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| Titel |
Crustal stress, seismicity, acoustic emission (AE), and tectonics: the Kefallinìa (Greece) case study |
| VerfasserIn |
G. P. Gregori, M. Poscolieri, G. Paparo, G. Ventrice, S. De Simone, C. Rafanelli |
| Konferenz |
EGU General Assembly 2009
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| Medientyp |
Artikel
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| Sprache |
Englisch
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| Digitales Dokument |
PDF |
| Erschienen |
In: GRA - Volume 11 (2009) |
| Datensatznummer |
250026148
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| Zusammenfassung |
| New inferences - confirming previous results (see references)- are presented dealing with a few years Acoustic Emission (AE) records collected at Kefallinìa (Ionian Islands, Greece). A physical distinction between HF (high frequency) vs. LF (low frequency) AE is required. Step-wise changes of the AE underground conductivity are evidenced, and can be suitably handled. “Smooth” results concern (i) the annual variation, (ii) some long-lasting stress “solitons” crossing through the area, and (iii) tidal effects. In particular, every AE station can be operated like a monitoring station both for Earth’s tides and for the free oscillations of the Earth. In addition, Kefallinìa exhibits a much peculiar groundwater circulation, in which conduit flow is dominant, that originates a specific (and unique) AE effect. By means of AE time-series analysis, “extreme” or “catastrophic” events can be also monitored and possibly related to relevant tectonic occurrences (either earthquakes, or maybe other occasional phenomena). They can be investigated, and have a regional - rather than local - character. Therefore, every interpretation based on a single station record - being biased by some arbitrariness - can only result indicative. A standardized procedure and software is proposed for routine AE data handling and analysis.
References.:
Lagios et al., 2004. In Proc. SCI 2004 (The 8th World Multi-Conference on Systemics, Cybernetics and Informatic), Orlando, Florida, July 1004, 6 pp.
Poscolieri et al., 2006. In. G. Cello and B. D. Malamud, (eds), 2006. Geol. Soc. London, Special Publ., 261, 63-78.
Poscolieri et al., 2006a. Nat. Hazards Earth Syst. Sci., 6, 961-971. |
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