Journal
GEOPHYSICAL RESEARCH LETTERS
Volume 41, Issue 17, Pages 6137-6144Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1002/2014GL061199
Keywords
2009 L'Aquila earthquake; foreshock sequence; cross-correlation matched filter technique
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Funding
- executive program of scientific and technological cooperation between Italy and Japan
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We explored the detection capability of low-magnitude earthquakes before the 6 April 2009 M-w 6.3L'Aquila event by using a matched filter technique and 512 foreshocks as templates. We analyzed continuous waveforms from 10 broadband seismic stations in a 60km radius from the epicenter and for similar to 3months before the main shock. More than 3000 new events, mostly located on the main shock fault, were detected to define the spatial-temporal evolution of micro-seismicity. The foreshock sequence was active northwest of the M-w 6.3 hypocenter in January, then migrated toward it at a speed of similar to 0.5km/day in middle of February. At that time, in a similar to 4km(2) patch close to the main shock nucleation point, the cumulative number of earthquakes gradually increased until the M-w 6.3 event. This patch, characterized by a low b-value, played a key role in controlling the preparation stage to the 2009L'Aquila main rupture.
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