: 150
- Rank
- lithostratigraphic Formation
- Validity
- Unit is in Use
- Status
- valid formal name
Nomenclature
- Deutsch
- Psilonotenton-Formation
- Français
- Psilonotenton-Formation
- Italiano
- Psilonotenton-Formation
- English
- Psilonotenton-Formation
- Origin of the Name
-
Namengebendes Fossil: Ammonitenart Psiloceras psilonotum (Quenstedt) ; siehe Lithostratigraphisches Lexikon Deutschland (LithoLex)
- Historical Variants
-
Psilonotenton-Formation (STD 2002/2016, Bloos et al. 2005, LGRB 2016)
Description
- Thickness
- 4-12 m, bzw. kaum 1 m am Dinkelberg (Bloos et al. 2005)
Hierarchy and sequence
- Subordinate units
- Units at roof
- Lower boundary
-
Schichtlücke zwischen Trias und Jura.
Age
- Age at top
-
- early Hettangian
- Age at base
-
- early Hettangian
Geography
- Geographical extent
- Schwäbische Aln, Hochrhein.
Palaenography and tectonic
-
- Liassic of the Jura Moutains
- Tectonic unit (resp. main category)
- Kind of protolith
-
- sedimentary
-
«Psilonotenbank»
- Name Origin
-
Namengebendes Fossil (Ammonitenart): Psiloceras psilonotum.
- Rank
- lithostratigraphic Bed
- Status
- obsolete term (disused)
- Valid term
- Hallau-Bank
- In short
-
Kondensationshorizont an der Basis der Psilonotenton-Formation, bestehend aus einer sandigen Glaukonit führenden Lumachelle.
- Age
- early Hettangian