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• W2275323376 abstract "Seismicity in the area of Mygdonia basin (northern Greece) is lately characterizedby a lack of strong events (M≥5.0) on the seismogenic faults known to have beenrepeatedly activated in the past. Only small to moderate magnitude earthquakes(M≤4.8) have occurred since 2000 in the area. Therefore, microseismicity is the onlyavailable information to be exploited for the identification of active faults and hazardassessment, since it may occur everywhere, as well as onto the major hazardous faults.Earthquakes recorded between 2000 and 2014 by the Hellenic Seismological Networkwere relocated by using the available P- and S-seismic wave arrivals in order to improvelocation accuracy. The VP /VS velocity ratio which was found equal to 1.78, along withstation time delays, were all included in the Hypoinverse computer program. In thecase of strong spatial or temporal clustering the HypoDD algorithm was employedfor further improving location accuracy. The relocated seismicity was used to outlinethe geometrical properties of the local fault population and identify seismogenic faultsdeprived of a clear surface expression. Cross-sections made perpendicular to the mainaxis of the seismicity alignments, shed more light to the local fault network." @default.
• W2275323376 created "2016-06-24" @default.
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• W2275323376 date "2015-09-01" @default.
• W2275323376 modified "2023-09-23" @default.
• W2275323376 title "Fault population recognition through microseismicity in Mygdonia region (northern Greece)" @default.
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• W2275323376 doi "https://doi.org/10.4430/bgta0153" @default.
• W2275323376 hasPublicationYear "2015" @default.
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