Number of the records: 1
Analysis of the 2016-2018 fluid-injection induced seismicity in the High Agri Valley (Southern Italy) from improved detections using template matching
- 1.0547485 - ÚSMH 2022 RIV DE eng J - Journal Article
Stabile, T.A. - Vlček, Josef - Wcislo, Milosz - Serlenga, V.
Analysis of the 2016-2018 fluid-injection induced seismicity in the High Agri Valley (Southern Italy) from improved detections using template matching.
Scientific Reports. Roč. 11, č. 1 (2021), č. článku 20630. ISSN 2045-2322. E-ISSN 2045-2322
Institutional support: RVO:67985891
Keywords : irpinia fault zone * earthquake location * magnitude * apennines * algorithm * reservoir * network
OECD category: Geology
Impact factor: 4.997, year: 2021
Method of publishing: Open access
Result website:
https://www.nature.com/articles/s41598-021-00047-6
DOI: https://doi.org/10.1038/s41598-021-00047-6
Improving the capability of seismic network to detect weak seismic events is one of the timeless challenges in seismology: the greater is the number of detected and locatable seismic events, the greater insights on the mechanisms responsible for seismic activation may be gained. Here we implement and apply a single-station template matching algorithm to detect events belonging to the fluid-injection induced seismicity cluster located in the High Agri Valley, Southern Italy, using the continuous seismic data stream of the closest station of the INSIEME network. To take into account the diversity of waveforms, albeit belonging to the same seismic cluster, eight different master templates were adopted. Afterwards, using all the stations of the network, we provide a seismic catalogue consisting of 196 located earthquakes, in the magnitude range 1.2 <= Ml <= 1.2, with a completeness magnitude Mc = 0.5 +/- 0.1. This rich seismic catalogue allows us to describe the damage zone of a SW dipping fault, characterized by a variety of fractures critically stressed in the dip range between similar to 45 degrees and similar to 75 degrees. The time-evolution of seismicity clearly shows seismic swarm distribution characteristics with many events of similar magnitude, and the seismicity well correlates with injection operational parameters (i.e. injected volumes and injection pressures).
Permanent Link: http://hdl.handle.net/11104/0324884
Number of the records: 1