Abstract
The increasing importance of sediments for paleomagnetic research prompted a study of rockmagnetic parameters of natural goethite, pyrrhotite and hematite. Grain-size dependent behaviour of such parameters is poorly known for goethite and pyrrhotite as well as for fine-grained hematite. Data of hematite indicate a complex rockmagnetic behaviour. Existing data seem to be contradictory in many aspects. The rockmagnetic parameters reported in the present thesis for the natural goethite and pyrrhotite samples comprise twelve grain-size fractions from 250 micrometer down to <5 micrometer. For the natural hematite sample, which has a low-temperature origin, the <5 micrometer fraction was divided into six grain-size fractions down to <0.25 micrometer.
Original language | English |
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Qualification | Doctor of Philosophy |
Awarding Institution |
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Award date | 27 Jan 1988 |
Place of Publication | Utrecht |
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Publication status | Published - 27 Jan 1988 |