Application of seismic refraction methods for rock mass characterization at the lead mine tailings site in Olovo Mine

Authors

  • Ekrem Bektašević University of Tuzla, Faculty of Mining, Geology and Civil Engineering, Tuzla, Bosnia and Herzegovina; https://orcid.org/0000-0001-6742-966X
  • Krzysztof Skrzypkowski AGH University of Krakow, Faculty of Civil Engineering and Resource Management, Krakow, Poland; https://orcid.org/0000-0003-0819-2345
  • Semir Kahrimanović GEOMET Ltd., Olovo, Bosnia and Herzegovina
  • Luka Crnogorac University of Belgrade, Faculty of Mining and Geology, Belgrade, Serbia; https://orcid.org/0000-0002-9897-270X
  • Kemal Gutić University of Tuzla, Faculty of Mining, Geology and Civil Engineering, Tuzla, Bosnia and Herzegovina; https://orcid.org/0009-0008-9107-4641

DOI:

https://doi.org/10.7494/geol.2026.52.1.87

Keywords:

non-destructive methods, applied geophysics, seismic tomography, P-wave velocities

Abstract

In this study, the application of seismic refraction for the characterization of the rock mass at the lead mine tailings facility in Olovo is presented, with the aim of identifying lithostratigraphic horizons, structural discontinuities, and zones of reduced mechanical resistance that may affect tailings stability. The investigations were conducted along seven seismic profiles of varying lengths and resolutions, designed to cover both shallow and deeper portions of the rock mass to a depth of approximately 60 m. Data processing and interpretation were carried out using the Delta-t-V seismic tomography method, which enables reliable reconstruction of P-wave velocities even under conditions of complex geological structure and velocity inversions. The obtained results indicate pronounced heterogeneity of the rock mass, with clearly differentiated zones of surface embankments and unconsolidated materials (600–1,200 m/s), transitional zones of degraded and karstified rocks (1,800–3,200 m/s), and basal horizons of compact limestone, where P-wave velocities reach values of approximately 4,400 m/s. Particular attention was given to locally developed low-velocity anomalies within deeper horizons, interpreted as karst structures and cavernous zones that are potentially critical for tailings stability. By integrating the individual profiles, a unified 3D rock mass model was developed, enabling spatial analysis of anomalies and reliable terrain zoning. The results confirm that seismic refraction, combined with the Delta-t-V method, represents an efficient, non-destructive, and engineering-relevant tool for characterizing complex tailings rock masses. The developed models have direct application in stability assessment, remediation planning, and the enhancement of mining and environmental safety systems.

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2026-04-30

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How to Cite

Bektašević, E., Skrzypkowski, K., Kahrimanović, S., Crnogorac, L., & Gutić, K. (2026). Application of seismic refraction methods for rock mass characterization at the lead mine tailings site in Olovo Mine. Geology, Geophysics and Environment, 52(1), 87–102. https://doi.org/10.7494/geol.2026.52.1.87

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