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- W2030699461 abstract "1½m cores of fine grained organic lake sediments gradually redeposited over a period of 9 months accurately track the direction of the ambient magnetic field. Inclination errors are not significant and the delay between deposition and acquisition of a stable remanence is less than 2 days. Only a small degree of post-depositional grain reorientation occurs after this interval. The newly formed deposits are sufficiently cohesive to be subsampled without recourse to forced compaction and retain a stable remanence with water contents as high as 90% by volume (∼85% by weight). Use of the results to calibrate the simple relative paleointensity estimate Q = NRM/susceptibility for the natural sediments can lead to variable results even in similar sequences where the NRM is a DRM." @default.
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- W2030699461 date "1979-04-01" @default.
- W2030699461 modified "2023-10-17" @default.
- W2030699461 title "Detrital remanent magnetisation in five slowly redeposited long cores of sediment" @default.
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- W2030699461 doi "https://doi.org/10.1029/gl006i004p00229" @default.
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