Resumé
The topography of the contact between Quaternary sediments and underlying pre-Quaternary sediments within the map sheet 1215 Viborg (1:100.000) is constructed from geological data from more than 2000 wells.
It is concluded that fluvial erosion previous to the Quaternary glaciations is the main factor influenced on the topography. Halokinesis of Permian evaporites seems to have influenced locally.
The topography of the Quaternary sedimentary cover generally conforms to the topography of the pre-Quaternary top surface.
It is concluded that fluvial erosion previous to the Quaternary glaciations is the main factor influenced on the topography. Halokinesis of Permian evaporites seems to have influenced locally.
The topography of the Quaternary sedimentary cover generally conforms to the topography of the pre-Quaternary top surface.
Originalsprog | Dansk |
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Titel | DGU Årbog 1978 |
Forlag | DGU |
Sider | 119-129 |
Antal sider | 11 |
ISBN (Trykt) | 87-421-1111-1 |
DOI | |
Status | Udgivet - 1 nov. 1979 |
Publikationsserier
Navn | DGU Årbog |
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Vol/bind | 1978 |
ISSN | 0105-063X |
Programområde
- Programområde 1: Data