1. A change of the drainage system in the Permian-Triassic sedimentary sequence of the Hessian Depression (Germany).
- Author
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Koslowski, Wolfram and Tietze, Klaus-Werner
- Subjects
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DRAINAGE , *BRAIDED rivers , *PERMIAN-Triassic boundary , *ALLUVIAL fans , *FACIES - Abstract
The sedimentary sequence of the Permian-Triassic transition period of the central German "Hessian Depression" is characterised by up to 50 m of red beds. These sediments gradationally evolved from the Late Permian marine evaporitic formations of the Zechstein and they contain in their lower part several tens of metres of silts and clays of a mud playa environment, the main part of which is the [former] "Bröckelschiefer" [i. e. the Ohre, Friesland, and Fulda formations of the Hessian Depression] (Zechstein, Upper Permian). The overlying Lower Buntsandstein Subgroup is interpreted as an extended sandy braided river system, which had filled the subsiding basin. Although the entire sedimentary sequence seems to be rather continuous, there is a very distinct break in the main drainage direction between the "Bröckelschiefer" [facies, upper Zechstein] and the Lower Buntsandstein: The sedimentation of the "Bröckelschiefer" is, due to west-east directed drainage processes, associated with alluvial fans along the western bounding Rhenish Massif, which carried the finer clastic materials over a very low relief. On the contrary, the Lower Buntsandstein Subgroup in the same basin is a remnant of a braid-plain-like fluvial system, draining the mountainous highs of the Bohemian Massif, the Vindelician High, and the Massif Central in a strictly northward direction. This break in the drainage system reveals a relatively important tectonic uplifting of the southern surrounding areas. [ABSTRACT FROM AUTHOR]
- Published
- 2021
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