The “Lund Moraine” – the geomorphic limit of the last Young Baltic ice advance in the Öresund region-Reference-Cited by-同舟云学术

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The “Lund Moraine” – the geomorphic limit of the last Young Baltic ice advance in the Öresund region

Published:2023-12-21 Issue: Volume: Page:1-5
ISSN:1103-5897
Container-title:GFF
language:en
Short-container-title:GFF

Author:

Regnéll Carl¹²^ORCID,Alexanderson Helena³^ORCID,Greenwood Sarah L.¹²,Gyllencreutz Richard¹²^ORCID,Öhrling Christian⁴^ORCID

Affiliation:

1. Department of Geological Sciences, Stockholm University, Stockholm, Sweden

2. The Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden

3. Department of Geology, Lund University, Lund, Sweden

4. Department of Quaternary Geology for Physical Planning, Geological Survey of Sweden, Uppsala, Sweden

Funder

Swedish Research Council

Knut and Alice Wallenberg Foundation

Publisher

Informa UK Limited

Subject

Paleontology,Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/11035897.2023.2281676

Reference31 articles.

1. Adrielsson, L., 2001: Subglacial hydrology and bed deformation dynamics during Late Weichselian Ice lobe surge in the Öresund strait area, south Scandinavia. Abstract. In D.J.A. Evans, J.A. Piotrowski & C.D. Clark (eds.): Palaeo-ice Stream International Symposium. University of Aarhus, Denmark. p. 7.

2. Adrielsson L. Mohrén E. & Daniel E. 1981: Beskrivning till jordartskartan Helsingborg SV . Sveriges Geologiska Undersökning Serie Ae 16 104 pp.

3. Weichselian history of the Fennoscandian ice sheet in southern Sweden and the southwestern Baltic Basin

4. A10Be-based reconstruction of the last deglaciation in southern Sweden

5. Eemian and Weichselian stratigraphy in South Sweden

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