Abstract
The first results of the petrophysical research (gamma-ray spectrometry, magnetic susceptibility, diffuse spectral reflectance) of the Devonian/Carboniferous boundary interval in the southern and middle part of the Moravian Karst demonstrate a good correlation potential of outcrop logging by gamma-ray spectrometry. This method allows us to correlate distinct petrophysical patterns through the different lithofacies developments (Horákov and Hostěnice facies), while magnetic susceptibility and diffuse spectral reflectance failed to show correlatable patterns. The most prominent petrophysical patterns at the sections can be correlated with the polyphase Hangenberg Event.
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