DEFORMATION OF SEISMIC WAVELETS BY THIN LAYERS AND LAYERED BOUNDARIES*
作者:
R. MEISSNER,
E. MEIXNER,
期刊:
Geophysical Prospecting
(WILEY Available online 1969)
卷期:
Volume 17,
issue 1
页码: 1-27
ISSN:0016-8025
年代: 1969
DOI:10.1111/j.1365-2478.1969.tb02069.x
出版商: Blackwell Publishing Ltd
数据来源: WILEY
摘要:
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.
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