A theoretical treatment of paleointensity determination experiments on rocks containing pseudo-single or multi domain magnetic particles

Mathematics – Logic

Scientific paper

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Scientific paper

A phenomenological theory of thermoremanent magnetization (TRM) is applied to model the possible results of paleointensity determination experiments using the Thellier method. It is shown that intrinsic curvature of the Arai plot for samples containing pseudo-single or multi domain particles can be attributed exclusively to the presence of remanences which are unblocked below their blocking temperature. Thus the thermal demagnetization tail of partial TRM (pTRM) is not a direct measure for a sample's tendency to yield a curved Arai plot. Here it is proposed to use the advancing decay of a pTRM(T1, T2) which during heating occurs already below the lower temperature T1

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