(Tables 1-2) Composition of red coloured tills from Schobuell, Schleswig-Holstein and Møn Island, Denmark
Cobertura |
MEDIAN LATITUDE: 54.715220 * MEDIAN LONGITUDE: 10.633225 * SOUTH-BOUND LATITUDE: 54.504440 * WEST-BOUND LONGITUDE: 9.017450 * NORTH-BOUND LATITUDE: 54.926000 * EAST-BOUND LONGITUDE: 12.249000 * DATE/TIME START: 1976-01-01T00:00:00 * DATE/TIME END: 1978-07-01T00:00:00 * MINIMUM DEPTH, sediment/rock: 1 m * MAXIMUM DEPTH, sediment/rock: 3 m |
---|---|
Data(s) |
20/06/1981
|
Resumo |
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. |
Formato |
text/tab-separated-values, 122 data points |
Identificador |
https://doi.pangaea.de/10.1594/PANGAEA.784451 doi:10.1594/PANGAEA.784451 |
Idioma(s) |
en |
Publicador |
PANGAEA |
Direitos |
CC-BY: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted |
Fonte |
Supplement to: Meyer, Klaus-Dieter (1981): Die rote Gesteinsscholle von Schobüll bei Husum (Schleswig-Holstein) - Rotliegendes oder Old Red? Meyniana, 33, 1-7, doi:10.2312/meyniana.1981.33.1 |
Palavras-Chave | #Area/locality; DEPTH, sediment/rock; Description; Dolomite; Event label; Flint; HAND; Hjelm-Moen1978; Limestone; Magmatites; Møn Island, Denmark; Ratio; Sample ID; Sampling by hand; Sandstone; Schleswig-Holstein, Germany; Schobuell1976; Sediments; Size fraction; Sum |
Tipo |
Dataset |