Fig. 3 (2009): Susc_Vol., Susc_freq; ARM; "SIRM"; against depth; Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttö, Hungary)

Ähnliche Einträge

• Fig. 3 (2008): Susc_Vol., Susc_freq; ARM; "SIRM"; against depth; Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttö, Hungary)
  von: Rolf, Christian, et al.
  Veröffentlicht: (2020)
• Fig. 3 (all in one): Susc_Vol., Susc_freq; ARM; "SIRM"; against depth; Dating of a Last Glacial loess sequence by relative geomagnetic palaeointensity: A case study from the Middle Danube Basin (Süttö, Hungary)
  von: Rolf, Christian, et al.
  Veröffentlicht: (2020)
• Fig. 5 Süttö Hungary RPI normalisers by Klf, ARM and IRM@2000 mT show no correlation
  von: Rolf, Christian, et al.
  Veröffentlicht: (2020)
• Thermal demagnetisation of paleosol sequence (SK LPS) from the Suhia Kladenetz loess
  von: Jordanova, Diana, et al.
  Veröffentlicht: (2022)
• (Figs. 4, 5 and 6) Saturation remanent magnetization (SIRM), anhysteretic remanent magnetization (ARM), natural remanent magnetization (NRM), ARM/NRM ratio and ARM/SIRM ratio of sediment core GeoB6007-2
  von: Bleil, Ulrich, et al.
  Veröffentlicht: (2010)