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。
:
The exploration method of transient Rayleigh wave is a new seismic me-
thod for quick and economical determination of Rayleigh wave velocity in rock
and soil layers. The actual shear wave velosity is calculated using Rayleigh
wave velosity. In this paper, the principle and field testing technique of this
exploration method is described. Several case studies are cited to illustrate
its utility. Finally, the advantages of this method are discussed.
出处
《物探与化探》
CAS
CSCD
1992年第2期113-119,共7页
Geophysical and Geochemical Exploration
