DEFORMATION OF SEISMIC WAVELETS BY THIN LAYERS AND LAYERED BOUNDARIES*

Author:

MEISSNER R.,MEIXNER E.

Abstract

AbstractUsing plane wave theory and assuming a given input wavelet the shape of the reflected (or transmitted) wavelet from a layered boundary is derived. Several types of boundaries are considered, among them the weathered layer and a wedge shaped intermediate layer. Different angles of incidence and all internal multiples are taken into account. The examples shown in the figures can be used for a direct comparison between theoretical and observed shapes of reflected (or transmitted) wavelets from special boundaries.

Publisher

Wiley

Reference18 articles.

1. Recording high frequency reflected waves on the Russian Platform;Berson I. S.;Bull. Ac. Sci. USSR, Geoph,1956

2. Some spectral characteristics of waves reflected from thin layers;Berson I. S.;Izv., Geoph. Series,1959

3. On a spectrum of waves, reflected and refracted by a plate;Chekin B. S.;Izv., Geoph. Series,1958

4. Deutung der Reflexionen aus der Erdkruste mit Hilfe synthetischer Seismogramme. Vortrag auf der 28, Tagung der Deutschen Geophys;Fuchs K.;Ges. in Qausthal- Zellerfeld,1967

5. Reflection of plane elastic waves from transition layers;Gupta R. N.;Bull. Seis. Soc. Am.,1966

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