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On the role of Brownian motion in the control of detrital remanent magnetization of sediments

pure and applied geophysics, 1972
The field dependence of magnetic remanence in laboratory deposited sediments is re-examined in terms of the average orientation of small grains of magnetite subject to the combined effect of an aligning field and thermal agitation. The classical (Langevin) formula for paramagnetic susceptibility is generalized to describe an assembly of grains with ...
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