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Structure of the random measure associated with an isotropic stationary process

✍ Scribed by Alain, Boudou; Sylvie, Viguier-Pla

Book ID
122548348
Publisher
Elsevier Science
Year
2014
Tongue
English
Weight
1010 KB
Volume
123
Category
Article
ISSN
0047-259X

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Seismic random processes are characterized by high non-stationarity and, in most cases, by a marked variability of frequency content. The hypothesis modeling seismic signal as a simple product of a stationary signal and a deterministic modulation function, consequently, is hardly ever applicable. Se