Titlebook: Seismic Wave Propagation in Real Media; Modeli Real’nykh Sre I. S. Berzon Book 1969 Springer Science+Business Media New York 1969 Well logg

FUSC

Analysis of the Spectral Characteristics of a Thin-Bedded Sequenceteristics for various representations of layered media have been developed for waves of different types. Analyses have also been made of the properties of the spectral characteristics computed for several representations of the medium. Spectral characteristics have been established for the case of t

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狗窝

ITCH

Physical Basis for the Use of Reflected Wave forms for Studying Groups of Thin Bedsarlier in this collection have shown that the occurrence of thin-bedded sequences is common. The bed thickness may be comparable to the lengths of the waves travelling through them in some cases, or considerably longer or shorter in other cases. In view of this, there is both scientific and practica

Ataxia

The Effect of the Density Ratio at a Boundary on the form of the Spectral Response of a Thin Layerrimental conditions have been used frequently in interpreting seismic data. The principal desire has been the determination of the seismic properties of the section: the thickness of individual layers and the propagation speeds for elastic waves within these layers. Usually, the densities of the roc

发酵剂

Methods for Averaging the Forms of Recorded Wavesroblems. One such problem is the choice of an appropriate representation of the medium by comparing computed wave forms with those obtained experimentally. Coincidence of computed wave forms with observed wave forms may be one of the primary criteria in selecting a representative model of the medium

熟练

渗入

Method for Recording Direct Longitudinal Waves at the Surface and Within a Mediumhe nature of propagation of seismic waves in such media. The wave forms and arrival times of waves recorded both at the surface and at interior points in the medium are used in obtaining these data [1–6].

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