瞬态瑞雷波勘探方法

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摘要

瞬态瑞雷波勘探方法是一种新的地震方法。它可以快速和经济地测定岩土层的瑞雷波速度。由瑞雷波速度可换算成横波速度。本文简要叙述了它的原理和野外试验方法。并以实例说明了此方法的有效性。最后对这一方法的优点作了讨论。

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Abstract：

The exploration method of transient Rayleigh wave is a new seismic me-thod for quick and economical determination of Rayleigh wave velocity in rockand soil layers. The actual shear wave velosity is calculated using Rayleighwave velosity. In this paper, the principle and field testing technique of thisexploration method is described. Several case studies are cited to illustrateits utility. Finally, the advantages of this method are discussed.

出版日期: 1992-04-24

引用本文:

严寿民. 瞬态瑞雷波勘探方法[J]. 物探与化探, 1992, 16(2): 113-119.
Yan Shoumin. THE EXPLORATION METHOD OF TRANSIENTRAYLEIGH WAVE. Geophysical and Geochemical Exploration, 1992, 16(2): 113-119.

链接本文:

https://www.wutanyuhuatan.com/CN/ 或 https://www.wutanyuhuatan.com/CN/Y1992/V16/I2/113

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