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Geomagnetic Field and Radiocarbon Activity Through Holocene Time

  • Creer K
Springer Netherlands, (1988), 381-397
DOI: 10.1007/978-94-009-3011-7_24
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Abstract

The properties of baked clays and lake sediments as recorders of geomagnetic variations through pre-historic times are compared. Archaeomagnetism has provided a substantial body of intensity data but few directional data while lake sediment palaeomagnetism has provided continuous, smoothed records of direction but no reliable intensities.

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Creer, K. M. (1988). Geomagnetic Field and Radiocarbon Activity Through Holocene Time. In Secular Solar and Geomagnetic Variations in the Last 10,000 Years (pp. 381–397). Springer Netherlands. https://doi.org/10.1007/978-94-009-3011-7_24

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