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Lateral accretion features ( epsilon cross-bedding) and point bars in the weichselian Køge Esker, East­Sjælland, Denmark
Author(s) -
Jens P. Jensen
Publication year - 1988
Publication title -
bulletin of the geological society of denmark
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.674
H-Index - 28
eISSN - 2245-7070
pISSN - 0011-6297
DOI - 10.37570/bgsd-1988-37-02
Subject(s) - bedding , geology , accretion (finance) , bar (unit) , point bar , geomorphology , point (geometry) , geometry , physics , astrophysics , mathematics , oceanography , structural basin , horticulture , biology , fluvial
In the Køge Esker, Spanager lateral accretion features ( epsilon cross-bedding) were produced by complex point bar growth. The point bar genesis is based upon the presence of epsilon cross-bedding, the channel side attached nature of the bar (inner accretionary bank) and the paleoflow pattern. The Spanager sequence is divided into three flow discharge cycles ("megavarvic" sedimentation units).

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