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U.S. Department of Energy
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Multicomponent seismic and borehole experiment to establish and identify the cause of anisotropy in the 2nd white specks at Garrington, Alberta

Conference ·
OSTI ID:80201
;  [1]
  1. PanCanadian Petroleum, Calgary, Alberta (Canada)
An orthogonal 2D multicomponent grid using compressional/shear airguns was acquired along with two P-Sv converted wave offset VSP`s and a zero offset shear VSP. The objective was to establish fracture orientation (assumed from caving zones in producing wells) within the 2nd White Speckled Shale of the Upper Cretaceous Colorado Group. Measurements indicate a periodic thin layering (PTL) anisotropy or transverse isotropy (TI), as opposed to fracture induced azimuthal or extensive-dilatancy anisotropy (EDA). TI or PTL anisotropy can give similar observations of S{sub 1}/S{sub 2} ray splitting, to fracture induced EDA, from propagation in off-principal axes (25{degree}--40{degree}) through clastic cyclothems, that are considerably less than a seismic wavelength Conclusions on anisotropy were made from stacking velocity differences between in-line Sv and cross-line Sh, despite consistent T{sub 0} times and interpretation of shear stacks with borehole measurements for evidence of shear wave splitting or rotation.
OSTI ID:
80201
Report Number(s):
CONF-941015--
Country of Publication:
United States
Language:
English