Fig. 6 (middle) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and "S"IRM
Fuente:
PANGAEA
Guardado en:
| Autores principales: | Rolf, Christian, Hambach, Ulrich, Novothny, Ágnes, Horváth, Erzsébet, Schnepp, Elisabeth |
|---|---|
| Formato: | Dataset Open Access |
| Lenguaje: | en |
| Publicado: |
PANGAEA
2020
|
| Materias: | |
| Acceso en línea: | |
| Etiquetas: |
Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
|
Ejemplares similares
Fig. 6 (bottom) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and ARM
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 6 (top) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and bulk susceptibility Klf
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 5 Süttö Hungary RPI normalisers by Klf, ARM and IRM@2000 mT show no correlation
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 8 (all in one sort depth) 8 RPI Süttö compared to Glopis and Piso data
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 8 RPI Süttö compared to Glopis and Piso data
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 7 data correlation susc at LPSS Süttö, tuned susc Chinese Loess Plateau and global ice volume (only susc. data Süttö)
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
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)
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (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)
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Fig. 4 Scatter plots of Klf vs. Kfd and Klf vs. KARM. Dating Last Glacial loess sequence by RPI: Middle Danube Basin (Süttö, Hungary)
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Susceptibility values of high resolution magnetic susceptibility record of the (penultimate and) last glacial cycles at the Süttő loess section, in Hungary 2009
por: Novothny, Ágnes, et al.
Publicado: (2020)
por: Novothny, Ágnes, et al.
Publicado: (2020)
Susceptibility values of high resolution magnetic susceptibility record of the (penultimate and) last glacial cycles at the Süttő loess section, in Hungary in 2008
por: Novothny, Ágnes, et al.
Publicado: (2020)
por: Novothny, Ágnes, et al.
Publicado: (2020)
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)
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Relative paleointensity (RPI) of the Earth's magnetic field of sediment core PS69/899-2
por: Fripiat, François, et al.
Publicado: (2026)
por: Fripiat, François, et al.
Publicado: (2026)
Holocene paleomagnetic data (inclination, declination, relative paleointensity and virtual geomagnetic pole positions) from three marine sediment cores collected on the North East Greenland Shelf during Expedition NorthGreen2017
por: Girard, Juliette, et al.
Publicado: (2026)
por: Girard, Juliette, et al.
Publicado: (2026)
Paleomagnetic and rock magnetic data of SO202-33-4, North Pacific
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Age model, d18O, declination, inclination, MAD and RPI from ODP Site 172-1063, Bermuda Rise
por: Channell, James E T, et al.
Publicado: (2020)
por: Channell, James E T, et al.
Publicado: (2020)
Paleomagnetic data (inclination, declination and relative paleointensity) from marine sediment core DA17-NG-ST03-039G collected on the North East Greenland Shelf
por: Girard, Juliette, et al.
Publicado: (2026)
por: Girard, Juliette, et al.
Publicado: (2026)
Antarctic relative palaeointensity stack (ANT-1600)
por: Hopkins, Becky, et al.
Publicado: (2024)
por: Hopkins, Becky, et al.
Publicado: (2024)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1305C at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1305B at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1305A at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1306B at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1304A at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1304B at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of IODP Hole 303-U1304D at the Matuyama-Brunhes boundary
por: Channell, James E T
Publicado: (2020)
por: Channell, James E T
Publicado: (2020)
Paleomagnetic and mineral magnetic data of the loess paleosol record Balta Alba Kurgan, Romania
por: Scheidt, Stephanie, et al.
Publicado: (2020)
por: Scheidt, Stephanie, et al.
Publicado: (2020)
XRF, carbon and CaCO3 data from the loess-paleosol sequence Süttö, Hungary
por: Profe, Jörn, et al.
Publicado: (2017)
por: Profe, Jörn, et al.
Publicado: (2017)
Relative paleointensity (RPI) slopes of sediment core SO264_22-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Relative paleointensity (RPI) slopes of sediment core SO264_19-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Relative paleointensity (RPI) slopes of sediment core SO264_56-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Paleomagnetic data (inclination, declination and relative paleointensity) from marine sediment core DA17-NG-ST18-213G collected on the North East Greenland Shelf
por: Girard, Juliette, et al.
Publicado: (2026)
por: Girard, Juliette, et al.
Publicado: (2026)
Rock- and palaeomagnetic investigations of an Upper Pleistocene loess–palaeosol sequence near Süttő, Hungary
por: Rolf, Christian, et al.
Publicado: (2020)
por: Rolf, Christian, et al.
Publicado: (2020)
Paleointensity of ODP Site 162-980
por: Channell, James E T, et al.
Publicado: (2013)
por: Channell, James E T, et al.
Publicado: (2013)
Paleointensity of ODP Site 162-983
por: Channell, James E T, et al.
Publicado: (2013)
por: Channell, James E T, et al.
Publicado: (2013)
Paleointensity of ODP Site 162-984
por: Channell, James E T, et al.
Publicado: (2013)
por: Channell, James E T, et al.
Publicado: (2013)
Age-depth model of sediment core SO264_22-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Age-depth model of sediment core SO264_56-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Age-depth model of sediment core SO264_19-2
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Paleomagnetic data (inclination, declination, relative paleointensity and virtual geomagnetic pole positions) from marine sediment core DA17-NG-ST07-073G collected on the North East Greenland Shelf
por: Girard, Juliette, et al.
Publicado: (2026)
por: Girard, Juliette, et al.
Publicado: (2026)
Relative paleointensity (RPI) slopes of sediment core SO202/1_33-4
por: Wang, Wanzhang, et al.
Publicado: (2022)
por: Wang, Wanzhang, et al.
Publicado: (2022)
Ejemplares similares
-
Fig. 6 (bottom) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and ARM
por: Rolf, Christian, et al.
Publicado: (2020) -
Fig. 6 (top) RPI records calculated using the intensity of magnetisation after demagnetisation at 15 mT and bulk susceptibility Klf
por: Rolf, Christian, et al.
Publicado: (2020) -
Fig. 5 Süttö Hungary RPI normalisers by Klf, ARM and IRM@2000 mT show no correlation
por: Rolf, Christian, et al.
Publicado: (2020) -
Fig. 8 (all in one sort depth) 8 RPI Süttö compared to Glopis and Piso data
por: Rolf, Christian, et al.
Publicado: (2020) -
Fig. 8 RPI Süttö compared to Glopis and Piso data
por: Rolf, Christian, et al.
Publicado: (2020)