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Magnetic susceptibility and Anhysteretic remanent magnetization in marine sed...
Magnetic measurements of U-channel samples were measured by the Bartington MS2 magnetic susceptibility system with an ASC auto-tracking rail and a cryogenic magnetometer (2G 755... -
Paleomagnetism in sediment core JC138-52GC from James Cook cruise JC138
Paleomagnetic data as mean deconvolute relative paleomagnetic intensity (after applying the deconvolution optimization with the UDECON software) in 52GC, as well as comparison... -
Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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Relative paleointensity (RPI) and virtual geomagnetic pole (VGP) latitude of ...
This dataset has no description
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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... -
Fig. 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... -
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... -
Relative paleointensity proxy of sediment core JR298-PC736
This dataset has no description
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Relative paleointensity proxy of sediment core JR298-PC732
This dataset has no description
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Relative paleointensity proxy of sediment core JR298-PC728
This dataset has no description