Imaging crustal structures through a passive seismic imaging approach in a mining area in Saxony, Germany

• Published in: Solid earth (Göttingen) 2021-11, Vol.12 (12), p.2703-2715
• Main Authors: Hassani, Hossein, HlouÅ¡ek, Felix, Buske, Stefan, Wallner, Olaf
• Format: Article
• Language: English
• Subjects: Abandoned mines; Active control; Crust; Earth; Earth science; Earthquakes; Fault lines; Fault zones; Flooding; Floods; Geological faults; Geological structures; Geology; Geothermal power; Hydrocarbons; Imaging techniques; Localization; Microseisms; Mineral industry; Mining; Mining industry; P waves; Passive imaging; Reflectors; Seismic activity; Seismic surveys; Seismic tomography; Surveying; Three dimensional models; Uranium; Waveforms
• ISSN: 1869-9529; 1869-9510; 1869-9529
• DOI: 10.5194/se-12-2703-2021

We have used several flooding-induced microseismic events that occurred in an abandoned mining area to image geological structures close to the hypocentres in the vicinity of the mine. The events have been located using a migration-based localization approach. We used the recorded full waveforms of these localized microseismic events and have processed these passive source data as if they resulted from active sources at the known hypocentre location and origin time defined by the applied location approach. The imaging was then performed using a focusing 3D prestack depth migration approach for the secondary P-wave arrivals. The needed 3D migration velocity model was taken from a recent 3D active (controlled-source) seismic survey in that area. We observed several clear and pronounced reflectors in our obtained 3D seismic image cube, some of them related to a major fault zone in that area and some correlating well with information from the nearby mining activities. We compared our results to the 3D seismic image cube obtained directly from the 3D active seismic survey and have found new structures with our approach that were not known yet, probably because of their steep dips which the 3D active seismic survey had not illuminated. The location of the hypocentres at depth with respect to the illumination angles of those structures proved to be favourable in that case, and our 3D passive image complements the 3D active seismic image in an elegant way, thereby revealing new structures that cannot be imaged otherwise with surface seismic configurations alone.