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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. 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 (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. 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... -
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. -
Magnetic record of Site 152-919
This dataset has no description
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High-resolution paleomagnetic secular variation and relative paleointensity s...
This dataset has no description
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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...
