--> Abstract: Spectral Inversion for Meaningful and Accurate Seismic Interpretation, by S. Chopra and K. J. Marfurt; #90090 (2009).
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Spectral Inversion for Meaningful and Accurate Previous HitSeismicNext Hit Previous HitInterpretationNext Hit

Chopra, Satinder 1; Marfurt, Kurt J.2
1 Arcis Corporation, Calgary, AB, Canada.
2 University of Oklahoma, Norman, OK.

Previous HitSeismicNext Hit sections are expected to bear a striking resemblance to geological cross-sections. When this happens, Previous HitinterpretationNext Hit becomes straight-forward. If this does not happen, Previous HitseismicNext Hit interpreters resort to the art of geological Previous HitinterpretationNext Hit of the Previous HitseismicNext Hit Previous HitdataNext Hit based on their knowledge of the basic principles of geology and geophysics and their experience. In the practical scenario a certain amount of imagination is relied on when the bandwidth of the Previous HitdataNext Hit is not supportive of the Previous HitinterpretationNext Hit. Spectral reflectivity inversion helps the Previous HitseismicNext Hit interpreters by narrowing the gap between the two extremes mentioned above and produces sparse reflectivity estimates that resolve thin layers below the tuning thickness. The process differs from other inversions in that it is driven by geological rather than mathematical assumptions, and is based on aspects of the local frequency spectrum obtained using spectral decomposition of various types. The resolution of spectral inversion is far superior to the input Previous HitdataNext Hit and so makes it very suitable for characterization of thin reservoirs. This aspect makes the method ideal for detailed delineation and characterization of thin reservoirs.

An interesting aspect about spectral inversion is about an important attribute of the reflection process that a Previous HitseismicNext Hit interpreter looks for (in addition to four other attributes, namely, reflection polarity, strength, continuity and relationship to other reflections). While thin-bed reflectivity serves to provide four of these characteristics clearly, the reflection character can be studied by convolving the reflectivity with a wavelet of a known frequency bandpass. Finally, relative acoustic impedance run on thin-bed reflectivity yields valuable information in terms of subsurface rock layers rather than interfaces. Examples will be shown to illustrate how spectral inversion can help the Previous HitseismicNext Hit interpreter carry out meaningful and accurate Previous HitinterpretationTop.

 

AAPG Search and Discovery Article #90090©2009 AAPG Annual Convention and Exhibition, Denver, Colorado, June 7-10, 2009