WO2016141598A1 - Surface consistent amplitude compensation method and device in common attitude gather - Google Patents

Surface consistent amplitude compensation method and device in common attitude gather Download PDF

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Publication number
WO2016141598A1
WO2016141598A1 PCT/CN2015/074246 CN2015074246W WO2016141598A1 WO 2016141598 A1 WO2016141598 A1 WO 2016141598A1 CN 2015074246 W CN2015074246 W CN 2015074246W WO 2016141598 A1 WO2016141598 A1 WO 2016141598A1
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seismic
energy
compensation
data
compensation factor
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PCT/CN2015/074246
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French (fr)
Chinese (zh)
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何登科
彭苏萍
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中国矿业大学(北京)
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Publication of WO2016141598A1 publication Critical patent/WO2016141598A1/en

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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/28Processing seismic data, e.g. for interpretation or for event detection
    • G01V1/36Effecting static or dynamic corrections on records, e.g. correcting spread; Correlating seismic signals; Eliminating effects of unwanted energy

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  • the invention relates to the field of seismic exploration, in particular to a method and a device for compensating amplitude uniformity of a common attitude gather in a seismic survey.
  • Seismic exploration technology is one of the important exploration methods and technologies in the fields of energy exploration engineering, geological engineering and engineering geophysical exploration.
  • a variety of seismic attributes can be used to detect geological anomalies, and the amplitude properties and their ancillary products play an extremely important role.
  • the seismic data on the same bin will come from different excitation sources and different detectors. Therefore, due to the difference in the characteristics of the excited source and the difference in the characteristics of the detector, there will be a large difference in the seismic data of the same surface.
  • the seismic response of non-subterranean geological anomalies includes the difference between the excitation energy of the source and the sensitivity of the received energy of the detector, and their influence belongs to the category of collecting foot marks.
  • the technique of rejecting or suppressing the influence of the excitation energy difference of the source and the influence of the difference in the sensitivity of the received energy of the detector is called surface consistency amplitude compensation.
  • the seismic data body conforms to the principle of surface consistency: that is, regardless of the source excitation of the physical point location, and regardless of the performance and model of the excitation source, the average energy or energy density they excite is equal. Regardless of which physical point location is received, and which detector is used for reception, the average energy or energy density they receive is equal.
  • the surface consistency amplitude compensation is a key link.
  • the principle of the method used is to first calculate the average energy of the whole work area, divide it by the energy of each track to obtain the total compensation factor of each track, and then decompose the total compensation factor into the source factor, detector factor, and offset factor. , the construction factor, etc., finally through the Gauss-Sedel iterative calculation to obtain the final compensation factor, and used to perform surface consistency amplitude compensation.
  • the related art provides a surface consistency amplitude compensation method, that is, firstly performing surface consistency on each component received by the detector.
  • the amplitude compensation factor is calculated, and the compensation factors of each detector in each component are kept unchanged.
  • the average value of each source compensation factor of all components is used as the final source compensation factor, and finally the surface consistency amplitude compensation is performed according to the final source compensation factor. .
  • the single-component and three-component surface consistency amplitude compensation has been widely used, which solves the amplitude difference caused by non-geological anomalies to some extent.
  • the same detector can be placed at different physical locations at different times, and the detectors deployed at different times in actual operation are Different, even if the individual detectors are the same, the coupling degree of the detector to the earth is different due to different laying conditions at different times, and the sensitivity of the detector and its coupling with the earth directly affect the detection.
  • the difference in amplitude recorded by the device which in turn affects the effect of surface consistency compensation. This problem exists in both multi-wave seismic exploration and longitudinal wave seismic exploration.
  • the calculation and correction of surface consistency amplitude compensation for the three-component seismic data respectively will destroy the relationship between the three components.
  • an embodiment of the present invention provides a method for coherent amplitude compensation of a common attitude gather set surface, including:
  • each compensation factor includes at least a source term compensation factor
  • the common attitude gathers are collected in the common detection wave track of the seismic data of the exploration work area, and the detector item compensation factor is calculated in the common attitude track set;
  • the surface consistency amplitude compensation of the seismic data of the entire work area is performed.
  • an embodiment of the present invention provides a first possible implementation manner of the first aspect, wherein the seismic data includes single component seismic data and three component seismic data;
  • Calculating the average total energy of all components of each seismic data in the seismic data includes:
  • T is the length of the time window
  • N is the number of components of the seismic data
  • C n,t is the nth component.
  • the embodiment of the present invention provides the second possible implementation manner of the first aspect, wherein the method further includes: performing a preliminary check on the surface consistency of each seismic energy And all seismic energy that meets the second preset condition constitutes a suspected non-surface consistent data volume;
  • a preliminary test of surface consistency is performed for each seismic energy, and all seismic energy of the first predetermined condition is determined as a representative data body including:
  • the difference between the statistical and the average value of the work area is the seismic energy in the mean square error region of the work area of 3 times, and the energy of the seismic track is taken as a representative data body;
  • a preliminary test of surface consistency is performed for each seismic energy, and all seismic energy that meets the second preset condition constitutes a suspected non-surface consistent data body, including:
  • the difference between the statistical and the average of the work area is the seismic energy outside the mean square error region of the work area, and the energy of the seismic trace is used as the suspected non-surface consistent data volume.
  • each compensation factor further includes: a offset component compensation factor and a structural item compensation factor.
  • the embodiment of the present invention provides the fourth possible implementation manner of the first aspect, wherein the method further includes :
  • the seismic energy of the detectors recorded in the construction class report is set in the common detection wave track as the corresponding common attitude gather;
  • the seismic trace energy of the detectors in different sets of time is extracted from the common detection wave track to form a corresponding common attitude gather.
  • the embodiment of the present invention provides the fifth possible implementation manner of the first aspect, wherein calculating the detector item compensation factor in the common attitude track set includes:
  • the detector term compensation factor is calculated in the co-statue track set; wherein Scale ⁇ is the compensation factor expectation value associated with the A-co-coordinate track set, and N ⁇ is the number of tracks of all seismic data included in the co-statue track set.
  • the embodiment of the present invention provides a sixth possible implementation manner of the first aspect, wherein the method further includes: calculating each item according to a Gauss-Seidel iterative method Compensation factor and detector term compensation factor; wherein the Gauss-Seidel iterative method includes a formula:
  • S s , A ⁇ , O o and C c are the source term compensation factor, the detector term compensation factor, the offset term compensation factor and the structural term compensation factor, respectively, Scale m, s, ⁇ , o, c are Total compensation factor.
  • the embodiment of the present invention provides the seventh possible implementation manner of the first aspect, wherein the ground data consistency amplitude compensation is performed on the seismic data of the entire work area, including:
  • the surface consistency amplitude compensation is performed on the seismic data of the entire work area
  • the method further includes:
  • the corresponding seismic trace data in the suspected non-surface consistent data volume is retained and subjected to surface consistency amplitude compensation;
  • the corresponding seismic trace data in the suspected non-surface consistent data volume is rejected or non-surface consistency amplitude compensation is performed.
  • the embodiment of the present invention provides the eighth possible implementation manner of the first aspect, wherein the non-surface consistency is performed on the corresponding seismic trace data in the suspected non-surface consistent data volume
  • the amplitude compensation includes:
  • the non-surface consistency amplitude compensation is performed on the corresponding seismic trace data in the suspected non-surface consistent data volume.
  • an embodiment of the present invention further provides a co-attack gather surface consistency amplitude compensation apparatus, including:
  • An acquisition unit configured to acquire seismic data in a exploration work area and a corresponding construction work report
  • a first calculating unit configured to calculate an average total energy of all components of each seismic data in the seismic data acquired by the acquiring unit, to obtain seismic channel energy of the track;
  • a verification unit configured to perform a preliminary test of surface consistency on the seismic energy calculated by each first computing unit
  • a first determining unit configured to determine all seismic energy of the first predetermined condition as a representative data volume
  • a second calculating unit configured to calculate, in a representative data body determined by the first determining unit, each compensation factor corresponding to each track energy, and each compensation factor includes at least a source term compensation factor;
  • the extracting unit is configured to extract a common attitude gather in the common detection wave point of the exploration work area according to different postures of the detector;
  • a third calculating unit configured to calculate a detector term compensation factor in the common attitude track set extracted by the extracting unit
  • the surface consistency amplitude compensation unit is configured to perform surface consistency on the seismic data of the entire work area according to the compensation factors calculated by the second calculation unit and the total compensation factor formed by the detector item compensation factor calculated by the third calculation unit. Amplitude compensation.
  • the method and device for coherent track gather surface consistency amplitude compensation provided by the embodiments of the present invention firstly acquire seismic data in a exploration work area and a construction work report corresponding to the seismic data; and then calculate all components of each seismic data in the seismic data. Average total energy, obtain the seismic energy of the track; then perform a preliminary test of the surface consistency of each seismic energy, and determine all the seismic energy of the first preset condition as a representative data volume; The representative data body calculates each compensation factor corresponding to each track energy, and calculates the detector term compensation factor in the common attitude track set; finally, according to the compensation factors and the total compensation factor composed of the detector term compensation factor, Performing surface consistency amplitude compensation for seismic data of the entire work area, and present There is a lack of a technique to better perform surface consistency amplitude compensation.
  • the three-component seismic data is calculated together to make the calculation result more accurate.
  • Subsequent surface consistency compensation lays a solid foundation, and considering the placement posture of the detector, calculating the detector term compensation factor in the common attitude track also makes the calculation result more accurate, both of which are ground-consistent. The result is more accurate.
  • the method and device for compensating the amplitude uniformity of the common attitude gathers on the ground surface of the present invention provide non-surface consistency amplitude compensation for the suspected non-surface consistent seismic traces, so that the seismic traces are The compensation result of the data is more accurate.
  • FIG. 1 is a schematic diagram of an observation system according to an embodiment of the present invention.
  • FIG. 2 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the Z component in the single attitude of FIG. 1 according to an embodiment of the present invention
  • FIG. 3 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the X component in the single attitude of FIG. 1 according to an embodiment of the present invention
  • FIG. 4 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the Y component in the single attitude of FIG. 1 according to an embodiment of the present invention
  • FIG. 5 is a schematic view showing comparison of the surface exit angles in a single attitude in FIG. 1 according to an embodiment of the present invention
  • FIG. 6 is a schematic diagram showing a comparison of the azimuth angles of the inspection in a single attitude in FIG. 1 according to an embodiment of the present invention
  • FIG. 7 is a schematic diagram showing a rolling construction arrangement of an observation system according to an embodiment of the present invention.
  • FIG. 8 is a schematic diagram showing a comparison between the current method for the Z component in various postures in FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention;
  • FIG. 9 is a schematic diagram showing a comparison between the current method for the X component in various postures of FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention;
  • FIG. 10 is a schematic diagram showing a comparison between the current method for the Y component in various postures of FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention;
  • FIG. 11 is a flowchart of a method for compensating amplitude consistency of a common attitude gather set surface according to an embodiment of the present invention
  • FIG. 12 is a schematic structural diagram of a co-attend track gather surface consistency amplitude compensation apparatus according to an embodiment of the present invention.
  • the invention relates to surface consistency amplitude compensation in multi-wave three-component (including longitudinal wave single component) seismic exploration, and proposes a new amplitude compensation method for accurately analyzing and correcting surface consistency compensation factors for data processing and interpretation inversion.
  • the features of the invention are:
  • the calculation of the three-component surface consistency amplitude compensation factor requires three components to be calculated together and cannot be performed separately.
  • the calculation of the surface uniform amplitude compensation factor needs to be three.
  • the total energy of the components is treated as a single component.
  • a separate factor analysis is performed on the three components, and the other factors are kept unchanged, and the average value of the source factors of each component is selected as the final source factor of all components. This solves the problem of the consistency of the source factor to a certain extent, but ignores the difference in the energy relationship between the individual components of the seismic body wave energy.
  • the total energy in a three-component seismic survey can be expressed as
  • the longitudinal and transverse wave components are separated, and the total energy of the transverse wave component is treated as a single component for surface uniform amplitude compensation.
  • the scheme guarantees the energy relationship between the shear wave components to a certain extent, and is beneficial to utilize the two shear wave components and the fast and slow wave components after the processing to perform the crack detection.
