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• W2081672583 abstract "Experimental data may be compatible with the hypothesis that a single direction of magnetic remanence rotates as a rigid marker with strains up to 40% shortening in coaxial, perfect flattening (X = Y >Z). Detailed agreement with the passive line model is relatively poor for the specimens in which remanance is carried by magnetite. However, for this range of strains the differences with the passive line model (Wettstein's equation) are so slight that the latter model may be more easily employed to de-strain or restore deformed remanance to its original attitude. In the case of hematite-bearing remanences, the differences between the passive line and rigid marker model are even smaller because of the higher aspect ratios of grains of hematite. Therefore it is suggested that Wettstein's equation may be safely used to restore remanence after even higher strains, where the remanence is carried by hematite." @default.
• W2081672583 created "2016-06-24" @default.
• W2081672583 creator A5079003914 @default.
• W2081672583 date "1993-03-01" @default.
• W2081672583 modified "2023-09-25" @default.
• W2081672583 title "Strain and magnetic remanence" @default.
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• W2081672583 doi "https://doi.org/10.1016/0191-8141(93)90134-v" @default.
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