Selective post-depositional realignment in a synthetic sediment

Physics

Scientific paper

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Scientific paper

Synthetic sediments were deposited as slurries in controlled magnetic fields. After settling, the slurries were turned with respect to the field and dried. A small percentage of the remanet magnetization was associated with grains able to realign in the later field. These grains were the magnetically-hardest fraction. Routine alternating field demagnetization of sediments, usually assumed to remove the magnetic overprints, can thus in fact preferentially remove the earliest signal.

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