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Original Articles

A 2000 year geomagnetic record from two Late Weichselian sequences in southeast Sweden

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Pages 21-29 | Received 16 Sep 1985, Published online: 06 Jan 2010

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Esin YÜZBAŞI. (2021) Isparta’nın İlk Kadın Milletvekili Fatma Mihriban Erden’in Meclis Faaliyetleri (1983-1987). JOURNAL OF HISTORY AND FUTURE 7:4, pages 800-824.
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Bryan C. Lougheed, Andreas Nilsson, Svante Björck, Ian Snowball & Raimund Muscheler. (2014) A deglacial palaeomagnetic master curve for Fennoscandia – Providing a dating template and supporting millennial-scale geomagnetic field patterns for the past 14 ka. Quaternary Science Reviews 106, pages 155-166.
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Bryan C. Lougheed, Ian Snowball, Matthias Moros, Karoline Kabel, Raimund Muscheler, Joonas J. Virtasalo & Lukas Wacker. (2012) Using an independent geochronology based on palaeomagnetic secular variation (PSV) and atmospheric Pb deposition to date Baltic Sea sediments and infer 14C reservoir age. Quaternary Science Reviews 42, pages 43-58.
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JONAS ISING. (2008) Late Weichselian pollen stratigraphy, clay varve chronology and palaeomagnetic secular variations in Lake Bolmen, Småland, south Sweden. Boreas 30:3, pages 189-204.
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Jonas Ising. (2001) Late Weichselian pollen stratigraphy, clay varve chronology and palaeomagnetic secular variations in Lake Bolmen, Småland, south Sweden. Boreas 30:3, pages 189-204.
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Svante Björck, Ingemar Cato, Lars Brunnberg & Bo Strömberg. 1992. The Last Deglaciation: Absolute and Radiocarbon Chronologies. The Last Deglaciation: Absolute and Radiocarbon Chronologies 25 44 .
T. J. F. Austin & J. J. Lowe. (1989) A Late Devensian Lateglacial palaeomagnetic record from Llyn Gwernan, North Wales: comparison with other NW European records. Geophysical Journal International 99:3, pages 699-710.
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PER SANDGREN, SVANTE BJÖRCK, LARS BRUNNBERG & JAN KRISTIANSSON. (2008) Palaeomagnetic records from two varved clay sequences in the Middle Swedish ice marginal zone. Boreas 17:2, pages 215-227.
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Svante Björck, Per Sandgren & Björn Holmquist. (2006) A magnetostratigraphic comparison between 14 C years and varve years during the Late Weichselian, indicating significant differences between the time‐scales . Journal of Quaternary Science 2:2, pages 133-140.
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