Are seismic waiting time distributions universal?
We show that seismic waiting time distributions in California and Iceland have many features in common as, for example, a power-law decay with exponent $α\approx 1.1$ for intermediate and with exponent $γ\approx 0.6$ for short waiting times. While the transition point between these two regimes scale...
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ftdatacite:10.48550/arxiv.cond-mat/0410444 2023-05-15T16:49:00+02:00 Are seismic waiting time distributions universal? Davidsen, Jörn Goltz, Christian 2004 https://dx.doi.org/10.48550/arxiv.cond-mat/0410444 https://arxiv.org/abs/cond-mat/0410444 unknown arXiv https://dx.doi.org/10.1029/2004gl020892 Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004 http://arxiv.org/licenses/assumed-1991-2003/ Statistical Mechanics cond-mat.stat-mech Geophysics physics.geo-ph FOS Physical sciences article-journal Article ScholarlyArticle Text 2004 ftdatacite https://doi.org/10.48550/arxiv.cond-mat/0410444 https://doi.org/10.1029/2004gl020892 2022-04-01T16:19:12Z We show that seismic waiting time distributions in California and Iceland have many features in common as, for example, a power-law decay with exponent $α\approx 1.1$ for intermediate and with exponent $γ\approx 0.6$ for short waiting times. While the transition point between these two regimes scales proportionally with the size of the considered area, the full distribution is not universal and depends in a non-trivial way on the geological area under consideration and its size. This is due to the spatial distribution of epicenters which does \emph{not} form a simple mono-fractal. Yet, the dependence of the waiting time distributions on the threshold magnitude seems to be universal. : 5 pages, 4 figures, accepted for publication in Geophys. Res. Lett Text Iceland DataCite Metadata Store (German National Library of Science and Technology) |
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topic |
Statistical Mechanics cond-mat.stat-mech Geophysics physics.geo-ph FOS Physical sciences |
spellingShingle |
Statistical Mechanics cond-mat.stat-mech Geophysics physics.geo-ph FOS Physical sciences Davidsen, Jörn Goltz, Christian Are seismic waiting time distributions universal? |
topic_facet |
Statistical Mechanics cond-mat.stat-mech Geophysics physics.geo-ph FOS Physical sciences |
description |
We show that seismic waiting time distributions in California and Iceland have many features in common as, for example, a power-law decay with exponent $α\approx 1.1$ for intermediate and with exponent $γ\approx 0.6$ for short waiting times. While the transition point between these two regimes scales proportionally with the size of the considered area, the full distribution is not universal and depends in a non-trivial way on the geological area under consideration and its size. This is due to the spatial distribution of epicenters which does \emph{not} form a simple mono-fractal. Yet, the dependence of the waiting time distributions on the threshold magnitude seems to be universal. : 5 pages, 4 figures, accepted for publication in Geophys. Res. Lett |
format |
Text |
author |
Davidsen, Jörn Goltz, Christian |
author_facet |
Davidsen, Jörn Goltz, Christian |
author_sort |
Davidsen, Jörn |
title |
Are seismic waiting time distributions universal? |
title_short |
Are seismic waiting time distributions universal? |
title_full |
Are seismic waiting time distributions universal? |
title_fullStr |
Are seismic waiting time distributions universal? |
title_full_unstemmed |
Are seismic waiting time distributions universal? |
title_sort |
are seismic waiting time distributions universal? |
publisher |
arXiv |
publishDate |
2004 |
url |
https://dx.doi.org/10.48550/arxiv.cond-mat/0410444 https://arxiv.org/abs/cond-mat/0410444 |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
https://dx.doi.org/10.1029/2004gl020892 |
op_rights |
Assumed arXiv.org perpetual, non-exclusive license to distribute this article for submissions made before January 2004 http://arxiv.org/licenses/assumed-1991-2003/ |
op_doi |
https://doi.org/10.48550/arxiv.cond-mat/0410444 https://doi.org/10.1029/2004gl020892 |
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1766039064311496704 |