Seismological interpretation of earthquake-induced water-level fluctuations in wells
Seismological interpretation of earthquake-induced water-level fluctuations in wells
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DOI：
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发表时间：
1959-07
影响因子：
3
通讯作者：
J. Eaton;K. Takasaki
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文献类型：
--
作者：
J. Eaton;K. Takasaki
Magnitudes for normal-depth earthquakes computed from the amplitude of water-level fluctuations induced in a well tapping a confined aquifer in Honolulu, Hawaii, agree closely with those assigned by Pasadena. The maximum fluctuations in the well are produced by long-period Rayleigh surface waves. The response of the well to earthquake waves diminishes rapidly as wave length decreases.
