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Scheidt, Stephanie; Hambach, Ulrich; Rolf, Christian (2019): Specimen three-component IRM analysis from the Heidelberg Basin, Germany [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.901167, In supplement to: Scheidt, S et al. (2015): A consistent magnetic polarity stratigraphy of late Neogene to Quaternary fluvial sediments from the Heidelberg Basin (Germany): A new time frame for the Plio–Pleistocene palaeoclimatic evolution of the Rhine Basin. Global and Planetary Change, 127, 103-116, https://doi.org/10.1016/j.gloplacha.2015.01.004

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Keyword(s):
Fluvial sediment; Heidelberg Basin; Magnetic polarity stratigraphy; Magnetostratigraphy; Plio-Pleistocene; Rhine Basin; Upper Rhine Graben (URG)
Related to:
Scheidt, Stephanie; Egli, Ramon; Frederichs, Thomas; Hambach, Ulrich; Rolf, Christian (2019): A mineral magnetic characterization of Plio-Pleistocene sediment material from the Heidelberg Basin (Germany) [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.901920
Scheidt, Stephanie; Hambach, Ulrich; Hao, Qingzhen; Rolf, Christian; Wennrich, Volker (2019): Environmental signals of Pliocene-Pleistocene climatic changes in Central Europe: insights from the mineral magnetic record of the Heidelberg Basin sedimentary infill (Germany) [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.901371
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Sample IDSample IDScheidt, Stephanie
2Thermal demagnetization stepStep°CScheidt, Stephanie
3Isothermal remanent magnetization intensityIRM intensitymA/mScheidt, Stephanie
4IRM, Intensity after demagnetization along X-axisIRM Int XA/mScheidt, Stephaniesoft axis (0.12 T)
5IRM, Intensity after demagnetization along Y-axisIRM Int YA/mScheidt, Stephaniemedium axis (0.4 T)
6IRM, Intensity after demagnetization along Z-axisIRM Int ZA/mScheidt, Stephaniehard axis (2.7 T)
Size:
470 data points

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