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   <subfield code="u">Department of Geophysics, Faculty of Mathematics and Physics, Comenius University, Bratislava</subfield>
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   <subfield code="a">Investigation of the possibility to determine the palaeointensity of the thermoremanently magnetised synthetic magnetite by the method of anhysteretic magnetising</subfield>
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   <subfield code="c">[Peter Vajda]</subfield>
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   <subfield code="a">Summary: Determination of palaeointensity using the method of anhysteretic magnetising is reported. It is based on the study of the synthetic magnetite of three fractions which was thermoremanently magnetised in a known laboratory field. The experimental data of the anhysteretic magnetisation were treated using cubic splines. A method of determining the palaeointensity from the behaviour of the anhysteretic magnetisation curve is described while using a designed methodology of three types of regimes of the anhysteretic magnetising process. A way of investigating the palaeointensity of a natural rock sample by the method of anhysteretic magnetising is suggested.</subfield>
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