Shear-Wave
Reflections in Southeast Wyoming
Jack Cameron
M. A. Martin and T. L. Davis have interpreted shear-wave
seismic reflection
data across the Silo field of southeast Wyoming in terms of microfractures. The
azimuthally polarized shear waves in the shallow section indicate
"microfractures" oriented at N40°W, and time delays between split shear waves
within the productive Niobrara (at about 8,000 ft depth) are believed to be
indicators of the direction and intensity of fracturing in that zone.
This section, however, includes about 6,200 ft of Pierre Shale, which is well
documented to be transversely isotropic. That characteristic is confirmed by an
offset vertical seismic profile in the Silo field that shows strong shear-wave
polarization in the vertical and horizontal planes. The coexistence of these two
types
of anisotropy may cause complications in shear-
wave
transmission, such as
multiple splitting.
Synthetic and real data demonstrate that under these circumstances
reflections are complex events, even when rotated into the optimum polarization
direction. However, converted wave
recordings, that is P waves reflected as S
waves, may be much simpler and much easier to interpret.
AAPG Search and Discovery Article #91035©1988 AAPG-SEPM-SEG Pacific Sections and SPWLA Annual Convention, Santa Barbara, California, 17-19 April 1988.