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- W2130206616 abstract "The angular probability distribution generated by adding a set of randomly oriented vectors to a set of constant parallel vectors has been studied. If one random vector of constant length is added to each constant vector, the resultant angular probability distribution departs widely from the distribution used by Fisher as the basis for palaeomagnetic analysis. However, if n random vectors of equal length are added to each constant vector and if n > 6, the resulting angular probability distribution is nearly identical to that proposed by Fisher over most of the range of angular dispersions encountered in palaeomagnetic investigations. Equations are developed from which the mean intensity of random magnetization can be calculated, given the mean total intensity and the angular dispersion. These parameters, in turn, are related to the ratio of random to non-random magnetization for each ferromagnetic mineral grain in a rock specimen." @default.
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- W2130206616 date "1964-05-01" @default.
- W2130206616 modified "2023-09-26" @default.
- W2130206616 title "Angular Dispersion Due to Random Magnetization" @default.
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- W2130206616 doi "https://doi.org/10.1111/j.1365-246x.1964.tb03856.x" @default.
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