Szczegóły publikacji
Opis bibliograficzny
Impact of mining-induced seismicity on land subsidence occurrence / Wojciech T. WITKOWSKI, Magdalena ŁUCKA, Artur GUZY, Henriette Sudhaus, Anna BARAŃSKA, Ryszard HEJMANOWSKI // Remote Sensing of Environment ; ISSN 0034-4257. — 2024 — vol. 301 art. no. 113934, s. 1–15. — Bibliogr. s. 14–15, Abstr. — Publikacja dostępna online od: 2023-12-05
Autorzy (6)
Słowa kluczowe
Dane bibliometryczne
| ID BaDAP | 150847 |
|---|---|
| Data dodania do BaDAP | 2023-12-13 |
| Tekst źródłowy | URL |
| DOI | 10.1016/j.rse.2023.113934 |
| Rok publikacji | 2024 |
| Typ publikacji | artykuł w czasopiśmie |
| Otwarty dostęp |  |
| Creative Commons | |
| Czasopismo/seria | Remote Sensing of Environment |
Abstract
Mining-induced seismicity can damage buildings and surface infrastructure and cause fatalities. It is a growing concern, owing to the sudden occurrence of seismic events, lack of effective prediction capabilities, and associated consequences. In this study, we analyzed 13 high-energy mining-induced earthquakes from 2016 to 2020 in Poland's Legnica-Glogow Copper District (LGCD), based on data recorded by the Induced Seismicity-European Plate Observing System (IS-EPOS). We used European Space Agency (ESA) Sentinel-1 Copernicus satellite radar images, to study the co-seismic subsidence in the region. Additionally, we employed volumetric point source approximation and a Bayesian inverse modeling scheme to estimate the location and strength of subsurface collapses from the land subsidence data. Finally, we correlated the geological constraints with the land subsidence and earthquake source parameters. The interferometric synthetic aperture radar (InSAR) displacement maps portrayed maximum line-of-sight (LOS) displacements of −144 mm and − 124 mm in ascending and descending images, respectively, with maximum land subsidence reaching −142 mm. Notably, only a few earthquakes with large magnitudes caused land subsidence. There was a significant correlation between earthquake magnitude and land subsidence; the greater the thickness of the loose Quaternary strata, the smaller the land subsidence. According to the inversion results, the focal depths of the collapses associated with the earthquakes were 437–669 m. However, the estimated collapse depths were situated above the mining exploitation fields, within the rigid Triassic rock layers. The associated collapse energy was 1.62 times greater than the seismic energy, indicating aseismic deformation in the field. Additionally, we observed spatial discrepancy between the location of the earthquake epicenters and the maximum land subsidence. Thus, our study can improve the current understanding of the impact of mining-induced seismicity, the occurrence of associated land subsidence, and seismic mechanisms in mining areas.
