Abstract
The influence of early diagenesis on the natural remanent magnetisation (NRM) in sediments from the Calabrian
ridge (Central Mediterranean) is analysed with the help of fuzzy c-means (FCM) cluster analysis and non-linear
mapping (NLM). The sediments are variably coloured: white, beige, purplish, greenish and grey layers occur with
occasionally intercalated sapropels. The NRM
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