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  • Macromorphologically, the study area in Pannonian Croatia is basically a mountain-and-basin region. Geologically, it is on the W border of the Pannonian Basin, in contact with Forealpian structures. Special importance is rendered to tectonic
  • movements in the origin of geological and geomorphological features. Various types of structures have been selected for study and recognised as particular types of morphostructure. Examples of relief properties suggest a relationship between orography
  • , geological structure and faults. The consequences of extension, compression and transgression, especially along transcurrent faults are investigated.