The magnitude-frequency distribution of earthquakes recorded with deep seismometers at Cajon Pass, southern California
The cumulative b-value (the slope of the Gutenberg-Richter relationship between earthquake occurrence rate and magnitude) is commonly found to be constant (∼1). Network catalogues, however, reveal a decrease at small magnitudes (
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Veröffentlicht in: | Tectonophysics 1996-08, Vol.261 (1), p.1-7 |
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Format: | Artikel |
Sprache: | eng |
Online-Zugang: | Volltext |
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Zusammenfassung: | The cumulative
b-value (the slope of the Gutenberg-Richter relationship between earthquake occurrence rate and magnitude) is commonly found to be constant (∼1). Network catalogues, however, reveal a decrease at small magnitudes ( |
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ISSN: | 0040-1951 1879-3266 |
DOI: | 10.1016/0040-1951(96)00052-2 |