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• W2059635480 endingPage "1218" @default.
• W2059635480 startingPage "1215" @default.
• W2059635480 abstract "Compressional wave attenuation, Q p −1 , and velocity, V p , for an alkalic olivine basalt have been measured from 1250° to 1450°C and from 5 to 10 MHz by an ultrasonic interferometric technique. V p shows no significant frequency or temperature dependence, and Q p −1 increases with increasing frequency and decreasing temperature. For the conditions of this study, the melt can be modeled as a viscoelastic material with a single thermally activated structural relaxation mechanism having an activation energy of 2.2 eV and a relaxation time on the order of 1 ns. The data presented here fall in the region of the relaxation spectrum where the frequency, f, is much smaller than the relaxation frequency, and the absorption coefficient is proportional to f². Analysis of the data suggests that (1) compressional wave losses will be negligible in a basalt melt at seismic frequencies, and (2) the volume viscosity of basalt melt is comparable in magnitude to shear viscosity." @default.
• W2059635480 created "2016-06-24" @default.
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• W2059635480 date "1981-12-01" @default.
• W2059635480 modified "2023-09-27" @default.
• W2059635480 title "Ultrasonic studies on a basalt melt" @default.
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• W2059635480 doi "https://doi.org/10.1029/gl008i012p01215" @default.
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