Natural remanent magnetization, thermoremanent magnetization and reliability of palaeointensity determinations on H chondrites

Physics

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Scientific paper

We have compared the NRM and artificial TRM behaviour of several chondrites of type H. The palaeointensity measurements do not give a straight line but a curve with a high slope for the low temperature steps. The TRM intensity depends on the highest temperature reached by the sample. The magnetic viscosity is strongly dependent on the temperature with a drastic increase between 20°C and 95°C. The Fe-Ni alloys present in the meteorites probably show diffusion after effects. These experiments cast a strong doubt on previous palaeointensity determinations by the double step heating method.

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