High fidelity vibratory source seismic method with source separation
September 20, 2016. Estimated Expiration Date is calculated based on simple USPTO term provisions. It does not account for terminal disclaimers, term adjustments, failure to pay maintenance fees, or other factors which might affect the term of a patent.Patent References 3332511 3885225 Method of three dimensional seismic prospecting Methods for seismic exploration Minimum phase bandpass filtering of seismic signals Method and apparatus for correcting distorted seismic data Method of suppressing vibration seismic signal correlation noise Simultaneous performance of multiple seismic vibratory surveys Seismic data acquisition technique having superposed signals Method of source coding and harmonic cancellation for vibrational geophysical survey sources InventorsAssigneeApplicationNo. 717176 filed on 09/20/1996US Classes:367/41, Transmitted correlation367/38, Signal analysis and/or correction367/43, Filters702/14, Seismology702/17, Filtering or noise reduction/removal702/32Specific signal data processingExaminersPrimary: Lobo, Ian J.Attorney, Agent or FirmInternational ClassG01V 001/28AbstractA method of separating the effects of the earth response on vibratory energy from individual ones of multiple vibrators to geophones, in generating a seismic survey, is disclosed. According to the disclosed method, measurements of the actual vibrations generated at the source are made, in addition to the geophone measurements of the refracted and reflected vibrations, both over a number of frequency sweeps. The source and geophone vibrations are first transformed into frequency domain representations, by way of Discrete Fourier Transforms. An inverse matrix of the recorded frequency-domain source vibrations is then generated for each frequency. When the number of sweeps equals the number of vibrators, the inverse matrix is merely the multiplicative inverse of the source measurements; if the number of sweeps exceeds the number of vibrators, the inverse matrix is the generalized inverse of the original matrix. The inverse matrix for the frequency is applied to the recorded geophone vibrations at that frequency, to derive the transfer function, corresponding to the earth response, for each vibrator-geophone path in the survey. A weighting factor may be used to discount the effects of poorly behaved sweeps, and may be based on the ratio of the maximum and minimum eigenvalues for the inverse matrix. Using these derived transfer functions, an earth reflectivity function may be derived for each vibrator-geophone path by applying a minimum phase filter to the separated vibrator-geophone transfer function over frequency; this filter removes the effects of a ##EQU1## term, and yields the earth reflectivity function for the path.Other References
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