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Analysis of the 2016-2018 fluid-injection induced seismicity in the High Agri Valley (Southern Italy) from improved detections using template matching
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SYSNO ASEP 0547485 Document Type J - Journal Article R&D Document Type Journal Article Subsidiary J Článek ve WOS Title Analysis of the 2016-2018 fluid-injection induced seismicity in the High Agri Valley (Southern Italy) from improved detections using template matching Author(s) Stabile, T.A. (IT)
Vlček, Josef (USMH-B) ORCID, RID
Wcislo, Milosz (USMH-B) RID, ORCID
Serlenga, V. (IT)Number of authors 4 Article number 20630 Source Title Scientific Reports. - : Nature Publishing Group - ISSN 2045-2322
Roč. 11, č. 1 (2021)Number of pages 13 s. Language eng - English Country DE - Germany Keywords irpinia fault zone ; earthquake location ; magnitude ; apennines ; algorithm ; reservoir ; network Subject RIV DC - Siesmology, Volcanology, Earth Structure OECD category Geology Method of publishing Open access Institutional support USMH-B - RVO:67985891 UT WOS 000709050100025 DOI 10.1038/s41598-021-00047-6 Annotation 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). Workplace Institute of Rock Structure and Mechanics Contact Iva Švihálková, svihalkova@irsm.cas.cz, Tel.: 266 009 216 Year of Publishing 2022 Electronic address https://www.nature.com/articles/s41598-021-00047-6
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