Did the 7/9/1999 M5.9 Athens Earthquake Come with a Warning?

Andreas Tzanis and Konstantinos Makropoulos

Natural Hazards: Journal of the International Society for the Prevention and Mitigation of Natural Hazards, 2002, vol. 27, issue 1, 85-103

Abstract: Prior to the 7/9/1999 M S =5.9 Athens earthquake, regional seismicity has exhibited a power-law increase, of the form ΣΩ=K+A(t c - t) n , where Ω is estimated using an expression log Ω=cM + d and t c is the time of the culminating event. Such changes appeared after the 17/8/1999 M7.4 Izmit event. We quantified the performance of the power law vs. the null hypothesis of constant seismic release rates, by defining the curvature C as the ratio of the power law fit RMS/linear fit RMS, so that the smaller C is, the better the power law behaviour. By mapping C, we have established a critical radius of 110 km and observed that the region of correlated accelerating seismic release extended from the N. Aegean, through Euboea and Attica to the SW Peloponnese. A few days prior to the Athens event, min(C) was centred at the epicentral area and numerical simulation yielded t c =1999.676 and predicted M S =5.77. Seismicity rates returned to normal (quasi-constant) after the Athens event. We interpret this effect as critical point behaviour, following remote excitation of a broad area by stress redistribution due to the Izmit event which, at Athens, has triggered `premature' failure of a fault nearing its load bearing capacity. If this is correct, we have documented a case of remote earthquake triggering by another earthquake, as well as insight into the mechanisms producing it. As a corollary, we note that a large event may beget another large event in its broader region of interaction, which may be preceded by characteristic precursory seismicity changes. Copyright Kluwer Academic Publishers 2002

Date: 2002
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DOI: 10.1023/A:1019957228371

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