Evolution of an overdeepened trough in the northern Alpine Foreland at 
Niederweningen, Switzerland

Dehnert, A.; Lowick, S. E.; Preusser, F.; Anselmetti, F. S.; Drescher-Schneider, R.; Graf, H. R.; Heller, F.; Horstmeyer, H.; Kemna, H. A.; Nowaczyk, Norbert; Züger, A.; Furrer, H.

doi:10.1016/j.quascirev.2011.12.015

Datensatz

DATENSATZ AKTIONENEXPORT

Zur Ablage hinzufügen

Lokale TagsFreigabegeschichteDetailsÜbersicht

Freigegeben

Zeitschriftenartikel

Evolution of an overdeepened trough in the northern Alpine Foreland at Niederweningen, Switzerland

Urheber*innen

Dehnert, A.
External Organizations;

Lowick, S. E.
External Organizations;

Preusser, F.
External Organizations;

Anselmetti, F. S.
External Organizations;

Drescher-Schneider, R.
External Organizations;

Graf, H. R.
External Organizations;

Heller, F.
External Organizations;

Horstmeyer, H.
External Organizations;

Kemna, H. A.
External Organizations;

/persons/resource/nowa

Nowaczyk, Norbert
5.2 Climate Dynamics and Landscape Evolution, 5.0 Earth Surface Processes, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum;

Züger, A.
External Organizations;

Furrer, H.
External Organizations;

Externe Ressourcen

Es sind keine externen Ressourcen hinterlegt

Volltexte (frei zugänglich)

Es sind keine frei zugänglichen Volltexte in GFZpublic verfügbar

Ergänzendes Material (frei zugänglich)

Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar

Zitation

Dehnert, A., Lowick, S. E., Preusser, F., Anselmetti, F. S., Drescher-Schneider, R., Graf, H. R., Heller, F., Horstmeyer, H., Kemna, H. A., Nowaczyk, N., Züger, A., Furrer, H. (2012): Evolution of an overdeepened trough in the northern Alpine Foreland at Niederweningen, Switzerland. - Quaternary Science Reviews, 34, 127-145.
https://doi.org/10.1016/j.quascirev.2011.12.015

https://gfzpublic.gfz-potsdam.de/pubman/item/item_244519

Zusammenfassung

Quaternary deposits in the overdeepened Wehntal, Switzerland, were investigated using both seismic profiling and the analysis of 93.6 m long drill core using sedimentology, geochemistry, palynology, magnetic properties, and luminescence dating. The sediments reveal evidence for two glacial advances that reached the area during Marine Isotope Stage (MIS) 6. The first advance (∼185 ka) may have carved out the basin or at least removed the entire previous Quaternary sediment filling. This first advance likely reached far beyond the limit of the maximum of the Last Glaciation. The second advance (∼140 ka) was of smaller extent, possibly of cold-based nature, and likely reached only slightly beyond the limits of the Last Glaciation.