  • this scheme still destroys the relationship between the longitudinal wave energy and the shear wave energy, and it will be misunderstood in the application of full waveform inversion.
  • a star symbol represents a shot, a total of 10 shot lines, 10 shots per line, and the point and line spacing are both 60 meters;
  • the detection point, a total of 24 detector lines, 24 detectors per line, point and line spacing are 50 meters.
  • Different energy amplification factors are randomly generated for each shot point and detection point respectively, and the energy factor of each track in the whole area is the factor product of the corresponding shot point and the detection point.
  • a two-layer geological model was designed with an interface depth of 800 m.
  • the longitudinal wave velocities of the upper and lower layers were 2400 m/s and 3000 m/s, the shear wave velocities were 800 m/s and 1000 m/s, and the density was 2.0 kg/m 3 and 2.3 kg/ m 3 .
  • the longitudinal and transverse wave reflection coefficients of each channel when the longitudinal wave is incident are calculated by the Zeoppritz formula, and the sum of the squares is taken as the square of the total energy of the body wave.
  • the influence of the weathering layer assumes that the surface emission angle of each channel is 1/1 of the longitudinal wave reflection angle.
  • the zero degree of the azimuth of the inspection is from the positive X-axis, and the counterclockwise is positive; the azimuth of the X-component transverse wave detector is directed to the positive X-axis.
  • the total energy received by each channel is the product of the total body wave energy and the corresponding shot point factor and the detection point factor.
  • the amplitude of the three components is calculated according to formula (1).
  • FIG. 2 to FIG. 4 the effect comparison of two different methods of Z, X, and Y components is sequentially shown in FIG. 2 to FIG. 4.
  • the original amplitude, the amplitude after compensation in the prior art and the amplitude after compensation by the technique of the present invention are sequentially displayed.
  • both the prior art and the technique of the present invention can perform amplitude compensation well, and the relative difference in amplitude of the Z component is corrected from about 4 times to about 1 time, and the X and Y components are The relative amplitude difference is corrected from -10 to 10 times to -3 to 3 times.
  • the top surface of the figure is the original surface exit angle, the surface exit angle after prior art compensation, the surface exit angle after compensation by the technique of the present invention, and the exit angle error after prior art compensation. It can be seen from FIG. 5 that the surface exit angle after compensation by the technique of the present invention is consistent with the original exit angle, and the exit angle error after compensation in the prior art is -9° to 3°, which seriously destroys the longitudinal wave energy and the shear wave energy. The relationship between them.
  • the current three-component surface consistency amplitude compensation method cannot maintain the energy relationship between the components, and the new method proposed by the present invention can do this.
  • the so-called common attitude gathers that is, in the common detector locus set, according to different postures of the detector (including the inclination angles of the three component detectors and the azimuth of the transverse wave components), the sub-tracks composed of different seismic data are extracted. set.
  • multiple coverage techniques are common techniques.
  • the seismic observation system will move forward a certain distance according to the design requirements and roll construction.
  • the same detector The physical location will have different detectors at different construction times.
  • the above figure is a single-chip observation system.
  • the following figure is the observation system after rolling. There are two bundles, three bundles each, each marked with numbers 1 to 6.
  • the numerical serial number also indicates the sequence of rolling construction. .
  • the detector In the overlap of the 1, 2 single piece and the 5, 6 single piece in Fig. 7, the detector is placed at least twice in the same detector position, that is, at least two different postures. In actual construction, there are often more than two attitudes of detector placement for various reasons. For example, in a three-component seismic exploration project in the application of the present invention, there are a total of 7261 geophysical point positions in the whole area, and the actual common attitude gather is 36,342, and the average physical point of each detector is about 5 postures, at most One detector position has 21 positions. Therefore, at the same detector position, since the detectors disposed at different times are different, the sensitivity of the detector and the degree of coupling of the detector to the earth are also different. Even if the same detector is accidentally placed at the same detector physical point position at different times, the sensitivity is the same, but the degree of coupling with the ground is different due to different layout conditions.
  • the comparative analysis method adopts the three-component surface consistency amplitude compensation method proposed by the present invention, that is, according to formula (2), the total energy of the three components is regarded as a single component for amplitude compensation factor analysis, and the comparative analysis is
  • the current co-detection wave point gather method is also used to calculate the amplitude compensation factor using the common attitude gather method in the present invention.
  • the detectors between the two dotted lines have a total of four postures, and each posture receives a record of 25 shots, respectively, outside the two dotted lines.
  • the detector has only one gesture.
  • the direct simulation randomly generates the detector amplitude factor in different poses.
  • the compensation factor is calculated using the three-component surface consistency amplitude compensation of the present invention.
  • the Z, X and Y component analysis results are sequentially displayed. From top to bottom in each figure are the original amplitude, the amplitude after the prior art compensation, and the amplitude after compensation by the common attitude gather analysis method proposed by the present invention.
  • the current common detection point gather analysis method does not solve the amplitude compensation problem, and the new method of the common attitude gather set of the present invention performs the amplitude compensation well.
  • the original relative difference of the Z component is less than 10 times, and the compensation is more than 10 times;
  • the original relative difference of the X component is about -12 to 8 times, and the compensation is changed. It is -15 to 9 times;
  • the original relative difference of the Y component is about -12 to 10 times, and after compensation, it becomes -25 to 11 times.
  • the relative difference distribution after compensation is not positively correlated with the original relative difference distribution.
  • the method of the present invention proposes a common attitude gather surface uniformity amplitude compensation technique, it can solve the problem of good surface uniformity amplitude anomaly.
  • Non-surface consistency amplitude compensation analysis and correction methods are designed in the present invention. Firstly, the average energy and energy mean squares of all the seismic traces in the whole area are counted, and the seismic traces whose energy is located outside the 3 times mean square error are removed from the seismic data of the whole area as the abnormal track. The remaining seismic data constitutes representative data. body. The average energy and energy mean squared are re-stated in a representative data volume. This average energy is the expectation after the regional uniformity amplitude compensation. For the rejected track, the correction will be corrected according to the expectation of the compensation correction, that is, the non-surface consistency amplitude compensation is performed. Eventually, the amplitude energy of all the seismic traces in the region will be compensated to the desired amplitude energy level. Like surface consistency amplitude compensation, non-surface consistency amplitude compensation is still performed according to the working principle and method of three-component surface consistency amplitude compensation, maintaining the inherent relationship of energy between the three components.
  • the co-attack gathers the ground surface uniform amplitude compensation method
  • the different postures of the detector are divided in the common detection wave track, and the different common attitude gathers are separately implemented to perform the detector compensation factor analysis, and at the same time
  • the total energy of the three-component seismic data is used as a single-component implementation of surface uniform amplitude compensation, which ensures the correct energy relationship between the three components, and also corrects the non-surface consistency amplitude anomaly, so compared with the prior art, It has the advantage of being able to accurately compensate for amplitude differences caused by surface consistency factors while ensuring the correct energy relationship between the components:
  • FIG. 11 is a flow chart showing a method for compensating amplitude consistency of a common attitude track set surface according to an embodiment of the present invention.
  • the method includes two key technologies: one is that the geophone's surface consistency amplitude compensation factor analysis and the amplitude compensation are all performed in the common attitude track set. Second, in three-component seismic exploration, the sum of the energy of the three components is treated as a single component for surface consistency amplitude compensation analysis. When correcting, the correction factors of the three components of each channel are the same. The specific process is as follows:
  • all the seismic energy of the test result conforming to the first preset condition is determined as a representative data body, and all the seismic energy of the second preset condition is determined as a suspected non-representative data body.
  • the first preset condition and the second preset condition may be two different manners of the same condition, or may be two different conditions.
  • the first preset condition and the second preset condition are the former, specifically: the first preset condition that satisfies the principle of 3 times mean square error, and the second condition that does not meet the principle of 3 times mean square error .
  • each compensation factor corresponding to each track energy in a representative data body, and each compensation factor includes at least a source term compensation factor.
  • the common detection track gathers are extracted from the common detection wave points extracted from the seismic data of the exploration work area, and the detector item compensation factor is calculated in the common attitude track.
  • Step 201 Establish an observation system for the original data in the seismic exploration (ie, the seismic data in the exploration work area), and edit the original data to eliminate the seismic road with serious noise pollution.
  • Step 202 Select an appropriate time window, calculate the average total energy of all components of each seismic data in the time window, and use the energy of each seismic trace.
  • the calculation formula is
  • N is the number of components of the seismic data, if it is a single component, such as longitudinal wave seismic exploration, N is equal to 1, and if it is a three-component seismic exploration, N is equal to 3.
  • C n,t is the amplitude value of the t-th sample point of the nth component in the time window.
  • Step 203 Calculate the average value Avg and the mean square error Std of all the seismic energy of the whole area, perform a preliminary test of the surface consistency of each seismic energy according to the principle of 3 times mean square error, and remove the abnormal seismic track according to the test result (ie, suspected non- The data consistency of the surface consistency), the surface consistency amplitude compensation is performed in the remaining seismic gathers (ie, the representative data volume), and the non-surface consistency amplitude correction is performed on the excluded seismic traces.
  • the average energy is calculated in a representative data volume as the expected value of the full-area amplitude correction.
  • the specific calculation formula is:
  • M is the total number of seismic traces in the whole zone
  • K is the total number of seismic traces of representative data volumes.
  • Step 204 Calculate the total compensation factor expectation value of each track in a representative data body, and the specific calculation formula is:
  • Step 205 Extract a common shot point gather in a representative data body, and statistically analyze the compensation factors of each source.
  • Scale s is the compensation factor expectation value of the seismic trace associated with the S-th shot
  • N s is the number of coverage times of the common shot gather.
  • Step 206 Extract a common offset track gather in a representative data body, and statistically analyze the compensation factors of each offset segment.
  • Scale o is the expected value of the compensation factor for the seismic trace associated with the 0th offset section
  • N o is the number of coverages of the total offset set.
  • Step 207 Extract the same structural item gathers in the representative data body, and statistically analyze the compensation factors corresponding to the respective structural items.
  • Scale c is the compensation factor expectation value of the seismic trace associated with the Cth construction term
  • N c is the number of coverage times of the construction item gather.
  • the extraction of the construction item gather is basically the same as the current method.
  • the common center point (ie CMP, or CDP) gather is the structural item gather; if it is the converted shear wave seismic data processing, the common asymptotic transition point gather is generally used as the structural item gather .
  • the three-component seismic data it needs to be determined according to the time window selected in step 202. If the main energy in the time window range is the longitudinal wave energy, the common center gather is used as the structural item gather; if the main energy When the shear wave energy is converted, the common asymptotic conversion point gather is used as a structural item gather.
  • Step 208 Extract a common attitude gather in the common detection track gather, perform statistical analysis on each common attitude gather, and obtain a detector compensation factor corresponding to each common attitude gather.
  • the specific method is as follows: (1) In the three-component seismic exploration, the inclination value of each component can be read from the seismic data track head, and each inclination value or a combination thereof is used as the attitude identification code. If there are more than two attitude identification codes in different detector placement times in the common detector locus, it is possible to add the layout time and combine them together to form a new gesture identification code. (2) For single-component seismic exploration, the same detector physics can be recorded from the field construction record At the point position, the order of the detectors is set in the order of the time, and the layout time is used as the identification code of the gesture. Finally, different common attitude gathers are extracted according to different pose identification codes in the common checkpoint track set.
  • the compensation factor for the common attitude gather is calculated as:
  • Scale ⁇ is the compensation factor expectation associated with the A-co-coordinate set of gathers
  • N ⁇ is the number of coverages of the common pose gather.
  • Step 209 Decompose the total compensation factor of each seismic data into a shot compensation factor S m, s , a detection point compensation factor A m, ⁇ , a offset compensation factor O m, o, and a structural item compensation factor C m, c Etc., and calculate the total compensation factor for each seismic trace data according to formula (10).
  • Step 210 Perform an iterative calculation according to the classical Gauss-Seidel iterative method to obtain the final compensation factors.
  • the left end of each equation is calculated as the compensation factor of the shot point, the detection point, the offset, and the structural item in the Kth iteration. After 3 iterations, a suitable compensation factor can be obtained.
  • Step 211 Perform the surface consistency compensation for each seismic data in the representative data volume by using the compensation factor obtained in step 210.
