Autor: |
Dolgikh, G. I., Shengchun, Piao, Budrin, S. S., Yang, Song, Dolgikh, S. G., Ovcharenko, V. V., Chupin, V. A., Yakovenko, S. V., Yang, Dong, Xiaohan, Wang, Shvets, V. A. |
Předmět: |
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Zdroj: |
Doklady Earth Sciences; Apr2020, Vol. 491 Issue 2, p285-289, 5p |
Abstrakt: |
By the analysis of the experimental data and model calculations, features of the propagation of hydroacoustic signals over a shelf of decreasing depth generated by a low-frequency hydroacoustic emitter at a frequency of 22 Hz and their transformations at the "water–bottom" interface into the Rayleigh waves recorded by a coastal laser strainmeter are studied. Energy estimates for the propagating hydroacoustic signals are presented at different points on the shelf; and such estimates for the transformed seismic–acoustic signals are obtained at the location of a laser strainmeter in the Earth's crust. [ABSTRACT FROM AUTHOR] |
Databáze: |
Complementary Index |
Externí odkaz: |
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