The 24 May 2014 (Mw6. 8) earthquake (North Aegean Trough): spatiotemporal evolution, source and slip model from teleseismic data
A Kiratzi, E Tsakiroudi, C Benetatos… - … of the Earth, Parts A/B/C, 2016 - Elsevier
We use teleseismic data to calculate the source model of the 24 May 2014 earthquake and
regional catalogues to examine the spatial-temporal characteristics of the sequence. The
sequence started in Saros Basin but almost simultaneously aftershocks spread along a∼
200 km zone, activating the entire North Aegean Trough. The aftershock sequence was rich
in moderate (M< 4) size events, but very deficient in strong events–only two Mw4. 9
aftershocks-a characteristic observed in previous sequences in the region. The teleseismic …
regional catalogues to examine the spatial-temporal characteristics of the sequence. The
sequence started in Saros Basin but almost simultaneously aftershocks spread along a∼
200 km zone, activating the entire North Aegean Trough. The aftershock sequence was rich
in moderate (M< 4) size events, but very deficient in strong events–only two Mw4. 9
aftershocks-a characteristic observed in previous sequences in the region. The teleseismic …
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