摘要
In this paper,the authors measured the magnetic parameters,grain size and XRD for four dry mud samples,which were taken from Lake Chiemsee,Bavaria of Germany.The results of low-temperature saturation remanence show clear Verwey transition,suggesting presence of multi-domain (MD) magnetite in the samples.That coarse size is out range of reported magnetosomes.That was also detected by particle size measurements showing a few peaks for the distribution curves.Some coarser sands and aeolian deposit around the lake would be possibly washed down to the lake by surface water flow.The multi-domain magnetite measured in the samples could be within these coarser sediments.