TESTING THE COMPLETENESS OF EARTHQUAKE CATALOGS AND THE HYPOTHESIS OF SELF-SIMILARITY
TESTING THE COMPLETENESS OF EARTHQUAKE CATALOGS AND THE HYPOTHESIS OF SELF-SIMILARITY
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DOI:
10.1038/337251a0
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发表时间:
1989-01-19
期刊:
影响因子:
64.8
通讯作者:
SACKS, IS
中科院分区:
文献类型:
--
作者:
RYDELEK, PA;SACKS, IS
Self-similarity of the earthquake process is consistent with the observed linearb-value relation log (N) =a – bM, whereNis the number of earthquakes with magnitudeM. Deviations from linearity are believed to be due to statistical fluctuations because of the scarcity of events at largeM, or from incompleteness because of a detection threshold at smallM. Above some magnitude level, all local events are detected, because they exceed the noise background on the seismogram. As magnitude decreases, however, events go undetected as the seismic signal approaches the noise background. Thus more of the smallest events should be logged at night than during the day, because the cultural noise sources and winds are diminished at night, resulting in presumably quieter seismograms. Here we use this day-to-night noise modulation to develop a completeness test for earthquake catalogues; catalogues that indicate no significant modulation are considered complete. We test three catalogues and show that the completeness magnitude can be different from the magnitude at which theb-value departs from linearity. In particular, catalogues that show significant deviations in linearity at smallMbut are otherwise complete, are at odds with the hypothesis of earthquake self-similarity.