A statistical simulation of magnetic particle alignment in sediments
Sedimentary magnetizations are fundamental to palaeomagnetism, but the mechanisms that control remanence acquisition remain poorly constrained. Observed sedimentary natural remanent magnetizations are often orders of magnitude smaller than the saturation
|Collections||ANU Research Publications|
|Source:||Geophysical Journal International|
|01_Heslop_A_statistical_simulation_of_2014.pdf||1.73 MB||Adobe PDF|
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