Investigating Dynamic Triggering of Seismicity by Regional Earthquakes: The Case of the Corinth Rift (Greece). Issue 21 (11th November 2017)

• Record Type: Journal Article
• Authors: De Barros, Louis; Deschamps, Anne; Sladen, Anthony; Lyon‐Caen, Hélène; Voulgaris, Nicholas
• Is Part Of: Geophysical research letters. Volume 44:Issue 21(2017)
• Page Start: 10, 921
• Page End: 10, 929
• Publication Date: 2017-11-11
• Subjects: dynamic triggering -- microseismicity -- regional earthquakes -- Corinth Rift; Geophysics -- Periodicals; Planets -- Periodicals; Lunar geology -- Periodicals; 550
• DOI: 10.1002/2017GL075460
• Languages: English
• ISSNs: 0094-8276

Abstract

Abstract: Dynamic triggering has been commonly observed after large teleseismic events, but the physics behind it is still under debate. To broaden observations, we here focus on the dynamic triggering by regional earthquakes, that is, by events with magnitude lower than 6.2 at distances smaller than 600 km. The western part of the Corinth Rift (Greece) is characterized by intense seismic swarms and is therefore adapted to study such responses. The microseismicity rates before and after the transient perturbations are high enough to analyze 30 regional earthquakes out of the 59 occurring in 2013. More than 40% of those 30 events, including earthquakes with magnitude as small as 4.5, are associated with a significant seismicity rate increase. The triggerability primarily depends on the amplitude of the seismic waves. However, triggering is mainly observed when the seismic perturbations are orthogonal to the faults, which suggests that fluid pressurization is likely involved. Key Points: Changes in the microseismicity rate after regional earthquakes are analyzed in the Corinth rift (Greece) Dynamic triggering is observed unambiguously after 20% of the regional earthquakes occurring in 2013 Dynamic triggering depends not only on the perturbation amplitude but also on its azimuth, suggesting that a fluid process is likely