Sen-Elster smeltevandsler - en mulig ledehorisont i det vestlige Jylland

Translated title of the contribution: ( Late-Elster outwash clay - a possible marker horizon in western Jutland).

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Abstract

According to glaciostratigraphic investigations the glaciolacustrine clay is found below a Warthe (Saale II) till and a younger unit of Weichselian meltwater deposits. The glaciolacustrine clay unit is correlated to late Elsterian age. Sedimentological investigations indicate that the glaciolacustrine clay unit at Nygard Hage is deposited in the deeper wave-dominated part of a glacial lacustrine basin, whereas at Toftum Bjerge distal delta deposits are found in addition to the glacial lacustrine clay. The glaciolacustrine clay unit is distributed over a large area of the western part of Jutland and may probably be used as a stratigraphically significant marker horizon.-from English summary

Translated title of the contribution( Late-Elster outwash clay - a possible marker horizon in western Jutland).
Original languageDanish
Pages (from-to)21-35
Number of pages15
JournalÅrsskrift for Dansk geologisk Forening
Volume1984
Publication statusPublished - 28 Feb 1985
Externally publishedYes

Programme Area

  • Programme Area 5: Nature and Climate

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