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
- 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
Similar Records
Fracture characterization at the Conoco Borehole Test Facility using shear-wave anisotropy
Linear-transform techniques for processing shear-wave anisotropy in four-component seismic data
Analysis of P and S wave vertical seismic profile data from the Salton Sea Scientific Drilling Project
Conference
·
Sat Dec 30 23:00:00 EST 1995
·
OSTI ID:542871
Linear-transform techniques for processing shear-wave anisotropy in four-component seismic data
Journal Article
·
Sun Jan 31 23:00:00 EST 1993
· Geophysics; (United States)
·
OSTI ID:6136520
Analysis of P and S wave vertical seismic profile data from the Salton Sea Scientific Drilling Project
Journal Article
·
Wed Nov 09 23:00:00 EST 1988
· J. Geophys. Res.; (United States)
·
OSTI ID:6569798