  • the invention proposes to apply, only two compensation factors of the shot point and the detection point are applied, and not all factors are applicable. Because the structural term corresponds to the response of the subsurface geological anomaly, the offset term corresponds to the variation of the amplitude with the offset (ie AVO), which is also the response related to the underground geological body, and the non-surface consistency problem.
  • Step 212 Calculate the average value and the mean square error of the compensated amplitude energy according to the methods of steps 202 and 203 for the compensated seismic data in step 211.
  • Step 213 Perform non-surface consistency amplitude verification and correction.
  • the seismic channel data is amplitude compensated.
  • the compensated amplitude energy is tested according to the average value and the mean square error in step 212. If it belongs to the range of 3 times mean square error, the amplitude difference of the seismic data is considered to belong to the surface. Consistency issues and acceptance of surface consistency compensation. If the range of the mean square error is more than 3 times, the amplitude difference of the seismic data is considered to be a non-surface consistency problem, and the ground surface consistency compensation is rejected, and the seismic data energy is corrected to the expected value of the earthquake data amplitude correction of the whole region.
  • the surface consistency amplitude compensation was performed on the seismic data of the whole region, and the non-surface consistency amplitude correction was also performed on a few seismic traces that did not satisfy the surface consistency amplitude test.
  • the seismic data of the whole region can obtain high-fidelity amplitude compensation, eliminating the surface amplitude anomaly, and retaining the inherent energy proportional relationship between the three components in the three-component seismic exploration. Provides high quality basic data for subsequent data processing and interpretation inversion.
  • the embodiment of the present invention further provides a co-attack gather surface consistency amplitude compensation device, as shown in FIG. 12, including:
  • the obtaining unit 11 is configured to acquire seismic data in the exploration work area and the corresponding construction work report.
  • the first calculating unit 12 is configured to calculate an average total energy of all components of each seismic data in the seismic data acquired by the acquiring unit 11 to obtain the seismic channel energy of the track.
  • the first calculating unit 12 is specifically used according to the formula Calculate the average total energy of all components of each channel of data to obtain the seismic energy of each channel.
  • the checking unit 13 is configured to perform a preliminary test of the surface consistency of each track energy calculated by the first calculating unit 12.
  • the checking unit 13 includes: a first calculating subunit for using a formula according to the formula Calculate the mean and mean square error of all seismic energy in the exploration area, and obtain the average and mean square error of the work area; where M is the total number of seismic traces in the entire work area.
  • the first determining unit 14 is configured to determine all the seismic energy of the inspection result of the verification unit 13 according to the first preset condition as a representative data volume.
  • the first determining unit 14 includes a first statistical subunit and a first determining subunit, where the first statistical subunit is configured to calculate the seismic energy of the difference between the average value of the work area and the mean square error area of the work area; A determining subunit is configured to determine the seismic channel energy of the first statistical subunit as a representative data volume.
  • the second calculating unit 15 is configured to calculate each compensation factor corresponding to each track energy in the representative data body determined by the first determining unit 14, and each compensation factor includes at least a source term compensation factor.
  • the extracting unit 16 is configured to extract a common attitude gather in the common detection wave point gather of the exploration work area according to different postures of the detector.
  • the third calculating unit 17 is configured to calculate a detector term compensation factor in the common attitude track set extracted by the extracting unit 16.
  • the third calculating unit is specifically used according to the formula
  • the detector term compensation factor is calculated in the co-statue track set; wherein Scale ⁇ is the compensation factor expectation value associated with the A-co-coordinate track set, and N ⁇ is the number of tracks of all seismic data included in the co-statue track set.
  • the surface consistency amplitude compensation unit 18 is configured to perform seismic compensation data for the entire work area according to the total compensation factors formed by the compensation factors calculated by the second calculation unit 15 and the detector term compensation factors calculated by the third calculation unit 17 Surface consistency amplitude compensation.
  • the surface consistency amplitude compensation unit 18 includes a second calculation subunit and a surface consistency amplitude compensation subunit;
  • the surface consistency amplitude compensation sub-unit is configured to perform surface consistency amplitude compensation on the seismic data of the entire work area according to the total compensation factor calculated by the second calculation sub-unit.
  • the surface consistency amplitude compensation unit 18 is further configured to perform surface consistency amplitude compensation on the suspected non-surface consistent data volume.
  • the apparatus further includes a second determining unit configured to use all of the seismic energy of the second predetermined condition as the suspected non-surface consistent data volume.
  • the second determining unit includes a second statistic subunit and a second deterministic subunit, and the second statistic subunit is configured to count the difference between the average value of the work area and the seismic trace energy outside the mean square error region of the work area;
  • the second determining subunit is configured to determine the statistically obtained seismic trace energy as a suspected non-surface consistent data volume.
  • the apparatus further includes a third determining unit configured to determine the seismic channel energy of the common detection point concentrator detector in different deployment times as the corresponding common attitude gather.
  • the third determining unit is specifically configured to: according to the size of the respective dip angles of the three components measured by the seismic acquisition system and the construction class report, extract the seismic energy of the detectors in different sets of time in the common detection wave track, and determine Corresponding common attitude gathers.
  • the apparatus further includes a fourth calculating unit, configured to calculate each compensation factor and the detector term compensation factor according to the Gauss-Seidel iterative method;
  • the device further includes:
  • a fifth calculating unit is configured to calculate the seismic energy of the compensated suspected non-surface consistent data volume.
  • the sixth calculating unit is configured to calculate an average value and a mean square error of all the seismic energy of the representative data volume after the surface consistency amplitude compensation.
  • the verification unit is configured to verify the seismic energy of the suspected non-surface consistent data volume according to the average value and the mean square error calculated by the sixth calculating unit, and obtain the verification result.
  • a retaining unit configured to retain the suspected non-surface consistent data volume that passes through the surface consistency amplitude compensation when determining that the verification result of the verification unit meets the first preset condition.
  • the non-surface consistency amplitude compensation unit is configured to perform non-surface consistency amplitude compensation on the suspected non-surface consistent data volume when determining that the verification result meets the second preset condition.
  • the culling unit is configured to cull the suspected non-surface consistent data body when determining that the verification result of the verification unit meets the second preset condition.
  • non-surface consistency amplitude compensation unit comprises:
  • the third calculation subunit according to the formula Calculating the expected value of the representative data volume of the entire work area corresponding to the seismic data after the seismic data is compensated by the surface consistency amplitude, where K is the total number of seismic traces in the representative data volume;
  • the non-surface consistency amplitude compensation sub-unit performs non-surface consistency amplitude compensation on the suspected non-surface consistent data volume according to the final compensation factor calculated by the fourth calculation sub-unit.
  • the common attitude road set surface consistency amplitude compensation device provided by the invention, in addition to the surface consistency amplitude compensation in the amplitude compensation process, corrects the non-surface consistency amplitude difference of the unqualified seismic track, so that The correction and compensation results of the seismic trace data are more accurate.

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Abstract

A surface consistent amplitude compensation method and device in a common attitude gather, the method comprising: acquiring seismic data and a corresponding operation log in an exploration work area; calculating an average total energy of all components of each channel of the seismic data to serve as a seismic channel energy of the channel; performing a surface consistent preliminary test on the obtained energy of each seismic channel, and determining a seismic channel energy satisfying a first preset condition to be a representative data body; calculating each compensation factor corresponding to the seismic channel energy in the representative data body, and calculating a compensation factor for a detector in a common attitude gather; performing surface consistent amplitude compensation on the seismic data for the entire work area according to a total compensation factor consisting of the abovementioned two factors; and calculating the three seismic data components together, thus obtaining an energy distribution trigonometric function relationship among the three data components, taking into account a placement attitude of the detector, calculating the compensation factor for the detector in the common attitude gather, and thereby enabling a calculation result to be more accurate.

Description

共姿态道集地表一致性振幅补偿方法及装置Co-attitude gather surface consistency amplitude compensation method and device 技术领域Technical field
本发明涉及地震勘探领域,具体而言,涉及地震勘探中共姿态道集地表一致性振幅补偿方法及装置。The invention relates to the field of seismic exploration, in particular to a method and a device for compensating amplitude uniformity of a common attitude gather in a seismic survey.
背景技术Background technique
地震勘探技术是能源勘察工程、地质工程、工程物探等领域的重要勘探方法和技术之一。在地震勘探处理解释成果中,可以利用多种地震属性探测地质异常体,其中振幅属性及其附属产品具有极其重要的作用。在地震勘探野外数据采集过程中,由于多次覆盖技术的应用,同一个面元上的地震数据会来自不同的激发震源和不同的检波器。因此,受激发震源特性差异和检波器特性差异的影响,同一个面元上的各道地震数据也会存在较大的差异。在地震数据处理中,为了获得能够真实反映地下地质异常体的高保真、高精度、高分辨率的地震勘探数据成果,需要分析并剔除或压制非地下地质异常体的地震响应。其中,非地下地质异常体的地震响应包括震源激发能量差异和检波器接收能量灵敏度差异,它们的影响属于采集足痕的范畴。在地震数据处理流程中,剔除或压制震源激发能量差异的影响和检波器接收能量灵敏度差异的影响的技术,被称为地表一致性振幅补偿。该技术的目的就是在经过处理之后,地震数据体符合地表一致性原理:即无论是哪个物理点位置的震源激发,也不管激发震源的性能和型号,它们所激发的平均能量或能量密度都相等;无论在哪个物理点位置接收,也不管用哪个检波器接收,它们所接收到的平均能量或能量密度都相等。Seismic exploration technology is one of the important exploration methods and technologies in the fields of energy exploration engineering, geological engineering and engineering geophysical exploration. In the results of seismic exploration and interpretation, a variety of seismic attributes can be used to detect geological anomalies, and the amplitude properties and their ancillary products play an extremely important role. In the field of seismic exploration field data acquisition, due to the application of multiple coverage techniques, the seismic data on the same bin will come from different excitation sources and different detectors. Therefore, due to the difference in the characteristics of the excited source and the difference in the characteristics of the detector, there will be a large difference in the seismic data of the same surface. In seismic data processing, in order to obtain high-fidelity, high-precision, high-resolution seismic exploration data that can truly reflect underground geological anomalies, it is necessary to analyze and eliminate or suppress the seismic response of non-subterranean geological anomalies. Among them, the seismic response of non-subterranean geological anomalies includes the difference between the excitation energy of the source and the sensitivity of the received energy of the detector, and their influence belongs to the category of collecting foot marks. In the seismic data processing flow, the technique of rejecting or suppressing the influence of the excitation energy difference of the source and the influence of the difference in the sensitivity of the received energy of the detector is called surface consistency amplitude compensation. The purpose of this technique is that after processing, the seismic data body conforms to the principle of surface consistency: that is, regardless of the source excitation of the physical point location, and regardless of the performance and model of the excitation source, the average energy or energy density they excite is equal. Regardless of which physical point location is received, and which detector is used for reception, the average energy or energy density they receive is equal.
目前,国内外工业界在地震勘探数据处理过程中,地表一致性振幅补偿是一个关键环节。所采用的方法原理就是先统计全工区的平均能量,将其除以各道的能量得出各道的总补偿因子,其后将总补偿因子分解为震源因子、检波器因子、炮检距因子、构造项因子等,最后通过高斯—赛德尔迭代计算从而获得最终的补偿因子,并用来进行地表一致性振幅补偿。具体的,对于多波地震勘探(有时也称转换波地震勘探,或者3D3C地震勘探),相关技术提供了一种地表一致性振幅补偿方法,即先分别对检波器接收的各个分量进行地表一致性振幅补偿因子计算,保持各个分量中的各个检波器补偿因子不变,将所有分量的各个震源补偿因子的平均值作为最终的震源补偿因子,最后根据该最终的震源补偿因子进行地表一致性振幅补偿。在实际应用中,单分量和三分量的地表一致性振幅补偿都得到了广泛应用,一定程度上解决了非地质异常引起的振幅差异问题。At present, in the process of seismic exploration data processing at home and abroad, the surface consistency amplitude compensation is a key link. The principle of the method used is to first calculate the average energy of the whole work area, divide it by the energy of each track to obtain the total compensation factor of each track, and then decompose the total compensation factor into the source factor, detector factor, and offset factor. , the construction factor, etc., finally through the Gauss-Sedel iterative calculation to obtain the final compensation factor, and used to perform surface consistency amplitude compensation. Specifically, for multi-wave seismic exploration (sometimes called converted wave seismic exploration, or 3D3C seismic exploration), the related art provides a surface consistency amplitude compensation method, that is, firstly performing surface consistency on each component received by the detector. The amplitude compensation factor is calculated, and the compensation factors of each detector in each component are kept unchanged. The average value of each source compensation factor of all components is used as the final source compensation factor, and finally the surface consistency amplitude compensation is performed according to the final source compensation factor. . In practical applications, the single-component and three-component surface consistency amplitude compensation has been widely used, which solves the amplitude difference caused by non-geological anomalies to some extent.
