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- W69398087 abstract "A volcanic tremor is characterized by peaked spectra with frequencies ranging from 0.15 to 10Hz, which may be explained by resonance set up in magmatic conduits. Temporal changes of volcanic tremor periods have been observed on various volcanoes. Another feature of peaked tremor spectra is that, especially on Mount Etna, higher modes do not appear to be harmonics of the fundamental mode. These observations cannot be explained by a simple model consisting of a single resonating dike, which can only generate harmonic spectra. As an extension to the single dike model, I have considered two or more dikes placed in series with a different characteristic impedance. The characteristic impedance of the dike is determined by the cross-sectional area, the acoustic velocity, and the density of the fluid." @default.
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- W69398087 date "1992-01-01" @default.
- W69398087 modified "2023-09-23" @default.
- W69398087 title "Numerical Studies of the Dynamics of Fluid-Filled Cracks Placed in Series: A Model for Inharmonic Peaked Tremor Spectra" @default.
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- W69398087 doi "https://doi.org/10.1007/978-3-642-77008-1_14" @default.
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