The fracture-controlled carbonate Brejoes Karst System mapped with UAV, LiDAR, and electroresistivity in the Irece Basin - Brazil

Understanding how fractures influence fluid flow in carbonate rocks is essential to understanding karst evolution, oil reservoirs, and aquifer exploitation. The present study investigates karst fracture geometry at the surface and subsurface in the Irece Basin, a Neoproterozoic epicontinental cratonic basin in the Sao Francisco Craton, Brazil. We used an Unmanned Aerial Vehicle (UAV) to map both fractures in three outcrops and valley geometries, Light Detection And Ranging (LiDAR) to map 3500 m of cave conduits, and Electrical Resistivity Tomography (ERT) to identify karst zones between 90 and 110 m deep. Our results indicate that the Brejoes Karst System is comprised of dissolution and collapse features such as caves, dolines, pavements, and karst valley. The quantitative analysis of subseismic fractures (< 50 m long) identified 4398 fractures in Outcrop A, 2458 in Outcrop B, 4374 in Outcrop C, and 7172 in 18 cross-sections of the Brejoes Cave. These fractures form a corridor with four main sets striking N-S, NNE-SSW, NW-SE, and E-W, where the fracture system is essential to cave connectivity, permeability, and development. The highest frequency of fractures coincides with the main cave axes, where the intersection of the fracture/fault are sites prone to dissolution. The ERT profiles indicated a high density of geophysical anomalies that correspond to enlarged fractures in the epikarstic zone that extend between the surface and approximately 30 m deep. The cave infill impacts the cave characterization and leads to underestimating cave dimensions. This study may contribute to an underestimation of the role played by subseismic scale fractures in karst evolution in gently deformed settings.

Automated summary

Understanding how fractures influence fluid flow in carbonate rocks is crucial for understanding karst evolution, oil reservoirs, and aquifer exploitation. This study investigates the geometry of karst fractures in the Irece Basin, Brazil using UAV, LiDAR, and ERT techniques. The results highlight the importance of fracture systems in cave connectivity, permeability, and development.