Bayesian inversion of seismic spectral ratio for source scaling: Application to a persistent multiplet in the western Corinth rift
Author:
Affiliation:
1. Institut de Physique du Globe de Paris; Sorbonne Paris Cité, Université Paris Diderot, UMR 7154, CNRS; Paris France
2. Now at Swiss Seismological Service; ETH Zurich; Zurich Switzerland
Funder
Agence Nationale de la Recherche
Publisher
American Geophysical Union (AGU)
Subject
Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2015JB012217/fullpdf
Reference71 articles.
1. Earthquake source scaling relationships from −1 to 5 ML using seismograms recorded at 2.5-km depth;Abercrombie;J. Geophys. Res.,1995
2. Maximum likelihood estimate of b in the formula log N = a − bM and its confidence limits;Aki;Bull. Earthquake Res. Inst. Univ. Tokyo,1965
3. Global variations of stress drop for moderate to large earthquakes;Allmann;J. Geophys. Res.,2009
4. Seismicity and associated strain of central Greece between 1890 and 1988;Ambraseys;Geophys. J. Int.,1990
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