Lockerbraunerden, periglaziale Solifluktionsdecken und holozäne Kolluvien im Oberwald (Hoher Vogelsberg)
The conception that the substratum of the "Lockerbraunerde" of the Hohe Vogelsberg Mountains should represent a Late-Pleistocene, periglacial aeolian sediment, is rejected. It is demonstrated primary by means of radio carbon-datings of fossil Ah-horizons that a large portion of this subs...
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| Format: | Article |
| Language: | deu |
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Copernicus Publications
1998-01-01
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| Series: | Eiszeitalter und Gegenwart |
| Online Access: | https://www.eg-quaternary-sci-j.net/48/67/1998/egqsj-48-67-1998.pdf |