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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...
