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• W2078651857 startingPage "1452" @default.
• W2078651857 abstract "Love-wave excitation by large underground nuclear explosions at the Nevada Test Site is uniquely different from that by small explosions at shallow depths in its dependence on shot depth and its change with repeated experiments. There appears to be a magnitude threshold (or depth threshold: the two parameters are correlated) for strong excitation of Love waves from shots in a given geologic area, and the magnitude threshold for Yucca Flat has increased with time during the period 1962–1967. These results support the hypothesis that the tectonic stress release is the major cause of Love waves from the NTS explosions. Two working models of the stress release process are tested against observations. One model is the cavity model, in which pre-existing stress vanishes within a spherical zone around the shot point. The other is the trigger model, in which a fault displacement is triggered outside the immediate vicinity of the shot point. We favor the trigger model because of its better consistency with various observations. Under the assumption of the trigger model, we found that the process was characterized by a low stress drop (around 10 bars), the released energy being comparable to or smaller than the total seismic energy estimated from P-wave magnitude." @default.
• W2078651857 created "2016-06-24" @default.
• W2078651857 creator A5016854083 @default.
• W2078651857 creator A5059431735 @default.
• W2078651857 date "1972-03-10" @default.
• W2078651857 modified "2023-09-26" @default.
• W2078651857 title "Mechanism of Love-Wave excitation by explosive sources" @default.
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• W2078651857 doi "https://doi.org/10.1029/jb077i008p01452" @default.
• W2078651857 hasPublicationYear "1972" @default.
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