1986
DOI: 10.3285/eg.36.1.04
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Late Pleistocene Stratigraphy and Fluvial History of the Dinkel Basin (Twente, Eastern Netherlands)

Abstract: Abstract. Das glaziale Dinkelbecken ist erfüllt mit einer Sequenz von fluviatilen und äolischen Ablagerungen. Die Spätpleistozän-Stratigraphie und Paläomorphologie würde mit Hilfe von neuen Aufschlüssen, Bohrungen und geo-elektrischen Sondierungen erforscht. Besondere Beachtung galt der Verfeinerung in der Lithostratigraphie des Dinkeltals, des Typusgebietes der Twente-Formation, und einer Rekonstruktion des Ablagerungsmilieus in den verschiedenen Perioden der Weichseleiszeit. Die Talauffüllung besteht aus San… Show more

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Cited by 9 publications
(9 citation statements)
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“…Furthermore, facies 1 deposits are frequently disturbed by cryogenic processes associated with seasonal freezing and thawing and therefore the horizontal bedding has a wavy or crinkly appearance due to water saturation and water escape, and sometimes the original horizontal bedding has been almost totally erased giving the sediment a massive structure. Ice-wedge casts and vertical platy structures associated with intense surface cooling of the permafrost landscape are common periglacial features in this facies type (Van Huissteden et al, 1986;Mol et al, 1993;Kasse et al, 1995).…”
Section: Facies Types and Depositional Environmentmentioning
confidence: 99%
See 1 more Smart Citation
“…Furthermore, facies 1 deposits are frequently disturbed by cryogenic processes associated with seasonal freezing and thawing and therefore the horizontal bedding has a wavy or crinkly appearance due to water saturation and water escape, and sometimes the original horizontal bedding has been almost totally erased giving the sediment a massive structure. Ice-wedge casts and vertical platy structures associated with intense surface cooling of the permafrost landscape are common periglacial features in this facies type (Van Huissteden et al, 1986;Mol et al, 1993;Kasse et al, 1995).…”
Section: Facies Types and Depositional Environmentmentioning
confidence: 99%
“…b Age: The age of the deposits characterized by facies 1 is not well established. Organic remains are generally absent in The Netherlands (Van Huissteden et al, 1986, Kasse et al, 1995 and in Poland (Goździk, 1991;Kozarski, 1993;Bohncke et al, 1995). Underlying radiocarbon-dated Middle Pleniglacial deposits indicate that the overlying fluvio-aeolian deposit has a Late Pleniglacial age (Van Huissteden, 1990;Mol, 1997).…”
Section: Facies 4 With Large-scale Cross Beddingmentioning
confidence: 99%
“…Admixed with snow these shifted sands were redeposited as so-called coversand deposits, resulting in a series of low sand dunes over a partly deflated, partly buried, substrate (Van der Hammen 1951;Kasse 2002;Schokker et al 2007). 1 Meanwhile, smaller rivers like the Linde and Kuinder (fed from snowmelt on the till plateau to the north-east), and the larger rivers Vecht (its catchment reaching east into Münsterland: Van Huissteden et al 1986) and, in the beginning of the glacial, even the Rhine (the northerly course was abandoned half way through the Weichselian; (Busschers et al 2007;Peeters et al 2016), worked their ways through the open lowlands of the study area. The last severe cold phase peaked around 20,000 b.c.…”
Section: Pleistocene Landformsmentioning
confidence: 99%
“…To this end, four electrical resistivity tomography (ERT) profiles have been undertaken using a multimode resistivity imaging system (Syscal Pro Switch, Iris Instruments©). This method is widely employed in alluvial system (Vandenberghe and Desmedt, 1979;Vandenberghe, 1981;Van Huissteden et al, 1986;Chambers et al, 2012;Laigre et al, 2012;Hausmann et al, 2013;Rey et al, 2013;Matys Grygar et al, 2016;Bábek et al, 2018). The survey positioning was chosen in such a way that the paleochannels identified by aerial imagery were intersected.…”
Section: Geophysical Investigationsmentioning
confidence: 99%