(Tables 1-2) Composition of red coloured tills from Schobuell, Schleswig-Holstein and Møn Island, Denmark

DOI

The stratigraphic position of the glacially transported 'Scholle' (large-size erratic block) at Schobüll near Husum (Schleswig-Holstein) is now considered to be Devonian rather than 'Rotliegendes'. The 'Scholle', consisting of red clay and dolomite, is overlain by red-colored till without any flint but with up to 90% carbonate clasts (containing 15% dolomite), which indicates an eastern Baltic origin. The relationship of the 'Scholle' with the glacial till also points to an eastern Baltic origin for it, with up to 1 000 km transport distance.

DEPTH, sediment is approximate.

Supplement to: Meyer, Klaus-Dieter (1981): Die rote Gesteinsscholle von Schobüll bei Husum (Schleswig-Holstein) - Rotliegendes oder Old Red? Meyniana, 33, 1-7

Identifier
DOI https://doi.org/10.1594/PANGAEA.784451
Related Identifier https://doi.org/10.2312/meyniana.1981.33.1
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.784451
Provenance
Creator Meyer, Klaus-Dieter
Publisher PANGAEA
Publication Year 1981
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Dataset; Dataset
Format text/tab-separated-values
Size 122 data points
Discipline Earth System Research
Spatial Coverage (9.017W, 54.504S, 12.249E, 54.926N); Møn Island, Denmark; Schleswig-Holstein, Germany
Temporal Coverage Begin 1976-01-01T00:00:00Z
Temporal Coverage End 1978-07-01T00:00:00Z