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Relative paleointensity and environmental magnetics for IODP Site 303-U1307
Relative paleointensity (RPI; NRM/ARM) for the 20-50 mT demagnetization interval, magnetic susceptibility (κ) and magnetic grain size (κARM/κ) u-channel data, measured every... -
Paleointensity of two sediment cores from the north of the South China Sea
This dataset has no description
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Dole effect in the north of the South China Sea from sediment core PC27 and PC83
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM.Dole effect was... -
Stacked dole effect in the north of the South China Sea from sediment core PC...
Relative intensity proxy (RPI) be constructed using the equation: RPI=NRM/SIRM (20-60)mT * MDFSIRM-CM/MDFSIRM, where MDFSIRM-CM is the center of mass of MDFSIRM -
Relative paleointensity proxy of sediment core JR298-PC726
This dataset has no description
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Relative paleointensity proxy of sediment core JR298-PC728
This dataset has no description
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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 palaeointensity stack of IODP Site 379-U1533
Relative palaeointensity analyses for IODP Site 379-U1533, completed in 2020-2022 at the University of Southampton. Three methods shown: natural remanent magnetisation (NRM)... -
Antarctic relative palaeointensity stack (ANT-1600)
Relative palaeointensity (RPI) stack calculated by interpolating nine published RPI records with IODP Site 379-U1533, and 90% confidence interval of resulting stack. Site IODP... -
Rock and paleomagneitc measurements of PS67/197-1
The core was taken in 2005 during Polarstern cruise ANT-XXII/4 in the central Scotia Sea. Magnetic susceptibility, further paleomagnetic information and other proxies were... -
Palaeomagnetic intensity of sediment core PS75/190-3
This dataset has no description