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Late Pleistocene fluvial dynamics in the Hochrhein Valley and in the Upper Rhine Graben: chronologic...

Late Pleistocene fluvial dynamics in the Hochrhein Valley and in the Upper Rhine Graben: chronologic...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_856776565

Late Pleistocene fluvial dynamics in the Hochrhein Valley and in the Upper Rhine Graben: chronological frame

About this item

Full title

Late Pleistocene fluvial dynamics in the Hochrhein Valley and in the Upper Rhine Graben: chronological frame

Publisher

Berlin/Heidelberg: Springer-Verlag

Journal title

International journal of earth sciences : Geologische Rundschau, 2010-12, Vol.99 (8), p.1955-1974

Language

English

Formats

Publication information

Publisher

Berlin/Heidelberg: Springer-Verlag

More information

Scope and Contents

Contents

During the Pleistocene, the Rhine glacier system acted as a major south–north erosion and transport medium from the Swiss Alps into the Upper Rhine Graben, which has been the main sediment sink forming low angle debris fans. Only some aggradation resulted in the formation of terraces. Optically stimulated luminescence (OSL) and radiocarbon dating h...

Alternative Titles

Full title

Late Pleistocene fluvial dynamics in the Hochrhein Valley and in the Upper Rhine Graben: chronological frame

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_proquest_miscellaneous_856776565

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_proquest_miscellaneous_856776565

Other Identifiers

ISSN

1437-3254

E-ISSN

1437-3262

DOI

10.1007/s00531-009-0482-9

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