Method of suppressing vibration seismic signal correlation noise
First Claim
1. A method of seismic prospecting in which a plurality of seismic vibrating sources at a plurality of spaced source points contemporaneously radiate seismic signals into the earth, each source being responsive to an individual reference signal, the seismic signals traveling by different paths to a plurality of receivers in forming at each receiver a respective complete recorded signal comprising the steps of:
- a. generating a first signal of a first polarity and a first directional sweep over a first predetermined frequency range;
b. generating a second signal of a second and reverse polarity to said first polarity and second directional sweep opposite said first directional sweep over a second predetermined frequency range;
c. determining the common frequency of said first and second directional sweeps at a common time into their respective sweep patterns;
d. introducing alternately into first one and then the other of said first and second signals a taper at which said common frequency is reduced to zero;
e. recording returned portions of said first and second signals to form respective recorded signals;
f. separating the respective recorded signals into respective first signals and second signals to form first recorded complete signals and second recorded complete signals; and
g. inverse filtering said respective said first and second recorded signals to recover information attenuated by said tapers.
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Accused Products
Abstract
A method of seismic prospecting in which there is employed conventional upsweep and downsweep and opposed polarity of signals that are being sent into the earth as seismic signals and in which there is introduced a taper at the common frequency at the common time on the respective upsweep and downsweep signals to reduce the most significant part of the correlation noise, yet provide the advantages of each of the methods of using opposite phase polarity, to cancel and using opposite upsweep and downsweep to achieve reduction in the noise experienced, as well as the reduction of the most significant part of the correlation noise that distorts the desired zero-phase Klauder wavelet.
78 Citations
5 Claims
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1. A method of seismic prospecting in which a plurality of seismic vibrating sources at a plurality of spaced source points contemporaneously radiate seismic signals into the earth, each source being responsive to an individual reference signal, the seismic signals traveling by different paths to a plurality of receivers in forming at each receiver a respective complete recorded signal comprising the steps of:
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a. generating a first signal of a first polarity and a first directional sweep over a first predetermined frequency range; b. generating a second signal of a second and reverse polarity to said first polarity and second directional sweep opposite said first directional sweep over a second predetermined frequency range; c. determining the common frequency of said first and second directional sweeps at a common time into their respective sweep patterns; d. introducing alternately into first one and then the other of said first and second signals a taper at which said common frequency is reduced to zero; e. recording returned portions of said first and second signals to form respective recorded signals; f. separating the respective recorded signals into respective first signals and second signals to form first recorded complete signals and second recorded complete signals; and g. inverse filtering said respective said first and second recorded signals to recover information attenuated by said tapers. - View Dependent Claims (2, 3, 4, 5)
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Specification