1 Ocak 2011 Dergi makalesi Açık Erişim

Bouchon, Michel; Karabulut, Hayrullah; Aktar, Mustafa; Ozalaybey, Serdar; Schmittbuhl, Jean; Bouin, Marie-Paule

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    <subfield code="a">Laboratory and theoretical studies suggest that earthquakes are preceded by a phase of developing slip instability in which the fault slips slowly before accelerating to dynamic rupture. We report here that one of the best-recorded large earthquakes to date, the 1999 moment magnitude (M-w) 7.6 Izmit (Turkey) earthquake, was preceded by a seismic signal of long duration that originated from the hypocenter. The signal consisted of a succession of repetitive seismic bursts, accelerating with time, and increased low-frequency seismic noise. These observations show that the earthquake was preceded for 44 minutes by a phase of slow slip occurring at the base of the brittle crust. This slip accelerated slowly initially, and then rapidly accelerated in the 2 minutes preceding the earthquake.</subfield>
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