2011
DOI: 10.1016/b978-0-444-53447-7.00019-2
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Pleistocene Glaciations in Lithuania

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Cited by 48 publications
(45 citation statements)
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“…(Dm,Im) = (204.4°,N = 18,a95 = 5.06° / (Dm,Im) = (18.9°,57.1),N = 5,a95 = 6.98°;B) demagnetization of samples S4,S14,S16,S22 and S18. Brought to you by | MIT Libraries Authenticated Download Date | 5/13/18 12:07 AM Mikulian) sections in other European countries (Ber, 2000;Lindner et al, 2013;Shick, 2014;Stephan, 2014;and other). The environmental history of the Merkine˙ (Eemian) Interglacial (130-117 ka) is rather well studied (Guobytė and Satkūnas, 2011).…”
Section: Discussionmentioning
confidence: 99%
“…(Dm,Im) = (204.4°,N = 18,a95 = 5.06° / (Dm,Im) = (18.9°,57.1),N = 5,a95 = 6.98°;B) demagnetization of samples S4,S14,S16,S22 and S18. Brought to you by | MIT Libraries Authenticated Download Date | 5/13/18 12:07 AM Mikulian) sections in other European countries (Ber, 2000;Lindner et al, 2013;Shick, 2014;Stephan, 2014;and other). The environmental history of the Merkine˙ (Eemian) Interglacial (130-117 ka) is rather well studied (Guobytė and Satkūnas, 2011).…”
Section: Discussionmentioning
confidence: 99%
“…The Dzūkija till is of a grey, greenish grey and greyish brown colour and is predominated by gravel and pebbles of crystalline rocks presumably transported from southern Sweden (Gaigalas 1979). The high content of SiO 2 , TiO 2 , Ti, Zr and Yb as compared with other tills of the Middle and Upper Pleistocene and the low content of CO 2 , MgO and FeO are characteristic for the Dzūkija till (Guobytė, Satkūnas 2011).…”
Section: Middle Pleistocenementioning
confidence: 99%
“…The Kalviai Formation is overlain by the Vindžiūnai interglacial deposits (Kondratienė 1996;Guobytė, Satkūnas 2011) that have been discovered in the same Kalviai representative site and encountered in five sections (see Fig. 2).…”
Section: Middle Pleistocenementioning
confidence: 99%
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“…However, when dealing with marginal areas of the Late Weichselian Scandinavian ice sheet it faces many uncertainties related to the peculiarities of local environmental conditions and problems with stratigraphical subdivision of sediment layers (Satkūnas 2011;Šeirienė et al 2015). The landform variety of insular-type Samogitian Upland (Guobytė 2004) situated in the north−western part of Lithuania provides such specific conditions. The upland was formed during the Pomeranian (Baltija) Stage of the Weichselian (locally named Nemunas) glaciation.…”
Section: Introductionmentioning
confidence: 99%