Seismic surveying technique for the detection of azimuthal varia

Electricity: electrical systems and devices – Safety and protection of systems and devices – Automatic reclosing

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367 36, 367 37, G01V 100

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048170615

ABSTRACT:
Polarized shear wave surveys are performed to determine azimuthal variations in the earth's subsurface caused by fracture orientation and density. The surveys may be done by using the same polarization (either horizontal or vertical) shear waves along two different seismic lines of profile, or by using different polarization shear waves along one common line of profile. The survey data are then processed and compared; any differences constitute a measure of fracture orientation and density. Subsurface zones of high fracture density, once identified, have been found to afford a higher likelihood of successful well completion.

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Crampin, "A Review of the Effects of Anisotropic Layering on the Propagation of Seismic Waves", Geophys. J. R. Astr. Soc., (1977), 54, 9-27.
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Crampin et al., "Estimating Crack Parameters from Observations of P-Wave Velocity Anisotropy", Geophysics, vol. 45, No. 3, (1980), 345-360.
Crampin, "Seismic Wave Propagation Through a Cracked Solid: Polarization as a Possible Dilatancy Diagnostic", Geophys. J. R. Astr. Soc., (1978), 53, 467-496.

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