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Eifelian dolomites in the Zachełmie Quarry exhibit metre-scale depositional cyclicity, both in the lower, lagoonal part of the section and in the upper, shallow subtidal portion. Magnetic properties were studied in 30 samples (at c. 1 m intervals), including magnetic susceptibility (MS) and anhysteretic and isothermal remanent magnetization. The rock magnetic parameters are compared with the results of thin-section study and elemental chemistry. The forcing factors driving the MS pattern are identified. The MS signal is mostly related to a finely dispersed hematite, controlled by terrigenous input. Magnetite plays a subordinate role and it is confined to less terrigenous...

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