GB1065870A - Seismic data processing - Google Patents
Seismic data processingInfo
- Publication number
- GB1065870A GB1065870A GB2530864A GB2530864A GB1065870A GB 1065870 A GB1065870 A GB 1065870A GB 2530864 A GB2530864 A GB 2530864A GB 2530864 A GB2530864 A GB 2530864A GB 1065870 A GB1065870 A GB 1065870A
- Authority
- GB
- United Kingdom
- Prior art keywords
- signal
- weighting factors
- auto
- filter
- correlation function
- Prior art date
- Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
- Expired
Links
Classifications
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V1/00—Seismology; Seismic or acoustic prospecting or detecting
- G01V1/28—Processing seismic data, e.g. analysis, for interpretation, for correction
- G01V1/36—Effecting static or dynamic corrections on records, e.g. correcting spread; Correlating seismic signals; Eliminating effects of unwanted energy
- G01V1/364—Seismic filtering
- G01V1/366—Seismic filtering by correlation of seismic signals
-
- G—PHYSICS
- G01—MEASURING; TESTING
- G01V—GEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
- G01V2210/00—Details of seismic processing or analysis
- G01V2210/30—Noise handling
- G01V2210/32—Noise reduction
Abstract
1,065,870. Geophysical prospecting. TEXAS INSTRUMENTS Inc. June 18, 1964 [June 21 1963], No. 25308/64. Heading H4D. [Also in Division G1] In a method for minimizing reverberation effects in a seismic signal, particularly in a marine seismogram, the signal is processed by passing it through a delay line filter having an impulse time response which is approximately the inverse of the reverberation effect. In the embodiment shown in Fig. 2, seismic disturbances arising from the detonation of a shot 1 are detected by a linear array of seismometers whose outputs may be processed so as to provide a single noise-free signal f(t). The signal f(t) is fed to a delay line filter (5) (Fig. 3), which may be a magnetic drum type or a series of electrical delay circuits, having M + 1 outputs at equal time intervals. The signals from these outputs have their amplitudes multiplied by respective filter weighting factors # and are then combined in a summing network (6), such as a differential summing amplifier, whose output constitutes the processed signal. The required impulse time response of the filter (5) is obtained by adjustment of potentiometers (7). The values of the weighting factors are computed by recording the noise-free signal f(t) on magnetic tape and feeding it to an arrangement 3 which generates the autocorrelation function of f(t). Such an arrangement may comprise an analogue or digital computer using a sampling method to calculate a set of M + 1 auto-correlation function coefficients for the signal f(t). The weighting factors are uniquely defined in terms of the auto-correlation function coefficients by a matrix equation, and are calculated by a digital computer 4 using the auto-correlation function coefficients as input data. The power/frequency response of the delay line filter (5) is stated to be approximately inversely proportional to the power spectrum of the seismic signal f(t) and the weighting factors # may therefore be used to estimate the power spectrum of the signal f(t). Phase errors introduced into the seismic signal f(t) by the apparatus may be compensated for by the use of a second filter in front of the auto-correlation function generator 3. A detailed mathematical treatment of the autocorrelation principle, and numerical examples of auto-correlation function coefficients and their associated filter weighting factors #, are given. The mathematical relationship between the coefficients and their weighting factors is claimed.
Applications Claiming Priority (1)
Application Number | Priority Date | Filing Date | Title |
---|---|---|---|
US28958163A | 1963-06-21 | 1963-06-21 |
Publications (1)
Publication Number | Publication Date |
---|---|
GB1065870A true GB1065870A (en) | 1967-04-19 |
Family
ID=23112152
Family Applications (1)
Application Number | Title | Priority Date | Filing Date |
---|---|---|---|
GB2530864A Expired GB1065870A (en) | 1963-06-21 | 1964-06-18 | Seismic data processing |
Country Status (3)
Country | Link |
---|---|
DE (1) | DE1448725B2 (en) |
GB (1) | GB1065870A (en) |
MY (1) | MY6900243A (en) |
Cited By (1)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN113640878A (en) * | 2021-08-12 | 2021-11-12 | 西南石油大学 | Method for constructing azimuth-apparent velocity radar map by using virtual seismic source scanning |
-
1964
- 1964-06-18 GB GB2530864A patent/GB1065870A/en not_active Expired
- 1964-06-22 DE DE19641448725 patent/DE1448725B2/en not_active Withdrawn
-
1969
- 1969-12-31 MY MY6900243A patent/MY6900243A/en unknown
Cited By (2)
Publication number | Priority date | Publication date | Assignee | Title |
---|---|---|---|---|
CN113640878A (en) * | 2021-08-12 | 2021-11-12 | 西南石油大学 | Method for constructing azimuth-apparent velocity radar map by using virtual seismic source scanning |
CN113640878B (en) * | 2021-08-12 | 2024-03-29 | 西南石油大学 | Method for constructing azimuth-apparent velocity radar chart by utilizing virtual seismic source scanning |
Also Published As
Publication number | Publication date |
---|---|
MY6900243A (en) | 1969-12-31 |
DE1448725A1 (en) | 1969-04-17 |
DE1448725B2 (en) | 1972-02-10 |
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