不过,随着高保真、高精度、高分辨率地震勘探方法研究和实践应用的不断推进,目前的地表一致性振幅补偿方法和技术存在两个方面问题需要解决:(1)对于共检波点道集中所有地震数据进行地表一致性补偿因子 计算时,忽略了多次覆盖技术野外施工过程中相同检波器物理位置上会存在多次不同时间布设的检波器,默认它们与大地的耦合程度和接收信号的灵敏度相同。这与工业生产中的实际情况是不相符的,由于多次覆盖技术的使用,在相同的物理点位置会存在同一个检波器不同时间的布设情况,而实际操作中不同时间布设的检波器均不相同,即使有个别检波器相同,也会因为不同时间的布设条件不同而致使该检波器与大地的耦合程度不一样,而检波器的灵敏度和其与大地的耦合程度,都直接影响该检波器所记录到的振幅差异,进而影响地表一致性补偿的效果。这一问题在多波地震勘探和纵波地震勘探中都存在。(2)在多波地震勘探中,分别对三分量的地震数据进行地表一致性振幅补偿计算和校正,会破坏三分量之间的相互关系。这会严重影响多波勘探中的快慢波时差特性和方位特性,将会误导裂隙探测结果。另外,在全波形高保真反演中,不仅需要保持两个横波分量的振幅关系,而且也要保持纵波分量与横波分量之间的能量关系。However, with the continuous advancement of high-fidelity, high-precision, high-resolution seismic exploration methods and practical applications, the current surface consistency amplitude compensation methods and techniques have two problems to be solved: (1) for common detection wave points Concentrate all seismic data for surface consistency compensation factors In the calculation, it is neglected that the detectors in the physical position of the same detector in the field of multiple coverage techniques will have multiple detectors arranged at different times. By default, the coupling degree with the earth and the sensitivity of the received signal are the same. This is inconsistent with the actual situation in industrial production. Due to the use of multiple coverage techniques, the same detector can be placed at different physical locations at different times, and the detectors deployed at different times in actual operation are Different, even if the individual detectors are the same, the coupling degree of the detector to the earth is different due to different laying conditions at different times, and the sensitivity of the detector and its coupling with the earth directly affect the detection. The difference in amplitude recorded by the device, which in turn affects the effect of surface consistency compensation. This problem exists in both multi-wave seismic exploration and longitudinal wave seismic exploration. (2) In multi-wave seismic exploration, the calculation and correction of surface consistency amplitude compensation for the three-component seismic data respectively will destroy the relationship between the three components. This will seriously affect the fast and slow wave time difference characteristics and azimuth characteristics in multi-wave exploration, and will mislead the crack detection results. In addition, in the full-waveform high-fidelity inversion, it is necessary to maintain not only the amplitude relationship of the two transverse wave components but also the energy relationship between the longitudinal wave component and the transverse wave component.
发明人在研究中发现,上述两方面因素均对地震数据处理成果的保真度产生严重影响,目前缺少一种方法能够较好地进行地表一致性振幅补偿。本发明针对上述两方面的因素提出了一种新的地表一致性振幅补偿方法。The inventors found in the study that the above two factors have a serious impact on the fidelity of seismic data processing results. At present, there is a lack of a method to better perform surface consistency amplitude compensation. The invention proposes a new ground surface consistency amplitude compensation method for the above two factors.
发明内容Summary of the invention
本发明的目的在于提供一种共姿态道集地表一致性振幅补偿方法及装置,使得地表一致性补偿结果更加精确。It is an object of the present invention to provide a method and apparatus for compensating amplitude consistency of a common attitude gather set surface, so that the surface consistency compensation result is more accurate.
第一方面,本发明实施例提供了一种共姿态道集地表一致性振幅补偿方法,包括:In a first aspect, an embodiment of the present invention provides a method for coherent amplitude compensation of a common attitude gather set surface, including:
获取勘探工区中的地震数据及该地震数据对应的施工班报;Obtaining seismic data in the exploration work area and the construction work report corresponding to the seismic data;
计算地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量;Calculating the average total energy of all components of each seismic data in the seismic data to obtain the seismic energy of the track;
对各个地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体;Performing a preliminary test of surface consistency for each seismic energy, and determining all seismic energy of the first predetermined condition as a representative data volume;
在具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,各项补偿因子至少包括震源项补偿因子;Calculating each compensation factor corresponding to each track energy in a representative data body, and each compensation factor includes at least a source term compensation factor;
根据检波器的预设姿态,在勘探工区的地震数据的共检波点道集中抽取共姿态道集,并在共姿态道集中计算检波器项补偿因子;According to the preset posture of the detector, the common attitude gathers are collected in the common detection wave track of the seismic data of the exploration work area, and the detector item compensation factor is calculated in the common attitude track set;
根据各项补偿因子以及检波器项补偿因子构成的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿。According to the compensation factors and the total compensation factor composed of the detector term compensation factor, the surface consistency amplitude compensation of the seismic data of the entire work area is performed.
结合第一方面,本发明实施例提供了第一方面的第一种可能的实施方式,其中,地震数据包括单分量地震数据和三分量地震数据;With reference to the first aspect, an embodiment of the present invention provides a first possible implementation manner of the first aspect, wherein the seismic data includes single component seismic data and three component seismic data;
计算地震数据中每一道地震数据的所有分量的平均总能量包括: Calculating the average total energy of all components of each seismic data in the seismic data includes:
根据公式
Figure PCTCN2015074246-appb-000001
计算地震道数据中每一道数据的所有分量的平均总能量,得到每一道的地震道能量;公式中T为时窗长度,N为地震数据的分量个数,Cn,t为第n分量在时窗内第t采样点的振幅值。
According to the formula
Figure PCTCN2015074246-appb-000001
Calculate the average total energy of all components of each data in the seismic trace data to obtain the seismic energy of each channel; in the formula, T is the length of the time window, N is the number of components of the seismic data, and C n,t is the nth component. The amplitude value of the t-th sample point in the time window.
结合第一方面的第一种可能的实施方式,本发明实施例提供了第一方面的第二种可能的实施方式,其中,所述方法还包括:对各个地震道能量进行地表一致性初步检验,并将符合第二预设条件的所有地震道能量构成疑似非地表一致性数据体;With reference to the first possible implementation manner of the first aspect, the embodiment of the present invention provides the second possible implementation manner of the first aspect, wherein the method further includes: performing a preliminary check on the surface consistency of each seismic energy And all seismic energy that meets the second preset condition constitutes a suspected non-surface consistent data volume;
对各个地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体包括:A preliminary test of surface consistency is performed for each seismic energy, and all seismic energy of the first predetermined condition is determined as a representative data body including:
分别根据公式
Figure PCTCN2015074246-appb-000002
计算勘探工区中所有地震道能量的平均值和均方差,得到工区的平均值和均方差;其中,公式中M是整个勘探工区的地震道总数;
According to the formula
Figure PCTCN2015074246-appb-000002
Calculate the mean and mean square error of all seismic energy in the exploration area, and obtain the average and mean square error of the work area; where M is the total number of seismic traces in the entire exploration area;
统计与工区的平均值之差处于3倍工区的均方差区域内的地震道能量,并将该地震道能量作为具有代表性的数据体;The difference between the statistical and the average value of the work area is the seismic energy in the mean square error region of the work area of 3 times, and the energy of the seismic track is taken as a representative data body;
对各个地震道能量进行地表一致性初步检验,并将符合第二预设条件的所有地震道能量构成疑似非地表一致性数据体,包括:A preliminary test of surface consistency is performed for each seismic energy, and all seismic energy that meets the second preset condition constitutes a suspected non-surface consistent data body, including:
统计与工区的平均值之差处于3倍工区的均方差区域外的地震道能量,并将该地震道能量作为疑似非地表一致性数据体。The difference between the statistical and the average of the work area is the seismic energy outside the mean square error region of the work area, and the energy of the seismic trace is used as the suspected non-surface consistent data volume.
结合第一方面的第一种可能的实施方式,本发明实施例提供了第一方面的第三种可能的实施方式,其中,各项补偿因子还包括:炮检距项补偿因子和构造项补偿因子。With reference to the first possible implementation manner of the first aspect, the embodiment of the present invention provides a third possible implementation manner of the first aspect, wherein each compensation factor further includes: a offset component compensation factor and a structural item compensation factor.
结合第一方面的第二种可能的实施方式或第一方面的第三种可能的实施方式,本发明实施例提供了第一方面的第四种可能的实施方式,其中,所述方法还包括:With reference to the second possible implementation manner of the first aspect or the third possible implementation manner of the first aspect, the embodiment of the present invention provides the fourth possible implementation manner of the first aspect, wherein the method further includes :
对于单分量地震数据,在共检波点道集中将施工班报记录的检波器不同布设时间内的地震道能量,作为对应的共姿态道集;For the single-component seismic data, the seismic energy of the detectors recorded in the construction class report is set in the common detection wave track as the corresponding common attitude gather;
对于三分量地震数据,根据地震采集系统测量的三个分量各自倾角的大小以及施工班报记录,在共检波点道集中抽取检波器不同布设时间内的地震道能量,构成对应的共姿态道集。For the three-component seismic data, according to the respective dip angles of the three components measured by the seismic acquisition system and the construction class report records, the seismic trace energy of the detectors in different sets of time is extracted from the common detection wave track to form a corresponding common attitude gather. .
结合第一方面的第四种可能的实施方式,本发明实施例提供了第一方面的第五种可能的实施方式,其中,在共姿态道集中计算检波器项补偿因子,包括: With reference to the fourth possible implementation manner of the first aspect, the embodiment of the present invention provides the fifth possible implementation manner of the first aspect, wherein calculating the detector item compensation factor in the common attitude track set includes:
根据公式
Figure PCTCN2015074246-appb-000003
在共姿态道集中计算检波器项补偿因子;其中,Scaleα是与第A共姿态道集相关的补偿因子期望值,Nα是该共姿态道集中包括的所有地震数据的道数。
According to the formula
Figure PCTCN2015074246-appb-000003
The detector term compensation factor is calculated in the co-statue track set; wherein Scale α is the compensation factor expectation value associated with the A-co-coordinate track set, and N α is the number of tracks of all seismic data included in the co-statue track set.
结合第一方面的第五种可能的实施方式,本发明实施例提供了第一方面的第六种可能的实施方式,其中,所述方法还包括:根据高斯—赛德尔迭代方法,计算各项补偿因子和检波器项补偿因子;其中高斯—赛德尔迭代方法包括公式:With reference to the fifth possible implementation manner of the first aspect, the embodiment of the present invention provides a sixth possible implementation manner of the first aspect, wherein the method further includes: calculating each item according to a Gauss-Seidel iterative method Compensation factor and detector term compensation factor; wherein the Gauss-Seidel iterative method includes a formula:
Figure PCTCN2015074246-appb-000004
Figure PCTCN2015074246-appb-000004
式中,Ss、Aα、Oo和Cc分别为震源项补偿因子、检波器项补偿因子、炮检距项补偿因子和构造项补偿因子,Scalem,s,α,o,c为总补偿因子。Where S s , A α , O o and C c are the source term compensation factor, the detector term compensation factor, the offset term compensation factor and the structural term compensation factor, respectively, Scale m, s, α, o, c are Total compensation factor.
