Dataset - B2FIND

Paleomagnetic data (inclination, declination and relative paleointensity) fro...

We present paleomagnetic data (inclination, declination, relative paleointensity) of marine sediment core DA17-NG-ST18-213G collected on the North East Greenland Shelf during...

Paleomagnetic data (inclination, declination, relative paleointensity and vir...

We present paleomagnetic data (inclination, declination, relative paleointensity, virtual geomagnetic pole positions VGP) of marine sediment core DA17-NG-ST07-073G collected on...

Paleomagnetic data (inclination, declination and relative paleointensity) fro...

We present paleomagnetic data (inclination, declination, relative paleointensity) of marine sediment core DA17-NG-ST03-039G collected on the North East Greenland Shelf during...

Paleomagnetic data (inclination, declination, relative paleointensity) in sed...

This dataset contains paleomagnetic data (inclination, declination, relative paleointensity) of core AMD1902-10GC. This core was collected in Petermann Fjord (Nares Strait,...

Updated paleomagnetic Petermann stack (inclination, declination, relative pal...

This paleomagnetic stack was built using cores AMD1902-10GC (data available in PANGAEA, Girard et al., 2024), cores OD1507-04GC, OD1507-41GC, OD1507-40TC (data available in...

Paleosecular geomagnetic variation for the Holocene measured from U-channels ...

Inclination, declination, and relative palaeointensity calculated as a composite (WINPSV-12K) of four sediment cores (+54-03/57PC, +54-03/64PC, +54-03/67PC, +54-03/68PC) from...

High-resolution paleomagnetic secular variation and relative paleointensity s...

This dataset has no description

Magnetic record of Site 152-919

This dataset has no description

Palaeomagnetic investigation of sediment core HLY0501-01JPC from the Chukchi-...

Age was erroneously given in thousands of ka instead of ka, recalculated to ka on 2019-01-30.

Fig. 5 Süttö Hungary RPI normalisers by Klf, ARM and IRM@2000 mT show no corr...

Establishing of appropriate normalisers for the determination of relative palaeointensities, remanences measured after a peak AF treatment of 15 mT were normalised by Klf, ARM...

Fig. 6 (bottom) RPI records calculated using the intensity of magnetisation a...

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...

Fig. 6 (middle) RPI records calculated using the intensity of magnetisation a...

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...

Fig. 6 (top) RPI records calculated using the intensity of magnetisation afte...

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...

Fig. 8 (all in one sort depth) 8 RPI Süttö compared to Glopis and Piso data

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...