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EVIDENCE FOR INDUCED SEISMICITY FOLLOWING THE 2001 SKYROS MAINSHOCK

Adamaki, A.K. LU orcid ; Tsaklidis, G. M. ; Papadimitriou, E. E. and Karakostas, V. G (2010) In Bulletin of the Geological Society of Greece 43. p.1984-1993
Abstract
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.
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author
; ; and
publishing date
type
Chapter in Book/Report/Conference proceeding
publication status
published
subject
keywords
aftershocks, patterns, earthquake forecasting, Statistical seismology
host publication
Bulletin of the Geological Society of Greece : 12th International Conference of the G.S.G. - 12th International Conference of the G.S.G.
series title
Bulletin of the Geological Society of Greece
volume
43
edition
4
pages
1984 - 1993
DOI
10.12681/bgsg.11389
language
English
LU publication?
no
id
feeb9078-7ea0-441f-a150-fff423b7c7a0
date added to LUP
2023-10-05 14:22:57
date last changed
2023-10-09 17:07:00
@inproceedings{feeb9078-7ea0-441f-a150-fff423b7c7a0,
  abstract     = {{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.}},
  author       = {{Adamaki, A.K. and Tsaklidis, G. M. and Papadimitriou, E. E. and Karakostas, V. G}},
  booktitle    = {{Bulletin of the Geological Society of Greece : 12th International Conference of the G.S.G.}},
  keywords     = {{aftershocks; patterns; earthquake forecasting; Statistical seismology}},
  language     = {{eng}},
  pages        = {{1984--1993}},
  series       = {{Bulletin of the Geological Society of Greece}},
  title        = {{EVIDENCE FOR INDUCED SEISMICITY FOLLOWING THE 2001 SKYROS MAINSHOCK}},
  url          = {{http://dx.doi.org/10.12681/bgsg.11389}},
  doi          = {{10.12681/bgsg.11389}},
  volume       = {{43}},
  year         = {{2010}},
}