Geological structure of karst stratigraphical windows at Škocjan Caves, Slovenia

Research at Škocjan Caves, Slovenia, introduces the concept of 'karst stratigraphical windows' to describe surface exposures of older carbonate strata due to karst processes and collapse dolines. This discovery highlights how detailed geological mapping in karst areas can uncover hidden stratigraphic boundaries, providing deeper insights into subsurface structures. Unlike tectonic windows, these features arise from karst erosion and doline formation, offering a new perspective on understanding geological layers in regions with limited outcrops. The study emphasizes the importance of examining collapse dolines during surface mapping to enhance the comprehensiveness of geological data.

Šebela, S., & Novak, U. (2023). Geological structure of karst stratigraphical windows at Škocjan Caves, Slovenia. SN Applied Sciences, 5(4). https://doi.org/10.1007/s42452-023-05330-x