Abstract A method for detecting the presences of fractures in a subsurface formation being penetrated by a drill bit during drilling. Teeth on the drill bit act as individual seismic sources, generating both shear wave energy and compressional wave energy. As the drill bit passes through a formation, the shear wave energy generated by the bit propagates along the formation in a waveguide mode between the adjacent formations. As the shear wave signal passes through a fractured zone of the formation, two shear wave signals are generated, each polarized in relationship to the orientation of the fractures in the formation. As the polarized signals propagate along the formation, secondary shear wave signals are generated which return to the surface and are detected by appropriate sensors. The sensors have a plurality of detectors in order to detect the polarity or direction of particle motion cuased by the polarized wave, providing information that a fracture zone exists in the subsurface.
Inventors
👤 Bob A. Hardage
Bibliographic Details
Application Number—
JurisdictionUS
Data Sourcegoogle_patents
Last Synchronized2026-11-09 07:12
CPC Classifications
G; G01; G01V; G01V1/00; G01V1/40; G01V1/42
Claims Analysis
Total Claims: 4
Claim 1
Independent Claim
173 words
A method for determining the location of fractured zones in a subsurface formation having a higher seismic velocity than overlying and underlying formations, comprising: generating a shear wave signal within the higher velocity formation, said shear wave signal travelling through the formation as a channel wave and being refracted toward the earth's surface as a shear head wave through the interface between the higher velocity formation and the overlying lower velocity formation; detecting said refracted shear head wave at a plurality of spaced apart locations at the earth's surface; and determining as a function of the detection location variations in the particle displacement vector of the detected shear head wave resulting from the channel wave travelling through a fractured zone in the higher velocity formation prior to being refracted as a shear head wave toward the earth's surface; and determining the location of a fracture zone in the higher velocity formation on the basis of the pattern variation detected at the earth's surface of the particle displacement vector of the shear head wave.
Claim 2
Independent Claim
173 words
A method for determining the location of fractured zones in a subsurface formation having a higher seismic velocity than overlying and underlying formations, comprising: generating a shear wave signal within the higher velocity formation, said shear wave signal travelling through the formation as a channel wave and being refracted toward the earth's surface as a shear head wave through the interface between the higher velocity formation and the overlying lower velocity formation; detecting said refracted shear head wave at a plurality of spaced apart locations at the earth's surface; and determining as a function of the detection location variations in the particle displacement vector of the detected shear head wave resulting from the channel wave travelling through a fractured zone in the higher velocity formation prior to being refracted as a shear head wave toward the earth's surface; and determining the location of a fracture zone in the higher velocity formation on the basis of the pattern variation detected at the earth's surface of the particle displacement vector of the shear head wave.
Claim 3
Dependent Claim
22 words
The method of claim 1 wherein the shear wave signal is generated by a drill bit as it drills a well bore.
Claim 4
Dependent Claim
33 words
The method of claim 2 wherein the drill bit is drilling a substantially horizontal well substantially parallel to the interfaces between the higher velocity formation and the overlying and underlying lower velocity formations.