Angeliki Adamaki
Projektledare
EVIDENCE FOR INDUCED SEISMICITY FOLLOWING THE 2001 SKYROS MAINSHOCK
Författare
Summary, in English
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.
Publiceringsår
2010-01
Språk
Engelska
Sidor
1984-1993
Publikation/Tidskrift/Serie
Bulletin of the Geological Society of Greece
Volym
43
Dokumenttyp
Konferensbidrag
Ämne
- Geophysics
Nyckelord
- aftershocks
- patterns
- earthquake forecasting
- Statistical seismology
Status
Published