<> "The repository administrator has not yet configured an RDF license."^^ . <> . . . "Renormalization of earthquake aftershocks"^^ . "Assume that each earthquake can produce a series of aftershock independently of its size according to its “local” Omori's law with exponent 1 + θ. Each aftershock can itself trigger other aftershocks and so on. The global observable Omori's law is found to have two distinct power law regimes, the first one with exponent p− = 1-θ for time t < t* ∼ κ^(−1/θ), where 0 < 1 − κ < 1 measures the fraction of triggered earthquakes per triggering earthquake, and the second one with exponent p+ = 1 + θ for larger times. The existence of these two regimes rationalizes the observation of Kisslinger and Jones [1991] that the exponent p seems positively correlated to the surface heat flow: a higher heat flow is a signature of a higher crustal temperature, which leads to larger strain relaxation by creep, corresponding to fewer events triggered per earthquake, i.e. to a larger κ, and thus to a smaller t*, leading to an effective measured exponent more heavily weighted toward p+ > 1."^^ . "1999-07-01" . . "26" . "13" . . "American Geophysical Union"^^ . . . "Geophysical Research Letters"^^ . . . "00948276" . . . . . . . . . . "Didier"^^ . "Sornette"^^ . "Didier Sornette"^^ . . "Anne"^^ . "Sornette"^^ . "Anne Sornette"^^ . . "Laboratoire de Physique de la Matiere Condensee, CNRS UMR 6622 and Universite de Nice-Sophia Antipolis, Nice, France"^^ . . . "Department of Earth and Space Sciences and Institute of Geophysics and Planetary Physics, University of California, Los Angeles, CA"^^ . . . . . . "HTML Summary of #1504 \n\nRenormalization of earthquake aftershocks\n\n" . "text/html" . . . "Clustering and migration" . .