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Rolf, Christian; Hambach, Ulrich; Novothny, Ágnes; Horváth, Erzsébet; Schnepp, Elisabeth (2020): Fig. 8 RPI Süttö compared to Glopis and Piso data [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.918143, In: Rolf, C et al. (2020): Rock- and palaeomagnetic investigations of an Upper Pleistocene loess–palaeosol sequence near Süttő, Hungary [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.917734

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Published: 2020-05-29DOI registered: 2020-07-16

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Keyword(s):
data correlation; Piso and Glopis data stack; RPI; Süttö
Related to:
Rolf, Christian; Hambach, Ulrich; Novothny, Ágnes; Horváth, Erzsébet; Schnepp, Elisabeth (2014): Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttő, Hungary). Quaternary International, 319, 99-108, https://doi.org/10.1016/j.quaint.2013.08.050
Coverage:
Latitude: 47.738000 * Longitude: 18.448000
Minimum DEPTH, sediment/rock: 3.095 m * Maximum DEPTH, sediment/rock: 9.240 m
Event(s):
Suettoe * Latitude: 47.738000 * Longitude: 18.448000 * Location: Hungary * Comment: LPSS-profile outcropping at Hegyhati quarry (Süttö)
Comment:
Comparison between the RPI record obtained at Sütto and the GLOPIS (Laj et al., 2004) and the PISO stack (cut-out PISO 1.5 Ma; Channell et al., 2009). Correlation intervals for indirect dating. Above depths of 6 m, the RPI signal at Sütto is ambiguous. Nevertheless, based on the reasonable assumption of strongly increased accumulation rates, a possible correlation of the upper part of the section near 4 m to the time span between 22 and 24 ka is proposed.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1DEPTH, sediment/rockDepth sedmRolf, ChristianGeocode
2Relative paleointensity proxyRPIRolf, ChristianRPI trend corrected 0-1
3Year of observationYear obsa ADRolf, Christian
4Profile IDProfile IDRolf, Christian
Size:
825 data points

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