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1)  Seismic converted wave prospecting
天然地震转换波探测
2)  deep-sounding by converted waves of earthquakes
天然地震转换波测深
3)  teleseismic profiling
天然地震探测
1.
Quite a large amount of teleseismic profiling has been conducted in the past 10 years or so in the Tibetan Plateau to study the lower crust upper mantle structure, yielding informative data for the geomechanic features ranging from the in depth seismic velocity image, upper mantle anisotropy and the identification of the low velocity body and layer.
在青藏高原等地区为研究下地壳上地幔的构造特征,最近10 a 投入了较大工作量的天然地震探测。
4)  Deep sounding by converted waves of earthquakes
地震转换波测深
5)  natural seismic wave
天然地震波
1.
The Q-value studies are not only studied by the natural seismic wave, but also in the laboratory, where the attenuation theory of seismic wave and observing method of measuring Q-value are studied.
人们不仅利用天然地震波对Q值进行测量 ,还在实验室内对地震波的衰减理论和测量Q值的方法进行了研究。
6)  seismic exploration with transformed wave method
转换波法地震勘探
补充资料:核爆炸地震波探测(见核爆炸探测)


核爆炸地震波探测(见核爆炸探测)
nuclear explosion seismic detection

hebaozho dizhenbo tanee核爆炸地震波探测(nuclear explos,onseismie detecuon)见核爆炸探汉,l。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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