High-Resolution
Spectral Reflectivity Inversion: A Case Study on Thin Bed
Reservoirs
Carlos Cabarcas1, John Castagna1, and Oleg
Portniaguine3
1 The University of Oklahoma, Norman, OK
2 Fusion Geophysical,
Conventional wisdom generally considers a thin layer (thickness smaller
than 1/4 seismic wavelength) to be below seismic resolution
. Therefore, the top
and base reflections from a thin reservoir cannot be separated. However, these
well known
resolution
limitations (Widess, 1973, Kallweit 1982) are based on the
study of very special cases (Chung and Lawton, 1995) which may be inappropriate
for “real world” situations. For example,
resolution
below 1/4 wavelength is
possible for even signals. Also, the incorporation of instantaneous spectral
decomposition into a seismic reflectivity inversion can be tailored to overcome
conventional
resolution
limitations and effectively remove the seismic wavelet.
Our spectral inversion algorithm is applied to the Boonsville public
domain dataset. This dataset was acquired over a well-known giant gas field
located in the Forth Worth Basin, Texas. The aim of our algorithm is to improve
the characterization of thin bed reservoirs. The resolution
improvement and
detail obtained over the Atokan Age thin bed reservoirs of this field are very
remarkable. The Caddo Formation reservoirs are better delineated and extensively
correlated with production information. Elusive compartments recognized in
several wells but impossible to identify on the seismic volume are easily mapped
after the inversion. Spectral reflectivity inversion describes with sufficient
confidence isolated thin geologic bodies.
It should be noted that this methodology does not provide a unique solution and it is also very dependent on a good first approximation to the source wavelet. Nevertheless, the results after reflectivity inversion are more interpretable and useful than the original seismic data.
AAPG Search and Discovery Article #90039©2005 AAPG Calgary, Alberta, June 16-19, 2005