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- W2058889631 abstract "Thermomagnetic analyses of red bed samples from the Precambrian in England and the Paleozoic in eastern Canada show that a significant amount of magnetite is generated if these samples are heated either in partial vacuum or in nitrogen. However, only a very small amount of magnetite usually is generated if the analyses are carried out in air of atmospheric pressure and subsequently in partial vacuum. In that case, one of the essential ingredients aparently is inactivated at a temperature below that (about 400°C) at which magnetite production becomes noticeable on the time scale of the experiments. In the thermal demagnetization of red bed samples for paleomagnetic purposes the formation of magnetite must be avoided, and this can almost the achieved by heating the samples in air of atmospheric pressure. Hematite may also be formed at higher temperatures but this is probably not serious. The shape of the NRM decay curves obtained by heating the samples in air cannot be associated with either the occurrence of magnetochemical changes at higher temperatures or the presence of minerals with Curie points above 20°C other than hematite and, in some cases, magnetite." @default.
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- W2058889631 date "1968-01-01" @default.
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- W2058889631 title "Thermomagnetic analysis of some red beds" @default.
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- W2058889631 doi "https://doi.org/10.1016/s0012-821x(68)80061-5" @default.
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