Angulate tone formation
![](https://upload.wikimedia.org/wikipedia/commons/thumb/f/fc/Lithostratigraphie_s%C3%BCddeutscher_Jura.svg/400px-Lithostratigraphie_s%C3%BCddeutscher_Jura.svg.png)
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The Angulate Clay Formation is a lithostratigraphic formation of the southern German Jura. It is limited to the western part of the Swabian Alb and the Upper Rhine Graben and interlocks to the east with the Angulate sandstone formation . It is underlain by the Psilonotenton Formation and overlaid by the Arietenkalk Formation . The Angulate Clay Formation is dated to the Upper Hettangian ( Lower Jurassic ).
definition
The Angulate Clay Formation consists primarily of claystones with a few embedded siltstone banks and silty-sandy limestone banks. It is limited to the western part of the Swabian Alb (west of a line Stuttgart - Hechingen ) and the Upper Rhine area. The thickness varies between 3 and 9 m. The base of the formation is formed by the so-called "Oolithenbank", which contains Eisenooide and Schill. The upper limit is the lower limit of the Arietenkalk Formation , which is, however, formed quite differently. In many areas, the base of the Arietenkalk formation is formed by the so-called "copper rock bank". There is a gap between the Angulate Clay Formation and the Arietenkalk Formation. The sediments of the Angulatenton formation were during the Oberhettangiums deposited that the Ammoniten zones of Alsatites liasicus ( Liasicus zone ) and the Schlotheimia angulata ( Angulata zone comprises).
Breakdown
The Angulate Clay Formation is formally not further subdivided. The so-called "Oolithenbank" is eliminated at the base. In the higher part of the formation there is a 1 m thick sand-lime stone bank, the "Vaihingen-Plasterstein" or "Giant Angulate Bank".
Fossil guide
The Angulate Clay Formation contains ammonites and mussels .
literature
- Gert Bloos, Gerd Dietl, Günter Schweigert: The Jura of Southern Germany in the Stratigraphic Table of Germany 2002. In: Newsletters on Stratigraphy. Vol. 41, No. 1/3, 2005, ISSN 0078-0421 , pp. 263-277.
- Friedrich August Quenstedt: The Jura. Laupp Publishing House, Tübingen 1856–57.
Web links
- German Stratigraphic Commission (Ed.): Stratigraphische Tisch von Deutschland 2002 . Potsdam 2002, ISBN 3-00-010197-7 . (PDF; 6.57 MB)
- Geological overview of the sequence of layers in Baden-Württemberg (PDF; 183 kB)
- Lower Jurassic in Baden-Württemberg ( Memento from September 15, 2011 in the Internet Archive ) (PDF; 12 kB)