EVIDENCE FOR INDUCED SEISMICITY FOLLOWING THE 2001 SKYROS MAINSHOCK

A.K. Adamaki, G. M. Tsaklidis, E. E. Papadimitriou, V. G Karakostas

Forskningsoutput: Kapitel i bok/rapport/Conference proceedingKonferenspaper i proceedingPeer review

Sammanfattning

Estimation of the seismicity rate changes caused by a major earthquake is based upon the assumption that the earthquake occurrence can be described by stochastic processes. Three stochastic models are applied to the data, i.e. the homogeneous Poisson model, the non-homogeneous Poisson model with two different rate functions, and the Autoregressive model AR(2). The two latter models seem to be adequate to properly simulate the earthquake production in a given area. The identification of the model which best fits the data, enables the estimations of the seismicity rate changes and the numbers of the earthquakes following a specific main shock.
Originalspråkengelska
Titel på värdpublikationBulletin of the Geological Society of Greece
Undertitel på värdpublikation12th International Conference of the G.S.G.
Sidor1984–1993
Volym43
Utgåva4
DOI
StatusPublished - 2010 jan.
Externt publiceradJa

Publikationsserier

NamnBulletin of the Geological Society of Greece

Ämnesklassifikation (UKÄ)

  • Geofysik

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