Book Chapter
Synthesis of a Layered Medium from its Acoustic Transmission Response †
By
Jon F. Claerbout
Jon F. Claerbout
*
Stanford University Department of Geophysics, Stanford, California.
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Published:
January 01, 2008
A direct (noniterative) method 15 presented Lo determine an acoustic layered medium from the seismogram due to a time-limited plane wave incident from the lower halfspace. It is shown that one side of the autocorrelation of the seismogram due to an impulsive source at depth is the seismogram due to an impulsive source on the surface. This transforms the problem to the acoustic reflections problem as solved by Kunetz. Both the deep source time function and the layering can be determined from a surface seismogram.
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Society of Exploration Geophysicists Geophysics Reprint Series
Seismic Interferometry: History and Present Status
Society of Exploration Geophysicists

Volume
26
Copyright:
Society of Exploration Geophysicists
© Society of Exploration Geophysicists, ISBN >9781560801924$59.00
ISBN electronic:
9781560801924
Publication date:
January 01, 2008