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V/sub p//V/sub s/: a potential hydrocarbon indicator. [Incorporation of P wave data to detect zones of gas saturation]

Conference · · Geophysics; (United States)
OSTI ID:7247333

Theoretically and experimentally, the shear-wave velocity of a porous rock has been shown to be less sensitive to fluid saturants than the compressional wave velocity. Thus, observation of the ratio of the seismic velocities for waves which traverse a changing or laterally varying zone of undersaturation or gas saturation could produce an observable anomaly which is independent of the regional variation in compressional wave velocity. One source of shear-wave data in reflection seismic prospecting is mode conversion of P waves to shear waves in marine areas of high water bottom P-wave velocity. A relatively simple interpretative technique, based on amplitude variation as a function of the angle of incidence, is a possible discriminant between shear and multiple compressional arrivals, and data for a real case are shown. A normal moveout velocity analysis carefully coupled with this offset discriminant leads to the construction of a shear-wave reflection section which can then be correlated with the usual compressional wave section. Once such a section has been constructed, the variation in the ratio of the seismic velocities can be mapped, and potentially anomalous subsurface regions observed.

Research Organization:
Texaco Inc., Bellaire, TX
OSTI ID:
7247333
Journal Information:
Geophysics; (United States), Journal Name: Geophysics; (United States) Vol. 41:5; ISSN GPYSA
Country of Publication:
United States
Language:
English