Germanic Trias


The Germanic Trias Supergroup is a lithostratigraphic unit in the subsurface of large parts of western and central Europe and the North Sea. Almost all of the Germanic Trias was deposited during the Triassic period and consists of three clearly different units: Buntsandstein, Muschelkalk and Keuper, that gave the period its name. In the past the names of these three units were also used as units in the geologic timescale, but in modern literature they only have a lithostratigraphic meaning.

Origin

The Germanic Trias formed in the large Germanic Basin, a basin that covered much of midwestern Europe during the Triassic. The Muschelkalk has a predominantly marine facies whereas the Buntsandstein and Keuper are mostly continental.

Stratigraphy

In the central parts of the Germanic Basin, the Germanic Trias has an average thickness of 800 meters, but regional differences are considerable. In the north of Germany the thickness of the Buntsandstein alone can exceed 1400 meters. The Germanic Trias lies on top of the Permian Zechstein Group and below Lower Jurassic units, such as the Lias Group or Altena Group.
The base is not defined in the same way everywhere. In northern Germany the base is formed by the Calvörde Beds, in the Spessart and Odenwald by the base of the Heigenbrücken-Sandstone. Radiometric dating has shown the age of the Germanic Trias is not totally corresponding with the Triassic period. The base of the Buntsandstein was formed during the Changhsingian, the uppermost stage of the Permian, about. The top of the Keuper is Rhaetian in age and at about at least a few million years older than the Triassic-Jurassic boundary. Usually there is a stratigraphic hiatus between the base of the Lias and top of the Germanic Trias.
In German lithostratigraphy, Buntsandstein, Muschelkalk and Keuper are seen as groups. Dutch lithostratigraphy divides the Germanic Trias along other boundaries in a Lower Germanic Trias Group and an Upper Germanic Trias Group. The Dutch Keuper and Muschelkalk have the status of formations while the Dutch Buntsandstein is subdivided in a number of formations. The Bunter of British stratigraphy is similar in age, lithology and facies to the Buntsandstein.