结合第一方面的第六种可能的实施方式,本发明实施例提供了第一方面的第七种可能的实施方式,其中,对整个工区的地震数据进行地表一致性振幅补偿,包括:With reference to the sixth possible implementation manner of the first aspect, the embodiment of the present invention provides the seventh possible implementation manner of the first aspect, wherein the ground data consistency amplitude compensation is performed on the seismic data of the entire work area, including:
根据公式log(Scalem,s,α,o,c)=log(Sm,s)+log(Am,α)+log(Om,o)+log(Cm,c),计算各地震道数据的总补偿因子;Calculate each according to the formula log(Scale m, s, α, o, c )=log(S m,s )+log(A m,α )+log(O m,o )+log(C m,c ) Total compensation factor for seismic trace data;
根据总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿;According to the total compensation factor, the surface consistency amplitude compensation is performed on the seismic data of the entire work area;
所述方法还包括:The method further includes:
对疑似非地表一致性数据体进行地表一致性振幅补偿,并计算补偿后的疑似非地表一致性数据体的地震道能量;Performing surface consistency amplitude compensation on the suspected non-surface consistent data volume, and calculating the seismic energy of the compensated suspected non-surface consistent data volume;
计算地表一致性振幅补偿后的具有代表性的数据体的所有地震道能量的平均值和均方差,并根据该平均值和均方差对疑似非地表一致性数据体的地震道能量进行验证,得到验证结果;Calculate the mean and mean square error of all seismic energy of a representative data volume after surface uniform amplitude compensation, and verify the seismic energy of the suspected non-surface consistent data volume based on the average and the mean square error Validation results;
在确定验证结果符合第一预设条件时,保留疑似非地表一致性数据体中的对应地震道数据并对其进行地表一致性振幅补偿;When it is determined that the verification result meets the first preset condition, the corresponding seismic trace data in the suspected non-surface consistent data volume is retained and subjected to surface consistency amplitude compensation;
在确定验证结果符合第二预设条件时,剔除疑似非地表一致性数据体中对应地震道数据或者对其进行非地表一致性振幅补偿。 When it is determined that the verification result meets the second preset condition, the corresponding seismic trace data in the suspected non-surface consistent data volume is rejected or non-surface consistency amplitude compensation is performed.
结合第一方面的第七种可能的实施方式,本发明实施例提供了第一方面的第八种可能的实施方式,其中,对疑似非地表一致性数据体中对应地震道数据进行非地表一致性振幅补偿包括:With reference to the seventh possible implementation manner of the first aspect, the embodiment of the present invention provides the eighth possible implementation manner of the first aspect, wherein the non-surface consistency is performed on the corresponding seismic trace data in the suspected non-surface consistent data volume The amplitude compensation includes:
按照公式
Figure PCTCN2015074246-appb-000005
计算具有代表性的数据体中对应地震数据经过地表一致性振幅补偿之后的期望值,其中,公式中K是具有代表性的数据体中地震道的总数;
According to the formula
Figure PCTCN2015074246-appb-000005
Calculating the expected value of the corresponding seismic data in the representative data volume after the surface consistency amplitude compensation, wherein K is the total number of seismic traces in the representative data volume;
按照公式Scalem=Expect/Engm,计算非地表一致性补偿因子作为最终的补偿因子;Calculate the non-surface consistency compensation factor as the final compensation factor according to the formula Scale m =Expect/Eng m ;
根据最终的补偿因子,对疑似非地表一致性数据体中对应地震道数据进行非地表一致性振幅补偿。According to the final compensation factor, the non-surface consistency amplitude compensation is performed on the corresponding seismic trace data in the suspected non-surface consistent data volume.
第二方面,本发明实施例还提供了一种共姿态道集地表一致性振幅补偿装置,包括:In a second aspect, an embodiment of the present invention further provides a co-attack gather surface consistency amplitude compensation apparatus, including:
获取单元,用于获取勘探工区中的地震数据及其对应的施工班报;An acquisition unit, configured to acquire seismic data in a exploration work area and a corresponding construction work report;
第一计算单元,用于计算获取单元获取的地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量;a first calculating unit, configured to calculate an average total energy of all components of each seismic data in the seismic data acquired by the acquiring unit, to obtain seismic channel energy of the track;
检验单元,用于对各个第一计算单元计算得到的地震道能量进行地表一致性初步检验;a verification unit, configured to perform a preliminary test of surface consistency on the seismic energy calculated by each first computing unit;
第一确定单元,用于将符合第一预设条件的所有地震道能量确定为具有代表性的数据体;a first determining unit, configured to determine all seismic energy of the first predetermined condition as a representative data volume;
第二计算单元,用于在第一确定单元确定的具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,各项补偿因子至少包括震源项补偿因子;a second calculating unit, configured to calculate, in a representative data body determined by the first determining unit, each compensation factor corresponding to each track energy, and each compensation factor includes at least a source term compensation factor;
抽取单元,用于根据检波器的不同姿态,在勘探工区的共检波点道集中抽取共姿态道集;The extracting unit is configured to extract a common attitude gather in the common detection wave point of the exploration work area according to different postures of the detector;
第三计算单元,用于在抽取单元抽取的共姿态道集中计算检波器项补偿因子;a third calculating unit, configured to calculate a detector term compensation factor in the common attitude track set extracted by the extracting unit;
地表一致性振幅补偿单元,用于根据第二计算单元计算得到的各项补偿因子以及第三计算单元计算得到的检波器项补偿因子构成的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿。The surface consistency amplitude compensation unit is configured to perform surface consistency on the seismic data of the entire work area according to the compensation factors calculated by the second calculation unit and the total compensation factor formed by the detector item compensation factor calculated by the third calculation unit. Amplitude compensation.
本发明实施例提供的共姿态道集地表一致性振幅补偿方法及装置,首先获取勘探工区中的地震数据及该地震数据对应的施工班报;然后计算地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量;接着对各个地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体;然后在具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,并在共姿态道集中计算检波器项补偿因子;最后根据各项补偿因子以及检波器项补偿因子构成的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿,与现 有技术的缺少一种方法能够较好的进行地表一致性振幅补偿相比,其考虑到了三分量数据之间的能量投影三角函数关系,将三分量地震数据一起计算,使得计算结果更准确,为后续地表一致性补偿打下了坚实的基础,并且,考虑到检波器的布设姿态,在共姿态道集中计算检波器项补偿因子,同样使得计算结果更准确,这二者都是得地表一致性的结果更加准确。The method and device for coherent track gather surface consistency amplitude compensation provided by the embodiments of the present invention firstly acquire seismic data in a exploration work area and a construction work report corresponding to the seismic data; and then calculate all components of each seismic data in the seismic data. Average total energy, obtain the seismic energy of the track; then perform a preliminary test of the surface consistency of each seismic energy, and determine all the seismic energy of the first preset condition as a representative data volume; The representative data body calculates each compensation factor corresponding to each track energy, and calculates the detector term compensation factor in the common attitude track set; finally, according to the compensation factors and the total compensation factor composed of the detector term compensation factor, Performing surface consistency amplitude compensation for seismic data of the entire work area, and present There is a lack of a technique to better perform surface consistency amplitude compensation. Considering the energy projection trigonometric function relationship between three component data, the three-component seismic data is calculated together to make the calculation result more accurate. Subsequent surface consistency compensation lays a solid foundation, and considering the placement posture of the detector, calculating the detector term compensation factor in the common attitude track also makes the calculation result more accurate, both of which are ground-consistent. The result is more accurate.
进一步的,本发明提供的共姿态道集地表一致性振幅补偿方法及装置,除了做地表一致性振幅补偿外,还对疑似非地表一致性地震道进行非地表一致性振幅补偿,使得对地震道数据的补偿结果更加准确。Further, the method and device for compensating the amplitude uniformity of the common attitude gathers on the ground surface of the present invention provide non-surface consistency amplitude compensation for the suspected non-surface consistent seismic traces, so that the seismic traces are The compensation result of the data is more accurate.
附图说明DRAWINGS
为了更清楚地说明本发明实施例的技术方案,下面将对实施例中所需要使用的附图作简单地介绍,应当理解,以下附图仅示出了本发明的某些实施例,因此不应被看作是对范围的限定。In order to more clearly illustrate the technical solutions of the embodiments of the present invention, the drawings used in the embodiments will be briefly described below. It should be understood that the following drawings show only certain embodiments of the present invention, and therefore It should be seen as a limitation of scope.
图1示出了本发明实施例所提供的一种观测系统示意图;FIG. 1 is a schematic diagram of an observation system according to an embodiment of the present invention;
图2示出了本发明实施例所提供的关于图1中单一姿态下Z分量的单分量与三分量地表一致性振幅补偿效果对比示意图;2 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the Z component in the single attitude of FIG. 1 according to an embodiment of the present invention;
图3示出了本发明实施例所提供的关于图1中单一姿态下X分量的单分量与三分量地表一致性振幅补偿效果对比示意图;FIG. 3 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the X component in the single attitude of FIG. 1 according to an embodiment of the present invention; FIG.
图4示出了本发明实施例所提供的关于图1中单一姿态下Y分量的单分量与三分量地表一致性振幅补偿效果对比示意图;4 is a schematic diagram showing a comparison of the amplitude compensation effects of the single component and the three component surface uniformity of the Y component in the single attitude of FIG. 1 according to an embodiment of the present invention;
图5示出了本发明实施例所提供的关于图1中单一姿态下地表出射角的对比示意图;FIG. 5 is a schematic view showing comparison of the surface exit angles in a single attitude in FIG. 1 according to an embodiment of the present invention; FIG.
图6示出了本发明实施例所提供的关于图1中单一姿态下的炮检方位角的对比示意图;6 is a schematic diagram showing a comparison of the azimuth angles of the inspection in a single attitude in FIG. 1 according to an embodiment of the present invention;
图7示出了本发明实施例所提供的一种观测系统滚动施工布置示意图;FIG. 7 is a schematic diagram showing a rolling construction arrangement of an observation system according to an embodiment of the present invention; FIG.
图8示出了本发明实施例所提供的关于图1中多种姿态下的Z分量的目前方法与本发明的地表一致性振幅补偿效果对比示意图;8 is a schematic diagram showing a comparison between the current method for the Z component in various postures in FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention;
图9示出了本发明实施例所提供的关于图1中多种姿态下的X分量的目前方法与本发明的地表一致性振幅补偿效果对比示意图;FIG. 9 is a schematic diagram showing a comparison between the current method for the X component in various postures of FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention; FIG.
图10示出了本发明实施例所提供的关于图1中多种姿态下的Y分量的目前方法与本发明的地表一致性振幅补偿效果对比示意图;FIG. 10 is a schematic diagram showing a comparison between the current method for the Y component in various postures of FIG. 1 and the surface consistency amplitude compensation effect of the present invention provided by the embodiment of the present invention; FIG.
图11示出了本发明实施例所提供的共姿态道集地表一致性振幅补偿方法的流程图;FIG. 11 is a flowchart of a method for compensating amplitude consistency of a common attitude gather set surface according to an embodiment of the present invention;
图12示出了本发明实施例所提供的共姿态道集地表一致性振幅补偿装置的结构示意图。FIG. 12 is a schematic structural diagram of a co-attend track gather surface consistency amplitude compensation apparatus according to an embodiment of the present invention.
具体实施方式detailed description
下面将结合本发明实施例中附图,对本发明实施例中的技术方案进行清楚、完整地描述,显然,所描述的实施例仅仅是本发明一部分实施例, 而不是全部的实施例。通常在此处附图中描述和示出的本发明实施例的组件可以以各种不同的配置来布置和设计。因此,以下对在附图中提供的本发明的实施例的详细描述并非旨在限制要求保护的本发明的范围,而是仅仅表示本发明的选定实施例。基于本发明的实施例,本领域技术人员在没有做出创造性劳动的前提下所获得的所有其他实施例,都属于本发明保护的范围。The technical solutions in the embodiments of the present invention are clearly and completely described in the following with reference to the accompanying drawings in the embodiments of the present invention. It is obvious that the described embodiments are only a part of the embodiments of the present invention. Rather than all embodiments. The components of the embodiments of the invention, which are generally described and illustrated in the figures herein, may be arranged and designed in various different configurations. Therefore, the following detailed description of the embodiments of the invention in the claims All other embodiments obtained by those skilled in the art based on the embodiments of the present invention without creative efforts are within the scope of the present invention.
