Open AccessA geological concept of the map sheet Rønde based on dynamic structures
Author(s) -
Kaj Strand Petersen,
Leif Aabo Rasmussen
Publication year - 1987
Publication title -
danmarks geologiske undersøgelse. serie c/dgu serie. c
Language(s) - English
Resource type - Journals
eISSN - 2597-2995
pISSN - 0900-6362
DOI - 10.34194/seriec.v8.7102
Subject(s) - geology , paleontology , pleistocene , glacial period , quaternary , marine transgression , holocene , outwash plain , cenozoic , paleogene , geologic map , structural basin , geomorphology
During the mapping of the map sheet Rønde 1315 II an important kineto-stratigraphical frame for the Late Middle Weichselian in the central part of Denmark was demonstrated. Quaternary units are deposited on Paleogene sediments consisting of clayey Eocene-Paleocene strata to the southwest and Lower Paleocene-Danian limestone to the northeast. Middle Pleistocene till units are found as erosional remnants on the Prequaternary surface. The Late Pleistocene deposits are described within the kineto-stratigraphical concept, showing an older unit related to a glacial advance from the northeast and a younger one from the south, both belonging to the Late Middle Weichselian glaciation. Prominent extramarginal outwash sand deposits cover - the central part of the map sheet as a part of the drift unit from the south. The low-lying areas have beeen covered by the sea during the Holocene from the transgression in Early Atlantic up to the end of Subboreal. In the Subatlantic, freshwater deposits were formed, later covered by peat.