1 Ocak 2011 Dergi makalesi Açık Erişim

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

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        "name": "Bouchon, Michel"
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      {
        "name": "Karabulut, Hayrullah"
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      {
        "name": "Aktar, Mustafa"
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      {
        "affiliation": "Marmara Res Ctr, Earth & Marine Sci Inst, TUBITAK, TR-41470 Gebze, Kocaeli, Turkey", 
        "name": "Ozalaybey, Serdar"
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      {
        "name": "Schmittbuhl, Jean"
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    "description": "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.", 
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    "journal": {
      "issue": "6019", 
      "pages": "877-880", 
      "title": "SCIENCE", 
      "volume": "331"
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    "publication_date": "2011-01-01", 
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    "title": "Extended Nucleation of the 1999 M-w 7.6 Izmit Earthquake"
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