本发明涉及多波三分量(包括纵波单分量)地震勘探中地表一致性振幅补偿,提出一种新的振幅补偿方法,便于准确分析地表一致性补偿因子并予以校正,为数据处理和解释反演提供高质量的地震数据,促进地震勘探的科学研究和工业应用。本发明的特点是:The invention relates to surface consistency amplitude compensation in multi-wave three-component (including longitudinal wave single component) seismic exploration, and proposes a new amplitude compensation method for accurately analyzing and correcting surface consistency compensation factors for data processing and interpretation inversion. Provide high-quality seismic data to promote scientific research and industrial applications in seismic exploration. The features of the invention are:
第一,三分量地表一致性振幅补偿因子的计算需要三个分量一起计算,不能分开单独进行。为了做好高保真的全波反演,以及横波探测裂隙技术,需要保持纵横波之间以及横波分量之间的振幅能量关系,因此三分量地震勘探中,地表一致性振幅补偿因子计算需要将三个分量的总能量当成一个单一分量来进行。现有技术一般是分别对三个分量进行单独的因子分析,保持其它各项因子不变,选取各个分量的震源因子的平均值作为所有分量的最终震源因子。这在一定程度上解决了震源因子的一致性问题,但是忽视了地震体波能量在各个分量之间的能量关系的差异问题。First, the calculation of the three-component surface consistency amplitude compensation factor requires three components to be calculated together and cannot be performed separately. In order to do high-fidelity full-wave inversion and shear wave detection cracking technology, it is necessary to maintain the amplitude energy relationship between the longitudinal and transverse waves and between the shear wave components. Therefore, in the three-component seismic exploration, the calculation of the surface uniform amplitude compensation factor needs to be three. The total energy of the components is treated as a single component. In the prior art, a separate factor analysis is performed on the three components, and the other factors are kept unchanged, and the average value of the source factors of each component is selected as the final source factor of all components. This solves the problem of the consistency of the source factor to a certain extent, but ignores the difference in the energy relationship between the individual components of the seismic body wave energy.
其中,总的体波能量Eng在X、Y、Z三个分量上的能量与地表出射角
Figure PCTCN2015074246-appb-000006
和炮检方位角α之间的关系可表示为
Among them, the total body wave energy Eng in the three components of X, Y, Z and the surface exit angle
Figure PCTCN2015074246-appb-000006
The relationship between the azimuth angle α and the detected azimuth α can be expressed as
Figure PCTCN2015074246-appb-000007
Figure PCTCN2015074246-appb-000007
三分量地震勘探中的总能量可表示为The total energy in a three-component seismic survey can be expressed as
Figure PCTCN2015074246-appb-000008
Figure PCTCN2015074246-appb-000008
目前,还有另外一种振幅补偿方案:即将纵横波分量分开进行,横波分量中其总能量当成一个单分量进行地表一致性振幅补偿。该方案一定程度上保障了横波分量之间的能量关系,有利于利用两个横波分量及其处理之后的快慢波分量进行利裂隙检测。但是,该方案仍然破坏了纵波能量与横波能量之间的相互关系,在全波形反演等技术应用中会产生误解。At present, there is another amplitude compensation scheme: the longitudinal and transverse wave components are separated, and the total energy of the transverse wave component is treated as a single component for surface uniform amplitude compensation. The scheme guarantees the energy relationship between the shear wave components to a certain extent, and is beneficial to utilize the two shear wave components and the fast and slow wave components after the processing to perform the crack detection. However, this scheme still destroys the relationship between the longitudinal wave energy and the shear wave energy, and it will be misunderstood in the application of full waveform inversion.
如图1所示,在本发明实施例所提供的一种观测系统示意图中,星形符号代表炮点,共10条炮线,每线10炮,点、线距均为60米;三角形代表检波点,共24条检波线,每线24个检波器,点、线距均为50米。分别对各个炮点、检波点随机产生不同的能量放大倍数因子,全区中各道的能量因子为对应炮点和检波点的因子乘积。设计了两层地质模型,界面深度为800米,上下层的纵波速度分别为2400m/s和3000m/s,横波速度为800m/s和1000m/s,密度为2.0kg/m3和2.3kg/m3。通过Zeoppritz公式计算出纵波入射 时各道的纵、横波反射系数,将两者平方和作为体波总能量的平方;在风化层的影响假设各道的地表出射角为其纵波反射角的1/3;炮检方位角的零度从X轴正向开始,逆时针为正;X分量横波检波器方位角指向X轴正向。各道所接收到的总能量为体波总能量与对应炮点因子和检波点因子的乘积,三分量的振幅按照公式(1)计算。As shown in FIG. 1 , in a schematic diagram of an observation system provided by an embodiment of the present invention, a star symbol represents a shot, a total of 10 shot lines, 10 shots per line, and the point and line spacing are both 60 meters; The detection point, a total of 24 detector lines, 24 detectors per line, point and line spacing are 50 meters. Different energy amplification factors are randomly generated for each shot point and detection point respectively, and the energy factor of each track in the whole area is the factor product of the corresponding shot point and the detection point. A two-layer geological model was designed with an interface depth of 800 m. The longitudinal wave velocities of the upper and lower layers were 2400 m/s and 3000 m/s, the shear wave velocities were 800 m/s and 1000 m/s, and the density was 2.0 kg/m 3 and 2.3 kg/ m 3 . The longitudinal and transverse wave reflection coefficients of each channel when the longitudinal wave is incident are calculated by the Zeoppritz formula, and the sum of the squares is taken as the square of the total energy of the body wave. The influence of the weathering layer assumes that the surface emission angle of each channel is 1/1 of the longitudinal wave reflection angle. 3; the zero degree of the azimuth of the inspection is from the positive X-axis, and the counterclockwise is positive; the azimuth of the X-component transverse wave detector is directed to the positive X-axis. The total energy received by each channel is the product of the total body wave energy and the corresponding shot point factor and the detection point factor. The amplitude of the three components is calculated according to formula (1).
在模型记录上进行地表一致性振幅补偿分析和校正。首先,采用现有技术进行分析,即三分量分开实施炮点和检波点的地表一致性振幅补偿分析,然后保持检波点因子不变,将三个分量的炮点因子的平均值作为最终的炮点因子,再实施振幅补偿。其次采用本发明中的新方法,即将按照公式(2)计算各道的三分量的总能量,然后将总能量当成一个单分量进行地表一致性振幅补偿分析,得到炮点和检波点的补偿因子,最后三个分量均使用相同的炮点和检波点补偿因子进行振幅补偿。Surface consistency amplitude compensation analysis and correction were performed on the model record. Firstly, the analysis is performed by the prior art, that is, the three-component separately performs the surface consistency amplitude compensation analysis of the shot point and the detection point, and then the detection point factor is kept unchanged, and the average value of the shot factors of the three components is used as the final shot. Point factor, then perform amplitude compensation. Secondly, using the new method of the present invention, the total energy of the three components of each track is calculated according to formula (2), and then the total energy is treated as a single component for surface consistency amplitude compensation analysis, and the compensation factors of the shot and the detection point are obtained. The last three components use the same shot and detection point compensation factor for amplitude compensation.
具体的,在图2-图4中依次展示了Z、X、Y分量两种不同方法的效果对比。在图2-图4这三幅图中,依次显示原始振幅,现有技术补偿之后的振幅和本发明技术补偿之后的振幅。从图2-图4中均可以看到,现有技术和本发明技术都能较好地实施振幅补偿,Z分量的振幅相对差异从最大4倍左右校正到1倍附近,X和Y分量的振幅相对差异从-10~10倍校正到-3~3倍。Specifically, the effect comparison of two different methods of Z, X, and Y components is sequentially shown in FIG. 2 to FIG. 4. In the three figures of Figures 2 - 4, the original amplitude, the amplitude after compensation in the prior art and the amplitude after compensation by the technique of the present invention are sequentially displayed. It can be seen from both FIG. 2 and FIG. 4 that both the prior art and the technique of the present invention can perform amplitude compensation well, and the relative difference in amplitude of the Z component is corrected from about 4 times to about 1 time, and the X and Y components are The relative amplitude difference is corrected from -10 to 10 times to -3 to 3 times.
但是,如果仔细分析两者的补偿结果在三分量之间的能量关系,会发现两者补偿效果差异明显。如图5所示,图中从上到下依次为原始的地表出射角、现有技术补偿之后的地表出射角、本发明技术补偿之后的地表出射角以及现有技术补偿之后的出射角误差。从图5中可以看到,本发明技术补偿之后的地表出射角与原始出射角一致,而现有技术补偿之后的出射角误差在-9°~3°,这严重破坏了纵波能量与横波能量之间的相互关系。However, if the energy relationship between the two components is carefully analyzed, the difference between the two compensation effects will be obvious. As shown in Fig. 5, the top surface of the figure is the original surface exit angle, the surface exit angle after prior art compensation, the surface exit angle after compensation by the technique of the present invention, and the exit angle error after prior art compensation. It can be seen from FIG. 5 that the surface exit angle after compensation by the technique of the present invention is consistent with the original exit angle, and the exit angle error after compensation in the prior art is -9° to 3°, which seriously destroys the longitudinal wave energy and the shear wave energy. The relationship between them.
另外,在横波方位角分析中,现有技术同样产生了较大的误差。图6中展示了方位角误差对比情况,从上到下依次为原始的炮检方位角、现有技术补偿之后的检波器方位角、本发明技术补偿之后的检波器方位角以及现有技术补偿之后的方位角误差。从图6中可以看到,本发明技术补偿之后的检波器方位角与原始方位角一致,而现有技术补偿之后的方位角误差较大,误差范围在-50°~50°。In addition, in the analysis of the transverse wave azimuth, the prior art also produces a large error. The azimuthal error comparison is shown in Figure 6, from top to bottom, the original azimuth, the detector azimuth after prior art compensation, the detector azimuth after the technique of the present invention, and prior art compensation. Azimuth error afterwards. As can be seen from Fig. 6, the azimuth of the detector after compensation by the technique of the present invention is consistent with the original azimuth angle, and the azimuth error after compensation in the prior art is large, and the error range is -50 to 50.
综上所述,目前的三分量地表一致性振幅补偿方法不能保持各个分量之间的能量关系,而本发明提出的新方法能够做到。In summary, the current three-component surface consistency amplitude compensation method cannot maintain the energy relationship between the components, and the new method proposed by the present invention can do this.
第二,提出共姿态道集地表一致性振幅补偿方法,检波器补偿因子的计算在共姿态道集中进行。Secondly, a method for coherent amplitude compensation of the common attitude gathers is proposed. The calculation of the detector compensation factors is performed in the common attitude gather.
所谓共姿态道集,即是在共检波点道集中将按照该检波器的不同姿态(包括三个分量检波器的倾角和横波分量的方位角)划分,抽取出不同地震数据重新组成的子道集。在地震勘探野外采集过程中,多次覆盖技术是通用技术。为了获得均匀的覆盖次数,地震观测系统将按照设计要求向前移动一定的距离,滚动施工。一般在两束观测系统的结合部,相同检波器 物理位置会在不同的施工时间上布设不同的检波器。如图7所示,上图是一个单片的观测系统,下图是滚动之后的观测系统,一共两束,每束三片,分别数字1~6标注,数字序号也表示滚动施工的先后顺序。在图7中的1、2单片和5、6单片的重合部,同一检波器位置就会至少两次布设检波器,即至少有两个不同的姿态。实际施工中,由于各种原因往往还会存在多于两种姿态的检波器布设情况。例如在本发明实施应用中的某个三分量地震勘探项目中,全区共有7261个检波器物理点位置,实际共姿态道集为36342个,平均每个检波器物理点约5个姿态,最多的一个检波器位置有21个姿态。于是相同检波器位置上,因为不同时间布设的检波器不同,故检波器的灵敏度和该检波器与大地的耦合程度也不同。即使偶然有相同检波器在不同时间布设到相同的检波器物理点位置上,其灵敏度相同但是会因布设条件不同导致与大地的耦合程度不同。The so-called common attitude gathers, that is, in the common detector locus set, according to different postures of the detector (including the inclination angles of the three component detectors and the azimuth of the transverse wave components), the sub-tracks composed of different seismic data are extracted. set. In the field of seismic exploration field acquisition, multiple coverage techniques are common techniques. In order to obtain a uniform coverage, the seismic observation system will move forward a certain distance according to the design requirements and roll construction. Generally in the junction of two observation systems, the same detector The physical location will have different detectors at different construction times. As shown in Figure 7, the above figure is a single-chip observation system. The following figure is the observation system after rolling. There are two bundles, three bundles each, each marked with numbers 1 to 6. The numerical serial number also indicates the sequence of rolling construction. . In the overlap of the 1, 2 single piece and the 5, 6 single piece in Fig. 7, the detector is placed at least twice in the same detector position, that is, at least two different postures. In actual construction, there are often more than two attitudes of detector placement for various reasons. For example, in a three-component seismic exploration project in the application of the present invention, there are a total of 7261 geophysical point positions in the whole area, and the actual common attitude gather is 36,342, and the average physical point of each detector is about 5 postures, at most One detector position has 21 positions. Therefore, at the same detector position, since the detectors disposed at different times are different, the sensitivity of the detector and the degree of coupling of the detector to the earth are also different. Even if the same detector is accidentally placed at the same detector physical point position at different times, the sensitivity is the same, but the degree of coupling with the ground is different due to different layout conditions.
