Abstract
The paper presents investigation on diagenesis of Muschelkalk carbonates in the 25-BN Biskupice borehole, NE part of the Silesian-Cracow region. A cycle of dissolution and neomorphic alterations has been identified in the dolomites, Fe-dolomites and calcites occurring at the medium and late stages of diagenesis based on the analytical results of petrographic, cathodoluminescence and SEM methods.
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