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CRM: Kemisk Remanent Magnetisering er den magnetisering, som opstår, når et magnetisk mineral af kemisk vej ændres. 1967: The intensity of the ancient geomagnetis field: A review and analysis.

DRM: Detrital Remanent Magnetisering - er den magnetisering, som opstår i et blødt sediment, når magnetiske korn aflejres.

Methods, which attempt to improve the Thellier method, are briefly described. One group reduces the number of heatings, the other avoids heatings by substituting ARM for TRM.

Da disse bidrag er af størrelsesorden 1% eller mindre og med korte variationsperioder, ses der bort fra disse i en geologisk sammenhæng.

The classic method for palaeointensity determination is Thellier's method.

Unfortunately this method is slow and requires many heatings, which might alter the sample.

DRM or CRM, on the assumption that a satisfactory artificial method of remagnetization can be found.

Finn Nørgaard Svendsen, Laboratoriet for Geofysik, Geologisk Institut, Finlandsgade 6, DK-8200 Århus N, 21. 1974: Lunar magnetic field palaeointensities determined by an ARM method.

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Et påsat index refererer til oprindelsen af remanensen. Symbolet anvendes også for specifik magnetisering, som er remanent magnetisering pr. For ikke-sedimentære bjergarter er den hyppigste remanens af termisk oprindelse (TRM) opstået ved afkøling fra en smelte eller metamorf proces. 1974: A new method of determining the magnitude of palaeomagnetic field.

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