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Rolf, Christian; Hambach, Ulrich; Novothny, Ágnes; Horváth, Erzsébet; Schnepp, Elisabeth (2020): Fig. 6 (bottom) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and ARM [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.918044, 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: 2020-05-27DOI registered: 2020-07-16

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Keyword(s):
different normalizers; RPI calculation
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: 10.600 m
Event(s):
Suettoe * Latitude: 47.738000 * Longitude: 18.448000 * Location: Hungary * Comment: LPSS-profile outcropping at Hegyhati quarry (Süttö)
Comment:
Fig. 6. RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and ARM (bottom), “S”IRM (middle) and bulk susceptibility Klf (top) as normalisers, respectively. The depth section between 3 and 6.5 m was re-sampled in 2009 to better describe the behaviour of the EMF in this depth/time interval.
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1CommentCommentRolf, Christian
2DEPTH, sediment/rockDepth sedmRolf, ChristianGeocode
3Relative paleointensity proxyRPIRolf, ChristianRPI15/ARM, norm Max
Size:
1510 data points

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