下面将从模型模拟记录中对比分析共姿态道集的地表一致性振幅补偿效果差异。其中,对比分析方法中都采用了本发明提出的三分量地表一致性振幅补偿方法,即按照公式(2)将三个分量的总能量当成一个单分量进行振幅补偿因子分析,所对比分析的是采用目前的共检波点道集方法还是采用本发明中的共姿态道集方法进行振幅补偿因子计算。The difference in surface consistency amplitude compensation effect of the common attitude gathers will be compared and analyzed from the model simulation records. Among them, the comparative analysis method adopts the three-component surface consistency amplitude compensation method proposed by the present invention, that is, according to formula (2), the total energy of the three components is regarded as a single component for amplitude compensation factor analysis, and the comparative analysis is The current co-detection wave point gather method is also used to calculate the amplitude compensation factor using the common attitude gather method in the present invention.
如图1所示,在本发明实施例所提供的观测系统示意图中,假设两条点线之间的检波器共有4中姿态,每种姿态分别接收25炮的记录,两条点线之外的检波器只有一种姿态。在模型模拟中,直接模拟随机产生不同姿态下的检波器振幅因子。采用本发明的三分量地表一致性振幅补偿计算补偿因子。图8~图10等三幅图中,依次展示的是Z、X和Y分量分析结果。每一幅图中从上到下依次为原始振幅、现有技术补偿之后的振幅、本发明提出的共姿态道集分析方法补偿之后的振幅。从图8~图10中均可以看到,目前的共检波点道集分析方法没有解决好振幅补偿问题,而本发明的共姿态道集新方法都较好地实施振幅补偿。目前的共检波点道集分析方法中,Z分量的原始相对差异最大不到10倍,而补偿之后反而超过了10倍;X分量的原始相对差异大约在-12~8倍,而补偿之后变成-15~9倍;Y分量的原始相对差异大约在-12~10倍,而补偿之后变成-25~11倍。同时,补偿之后的相对差异分布与原始相对差异分布并不是正相关关系。As shown in FIG. 1 , in the schematic diagram of the observation system provided by the embodiment of the present invention, it is assumed that the detectors between the two dotted lines have a total of four postures, and each posture receives a record of 25 shots, respectively, outside the two dotted lines. The detector has only one gesture. In the model simulation, the direct simulation randomly generates the detector amplitude factor in different poses. The compensation factor is calculated using the three-component surface consistency amplitude compensation of the present invention. In the three figures of Fig. 8 to Fig. 10, the Z, X and Y component analysis results are sequentially displayed. From top to bottom in each figure are the original amplitude, the amplitude after the prior art compensation, and the amplitude after compensation by the common attitude gather analysis method proposed by the present invention. It can be seen from FIG. 8 to FIG. 10 that the current common detection point gather analysis method does not solve the amplitude compensation problem, and the new method of the common attitude gather set of the present invention performs the amplitude compensation well. In the current common detection wave point gather analysis method, the original relative difference of the Z component is less than 10 times, and the compensation is more than 10 times; the original relative difference of the X component is about -12 to 8 times, and the compensation is changed. It is -15 to 9 times; the original relative difference of the Y component is about -12 to 10 times, and after compensation, it becomes -25 to 11 times. At the same time, the relative difference distribution after compensation is not positively correlated with the original relative difference distribution.
第三,在振幅补偿过程中,除了做地表一致性振幅补偿外,还对非地表一致性振幅差异进行补偿。Third, in the amplitude compensation process, in addition to the surface consistency amplitude compensation, the non-surface consistency amplitude difference is compensated.
虽然在本发明的方法提出了共姿态道集地表一致性振幅补偿技术,能够解决好地表一致性振幅异常问题。但是,在野外实际施工中还会存在由于各种环境噪声所造成的振幅差异,这些异常振幅不属于地下地质异常体的地震响应,而是属于地表上非地表一致性差异。采用地表一致性方法和技术难以解决该振幅异常的校正。 Although the method of the present invention proposes a common attitude gather surface uniformity amplitude compensation technique, it can solve the problem of good surface uniformity amplitude anomaly. However, in the actual construction in the field, there will be amplitude differences caused by various environmental noises. These abnormal amplitudes are not the seismic response of the underground geological anomaly, but belong to the non-surface consistency difference on the surface. Correction of this amplitude anomaly is difficult to solve using surface consistency methods and techniques.
在本发明中设计了非地表一致性振幅补偿分析和校正方法。先统计全区所有地震道的平均能量和能量均方差,将能量位于3倍均方差区域外的地震道作为异常道从全区地震数据体中剔除去,余下的地震数据构成具有代表性的数据体。在具有代表性的数据体中重新统计其平均能量和能量均方差。该平均能量即是全区地表一致性振幅补偿后的期望。对于被剔除去地震道将按照补偿校正的期望进行校正,即进行非地表一致性振幅补偿。最终全区所有地震道的振幅能量都将补偿校正到期望的振幅能量水平。与地表一致性振幅补偿一样,非地表一致性振幅补偿仍按照三分量地表一致性振幅补偿的工作原理和方法进行,保持三分量之间能量的固有关系。Non-surface consistency amplitude compensation analysis and correction methods are designed in the present invention. Firstly, the average energy and energy mean squares of all the seismic traces in the whole area are counted, and the seismic traces whose energy is located outside the 3 times mean square error are removed from the seismic data of the whole area as the abnormal track. The remaining seismic data constitutes representative data. body. The average energy and energy mean squared are re-stated in a representative data volume. This average energy is the expectation after the regional uniformity amplitude compensation. For the rejected track, the correction will be corrected according to the expectation of the compensation correction, that is, the non-surface consistency amplitude compensation is performed. Eventually, the amplitude energy of all the seismic traces in the region will be compensated to the desired amplitude energy level. Like surface consistency amplitude compensation, non-surface consistency amplitude compensation is still performed according to the working principle and method of three-component surface consistency amplitude compensation, maintaining the inherent relationship of energy between the three components.
在本发明提供方法中,由于提出共姿态道集地表一致性振幅补偿方法,在共检波点道集中划分出检波器的不同姿态并且不同的共姿态道集分开实施检波器补偿因子分析,同时将三分量地震数据的总能量当成一个单分量实施地表一致性振幅补偿,保证了三个分量之间正确的能量关系,也对非地表一致性振幅异常进行了校正,因此与现有技术相比,具有能够准确补偿因地表一致性因素所造成的振幅差异,同时保证了各个分量之间正确的能量关系的优点:In the method provided by the present invention, since the co-attack gathers the ground surface uniform amplitude compensation method, the different postures of the detector are divided in the common detection wave track, and the different common attitude gathers are separately implemented to perform the detector compensation factor analysis, and at the same time The total energy of the three-component seismic data is used as a single-component implementation of surface uniform amplitude compensation, which ensures the correct energy relationship between the three components, and also corrects the non-surface consistency amplitude anomaly, so compared with the prior art, It has the advantage of being able to accurately compensate for amplitude differences caused by surface consistency factors while ensuring the correct energy relationship between the components:
其一:能够获得满足地表一致性原理和要求的高保真地震数据。由于采用了共姿态道集分析方法,纠正了现有技术中基于共检波点道集分析的理论假设错误,正确实施地表一致性振幅补偿,保障后期的数据处理和反演解释。First, high-fidelity seismic data that meets the principles and requirements of surface consistency can be obtained. Because the common attitude gather analysis method is adopted, the theoretical hypothesis error based on the common detection wave point gather analysis in the prior art is corrected, and the surface consistency amplitude compensation is correctly implemented to ensure the later data processing and inversion interpretation.
其二:在准确补偿地表一致性振幅差异的同时,确保纵、横波之间以及横波各分量之间的能量分配的正确关系保持一致。经过本发明方法中三分量地表一致性振幅补偿处理之后,因为是将各个分量的能量总和作为一个单分量进行分析,所以各个分量之间的能量关系并不会改变,保持了其本来的振幅相对关系,为全波形反演、亮点技术、横波分裂探测裂隙等技术的高保真、高精度、高分辨率开展和推广应用提供高质量的数据保障。Secondly, while accurately compensating for the difference in amplitude of the surface consistency, it is ensured that the correct relationship of energy distribution between the longitudinal and transverse waves and between the components of the transverse wave is consistent. After the three-component surface consistency amplitude compensation process in the method of the present invention, since the sum of the energy of each component is analyzed as a single component, the energy relationship between the components does not change, maintaining its original amplitude relative to The relationship provides high-quality data protection for high-fidelity, high-precision, high-resolution development and promotion of full waveform inversion, bright spot technology, and shear wave splitting detection cracks.
图11示出了本发明实施例所提供的一种共姿态道集地表一致性振幅补偿方法的流程图。该方法包括两项关键技术:一是检波器项地表一致性振幅补偿因子分析以及振幅补偿都在共姿态道集中进行。二是三分量地震勘探中,将三个分量的能量总和当成一个单一分量进行地表一致性振幅补偿分析,校正的时候各道的三个分量的校正因子相同。具体过程如下:FIG. 11 is a flow chart showing a method for compensating amplitude consistency of a common attitude track set surface according to an embodiment of the present invention. The method includes two key technologies: one is that the geophone's surface consistency amplitude compensation factor analysis and the amplitude compensation are all performed in the common attitude track set. Second, in three-component seismic exploration, the sum of the energy of the three components is treated as a single component for surface consistency amplitude compensation analysis. When correcting, the correction factors of the three components of each channel are the same. The specific process is as follows:
101、获取勘探工区中的地震数据及该地震数据对应的施工班报。101. Obtain seismic data in the exploration work area and a construction work report corresponding to the seismic data.
102、计算地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量。102. Calculate an average total energy of all components of each seismic data in the seismic data to obtain seismic energy of the track.
103、对各个地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体。 103. Perform a preliminary test of surface consistency for each seismic energy, and determine all seismic energy of the first predetermined condition as a representative data volume.
本实施例中,将检验结果符合第一预设条件的所有地震道能量确定为具有代表性的数据体,并且将符合第二预设条件的所有地震道能量确定为疑似非代表性的数据体。In this embodiment, all the seismic energy of the test result conforming to the first preset condition is determined as a representative data body, and all the seismic energy of the second preset condition is determined as a suspected non-representative data body. .
本实施例中,第一预设条件和第二预设条件可以为同一条件的两种不同的方式,也可以为两个不同的条件。本实施例中,第一预设条件和第二预设条件为前者,具体为:符合3倍均方差的原则的为第一预设条件,不符合3倍均方差的原则的为第二条件。In this embodiment, the first preset condition and the second preset condition may be two different manners of the same condition, or may be two different conditions. In this embodiment, the first preset condition and the second preset condition are the former, specifically: the first preset condition that satisfies the principle of 3 times mean square error, and the second condition that does not meet the principle of 3 times mean square error .
104、在具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,各项补偿因子至少包括震源项补偿因子。104. Calculate each compensation factor corresponding to each track energy in a representative data body, and each compensation factor includes at least a source term compensation factor.
105、根据检波器的不同姿态,在勘探工区的地震数据中抽取的共检波点道集中抽取共姿态道集,并在共姿态道集中计算检波器项补偿因子。105. According to the different postures of the detector, the common detection track gathers are extracted from the common detection wave points extracted from the seismic data of the exploration work area, and the detector item compensation factor is calculated in the common attitude track.
