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Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin...

Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin...

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_6ef84e3e05724aa791c0a15759e42ae4

Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin sediment core

About this item

Full title

Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin sediment core

Publisher

Cham: Springer International Publishing

Journal title

Swiss Journal of geosciences, 2022-12, Vol.115 (1), p.7-25, Article 7

Language

English

Formats

Publication information

Publisher

Cham: Springer International Publishing

More information

Scope and Contents

Contents

The modern, over 250-m-deep basin of Lake Constance represents the underfilled northern part of an over 400-m-deep, glacially overdeepened trough, which reaches well into the Alps at its southern end. The overdeepening was formed by repeated glacial advance-retreat cycles of the Rhine Glacier throughout the Middle to Late Pleistocene. A seismic sur...

Alternative Titles

Full title

Postglacial evolution of Lake Constance: sedimentological and geochemical evidence from a deep-basin sediment core

Identifiers

Primary Identifiers

Record Identifier

TN_cdi_doaj_primary_oai_doaj_org_article_6ef84e3e05724aa791c0a15759e42ae4

Permalink

https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_6ef84e3e05724aa791c0a15759e42ae4

Other Identifiers

ISSN

1661-8726

E-ISSN

1661-8734

DOI

10.1186/s00015-022-00412-1

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