Re. Grimm et al., Detection and analysis of naturally fractured gas reservoirs: Multiazimuthseismic surveys in the Wind River basin, Wyoming, GEOPHYSICS, 64(4), 1999, pp. 1277-1292
Multiazimuth binning of 3-D P-wave reflection data is a relatively simple b
ut robust way of characterizing the spatial distribution of gas-producing n
atural fractures. In our survey, data were divided into two volumes by ray
azimuth (approximately perpendicular and parallel (+/-45 degrees) to the do
minant fracture strike) and separately processed. Azimuthal differences or
ratios of attributes provided a rough measure of anisotropy. Improved imagi
ng was also attained in the more coherent fracture-parallel volume. A neura
l network using azimuthally dependent velocity, reflectivity, and frequency
attributes identified commercial gas wells with greater than 85% success.
Furthermore, we were able to interpret the physical mechanisms of most of t
hese correlations and so better generalize the approach. The apparent veloc
ity anisotropy was compared to that derived from other P- and S-wave method
s in an inset three-component survey. Prestack determination of the azimuth
al moveout ellipse will best quantify velocity anisotropy, but simple two-
or four-azimuth poststack analysis can adequately identify regions of high
fracture density and gas yield.