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On the recent seismic activity in North-Eastern Aegean Sea including the M(w)5.8 earthquake on 8 January 2013
In the last week of November 2012, we announced that a strong electrotelluric disturbance, which we judged to be a Seismic Electric Signal (SES) activity, was recorded at station Assiros located in Northern Greece. This disturbance was actually followed by an M(w)5.8 earthquake on 8 January 2013 in...
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
The Japan Academy
2013
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Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3865358/ https://www.ncbi.nlm.nih.gov/pubmed/24213207 http://dx.doi.org/10.2183/pjab.89.438 |
Sumario: | In the last week of November 2012, we announced that a strong electrotelluric disturbance, which we judged to be a Seismic Electric Signal (SES) activity, was recorded at station Assiros located in Northern Greece. This disturbance was actually followed by an M(w)5.8 earthquake on 8 January 2013 in North-Eastern Aegean Sea. Here we show that, by analyzing this SES activity and employing the natural time analysis of subsequent seismicity, we estimated the epicentral location, magnitude and occurrence time which are reasonably compatible with those of the M(w)5.8 event. |
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