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題 名 | Velocity Dispersion and Amplitude Attenuation of Rayleigh Waves Across the Philippine Sea=雷利波越過菲律賓海的速度頻散及振幅衰減 |
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作 者 | 余貴坤; 蔡孟初; 黃瑞德; | 書刊名 | Terrestrial, Atmospheric and Oceanic Sciences |
卷 期 | 11:2 2000.06[民89.06] |
頁 次 | 頁515-524 |
分類號 | 351.95 |
關鍵詞 | 雷利波; 速度頻散; 振幅; Rayleigh waves; Attenuation coefficients; Q values; Shear velocity; |
語 文 | 英文(English) |
英文摘要 | The fundamental-mode interstation group and phase velocities andattenuation coefficients of Rayleigh waves along four paths across the Philippine Sea are determined to have periods of between 20 and 110 secondsby the two-station method. The values of group and phase velocities arequite consistent with the results of previous studies using the single-stationmethod. Group and phase velocities vary significantly with different wavepaths at periods of less than 50 seconds, but for longer periods, the phasevelocities are quite close. The inversion results show that the thickness ofthe lithosphere is about 60 km in the Philippine Sea, except in the area ofthe eastern volcanic islands where a slightly thinner lithosphere (about 50km) is deduced. The attenuation coefficients observed in the Philippine Seaare higher than the values obtained in the Pacific. This result simply reflects that the Philippine Sea plate is younger than that of the Pacific. Lateral variation in attenuation coefficient is not as clear as it is in velocitybecause of its large variance. However, the vertical distribution of Qβ-1 isquite similar to that for the shear velocity model. |
本系統中英文摘要資訊取自各篇刊載內容。