106、根据各项补偿因子以及检波器项补偿因子构成的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿。106. Perform surface consistency amplitude compensation on the seismic data of the entire work area according to the total compensation factors formed by the compensation factors and the detector item compensation factors.
下面具体介绍一下本发明的具体实现方案:The specific implementation of the present invention will be specifically described below:
步骤201:对地震勘探中原始数据(即勘探工区中的地震数据)建立观测系统,并对该原始数据进行道编辑,剔除噪声污染严重的地震道。Step 201: Establish an observation system for the original data in the seismic exploration (ie, the seismic data in the exploration work area), and edit the original data to eliminate the seismic road with serious noise pollution.
步骤202:选取适当的时窗,在时窗内计算各道地震数据所有分量的平均总能量,并作为各地震道的能量。计算公式为Step 202: Select an appropriate time window, calculate the average total energy of all components of each seismic data in the time window, and use the energy of each seismic trace. The calculation formula is
Figure PCTCN2015074246-appb-000009
Figure PCTCN2015074246-appb-000009
式中T为时窗长度,N为地震数据的分量个数,如果是单分量,例如纵波地震勘探,N等于1,如果是三分量地震勘探,则N等于3。Cn,t为第n分量在时窗内第t采样点的振幅值。Where T is the length of the time window, N is the number of components of the seismic data, if it is a single component, such as longitudinal wave seismic exploration, N is equal to 1, and if it is a three-component seismic exploration, N is equal to 3. C n,t is the amplitude value of the t-th sample point of the nth component in the time window.
步骤203:计算全区所有地震道能量的平均值Avg和均方差Std,按照3倍均方差的原则对各个地震道能量进行地表一致性初步检验,并根据检验结果剔除异常地震道(即疑似非地表一致性的数据体),地表一致性振幅补偿在余下的地震道集(即具有代表性的数据体)中进行,而在被剔除出去的地震道集中进行非地表一致性振幅校正。另外,在具有代表性的数据体中计算平均能量,作为全区振幅校正的期望值Expect。具体计算公式为:Step 203: Calculate the average value Avg and the mean square error Std of all the seismic energy of the whole area, perform a preliminary test of the surface consistency of each seismic energy according to the principle of 3 times mean square error, and remove the abnormal seismic track according to the test result (ie, suspected non- The data consistency of the surface consistency), the surface consistency amplitude compensation is performed in the remaining seismic gathers (ie, the representative data volume), and the non-surface consistency amplitude correction is performed on the excluded seismic traces. In addition, the average energy is calculated in a representative data volume as the expected value of the full-area amplitude correction. The specific calculation formula is:
Figure PCTCN2015074246-appb-000010
Figure PCTCN2015074246-appb-000010
式中M是全区的地震道总数,K是具有代表性的数据体的地震道的总数。Where M is the total number of seismic traces in the whole zone, and K is the total number of seismic traces of representative data volumes.
步骤204:在具有代表性的数据体中计算各道的总补偿因子期望值,具体计算公式为:Step 204: Calculate the total compensation factor expectation value of each track in a representative data body, and the specific calculation formula is:
Scalem=Expect/Engm    (5)Scale m =Expect/Eng m (5)
步骤205:在具有代表性的数据体中抽取共炮点道集,并统计分析各个震源的补偿因子。Step 205: Extract a common shot point gather in a representative data body, and statistically analyze the compensation factors of each source.
Figure PCTCN2015074246-appb-000011
Figure PCTCN2015074246-appb-000011
式中,Scales是与第S炮相关的地震道的补偿因子期望值,Ns是该共炮点道集的覆盖次数。Where Scale s is the compensation factor expectation value of the seismic trace associated with the S-th shot, and N s is the number of coverage times of the common shot gather.
步骤206:在具有代表性的数据体中抽取共炮检距道集,并统计分析各个炮检距段的补偿因子。Step 206: Extract a common offset track gather in a representative data body, and statistically analyze the compensation factors of each offset segment.
Figure PCTCN2015074246-appb-000012
Figure PCTCN2015074246-appb-000012
式中,Scaleo是与第O炮检距段相关的地震道的补偿因子期望值,No是该共炮检距道集的覆盖次数。Where Scale o is the expected value of the compensation factor for the seismic trace associated with the 0th offset section, and N o is the number of coverages of the total offset set.
步骤207:在具有代表性的数据体中抽取相同构造项道集,并统计分析各个构造项对应的补偿因子。Step 207: Extract the same structural item gathers in the representative data body, and statistically analyze the compensation factors corresponding to the respective structural items.
Figure PCTCN2015074246-appb-000013
Figure PCTCN2015074246-appb-000013
式中,Scalec是与第C构造项相关的地震道的补偿因子期望值,Nc是该构造项道集的覆盖次数。Where Scale c is the compensation factor expectation value of the seismic trace associated with the Cth construction term, and N c is the number of coverage times of the construction item gather.
其中,构造项道集的抽取基本上与目前的方法相同。如果是纵波地震数据处理,则共中心点(即CMP,或CDP)道集即为构造项道集;如果是转换横波地震数据处理,则一般采用共渐近转换点道集作为构造项道集。如果所处理的是三分量地震数据,需要根据步骤202中所选取的时窗来确定,如果时窗范围内的主要能量是纵波能量,则以共中心道集为构造项道集;如果主要能量是转换横波能量,则以共渐近转换点道集为构造项道集。Among them, the extraction of the construction item gather is basically the same as the current method. In the case of longitudinal wave seismic data processing, the common center point (ie CMP, or CDP) gather is the structural item gather; if it is the converted shear wave seismic data processing, the common asymptotic transition point gather is generally used as the structural item gather . If the three-component seismic data is processed, it needs to be determined according to the time window selected in step 202. If the main energy in the time window range is the longitudinal wave energy, the common center gather is used as the structural item gather; if the main energy When the shear wave energy is converted, the common asymptotic conversion point gather is used as a structural item gather.
步骤208:在共检波点道集中抽取共姿态道集,在各个共姿态道集中进行统计分析,从而得到各个共姿态道集对应的检波器补偿因子。Step 208: Extract a common attitude gather in the common detection track gather, perform statistical analysis on each common attitude gather, and obtain a detector compensation factor corresponding to each common attitude gather.
具体方法为:(1)在三分量地震勘探中,可以从地震数据道头上读取各个分量的倾角值,并将各个倾角值或者是它们的组合值作为姿态标识码。如果在共检波点道集中,不同的检波器布设时间上有两个以上的姿态标识码相同,可以在其基础上增加布设时间并一起组合成为新的姿态标识码。(2)对于单分量地震勘探,可以从野外施工记录班报中对同一检波器物理 点位置上检波器布设时间的先后顺序进行划分,将布设时间作为姿态的标识码。最后,在共检波点道集中按照不同的姿态标识码抽取不同的共姿态道集。The specific method is as follows: (1) In the three-component seismic exploration, the inclination value of each component can be read from the seismic data track head, and each inclination value or a combination thereof is used as the attitude identification code. If there are more than two attitude identification codes in different detector placement times in the common detector locus, it is possible to add the layout time and combine them together to form a new gesture identification code. (2) For single-component seismic exploration, the same detector physics can be recorded from the field construction record At the point position, the order of the detectors is set in the order of the time, and the layout time is used as the identification code of the gesture. Finally, different common attitude gathers are extracted according to different pose identification codes in the common checkpoint track set.
共姿态道集的补偿因子计算公式为:The compensation factor for the common attitude gather is calculated as:
Figure PCTCN2015074246-appb-000014
Figure PCTCN2015074246-appb-000014
式中,Scaleα是与第A共姿态道集相关的补偿因子期望值,Nα是该共姿态道集的覆盖次数。Where Scale α is the compensation factor expectation associated with the A-co-coordinate set of gathers, and N α is the number of coverages of the common pose gather.
步骤209:将各道地震数据的总补偿因子分解为炮点补偿因子Sm,s、检波点补偿因子Am,α、炮检距补偿因子Om,o和构造项补偿因子Cm,c等,并根据公式(10)计算各地震道数据的总补偿因子。Step 209: Decompose the total compensation factor of each seismic data into a shot compensation factor S m, s , a detection point compensation factor A m, α , a offset compensation factor O m, o, and a structural item compensation factor C m, c Etc., and calculate the total compensation factor for each seismic trace data according to formula (10).
log(Scalem,s,α,o,c)=log(Sm,s)+log(Am,α)+log(Om,o)+log(Cm,c)    (10)Log(Scale m,s,α,o,c )=log(S m,s )+log(A m,α )+log(O m,o )+log(C m,c ) (10)
步骤210:按照经典的高斯—赛德尔迭代方法进行迭代计算,从而获得最终的各项补偿因子。Step 210: Perform an iterative calculation according to the classical Gauss-Seidel iterative method to obtain the final compensation factors.
Figure PCTCN2015074246-appb-000015
Figure PCTCN2015074246-appb-000015
式中,各等式左端计算所得分别为第K次迭代中的炮点、检波点、炮检距和构造项等的补偿因子。一般经过3次迭代后,可以得到合适的补偿因子。In the formula, the left end of each equation is calculated as the compensation factor of the shot point, the detection point, the offset, and the structural item in the Kth iteration. After 3 iterations, a suitable compensation factor can be obtained.
步骤211:将步骤210中获得的补偿因子对具有代表性的数据体中的各道地震数据进行地表一致性补偿。本发明建议应用的时候只应用炮点和检波点两项补偿因子,不宜全部因子都应用。因为构造项对应的是地下地质异常体的响应,炮检距项对应的是振幅随炮检距(即AVO)的变化规律,这也是与地下地质体相关的响应,非地表一致性问题。Step 211: Perform the surface consistency compensation for each seismic data in the representative data volume by using the compensation factor obtained in step 210. When the invention proposes to apply, only two compensation factors of the shot point and the detection point are applied, and not all factors are applicable. Because the structural term corresponds to the response of the subsurface geological anomaly, the offset term corresponds to the variation of the amplitude with the offset (ie AVO), which is also the response related to the underground geological body, and the non-surface consistency problem.
步骤212:对步骤211中经过补偿之后的地震数据,按照步骤202和203的方法,计算补偿后振幅能量的平均值和均方差。Step 212: Calculate the average value and the mean square error of the compensated amplitude energy according to the methods of steps 202 and 203 for the compensated seismic data in step 211.
步骤213:实施非地表一致性振幅检验和校正。Step 213: Perform non-surface consistency amplitude verification and correction.
在步骤203中剔除来的疑似非地表一致性数据体中,如果其对应的炮点和检波点在步骤210的计算中均能找到对应的补偿因子,就对该地震道数据进行振幅补偿。同时,按照步骤212中的平均值和均方差检验补偿后的振幅能量,如果属于3倍均方差的范围,则认为该道地震数据振幅差异属于地表 一致性问题,并接受地表一致性补偿。如果超过3倍均方差范围,则认为该道地震数据振幅差异属于非地表一致性问题,拒绝接受地表一致性补偿,同时将其地震数据能量校正为全区地震数据振幅校正的期望值Expect。In the suspected non-surface consistent data body extracted in step 203, if the corresponding shot point and the detection point can find the corresponding compensation factor in the calculation of step 210, the seismic channel data is amplitude compensated. At the same time, the compensated amplitude energy is tested according to the average value and the mean square error in step 212. If it belongs to the range of 3 times mean square error, the amplitude difference of the seismic data is considered to belong to the surface. Consistency issues and acceptance of surface consistency compensation. If the range of the mean square error is more than 3 times, the amplitude difference of the seismic data is considered to be a non-surface consistency problem, and the ground surface consistency compensation is rejected, and the seismic data energy is corrected to the expected value of the earthquake data amplitude correction of the whole region.
如果某地震道在步骤210的计算中不能同时找到对应的炮点和检波点补偿因子,则认为该道数据振幅差异属于非地表一致性问题,将其地震数据能量校正为全区地震数据振幅校正的期望值Expect。If a seismic trace cannot find the corresponding shot point and the detection point compensation factor in the calculation of step 210, it is considered that the data amplitude difference of the track belongs to the non-surface consistency problem, and the seismic data energy is corrected to the whole area seismic data amplitude correction. The expected value of Expect.
至此,对全区地震数据进行了地表一致性振幅补偿,同时也对极少数不满足地表一致性振幅检验的地震道进行了非地表一致性振幅校正。最后,经过本发明的处理后,全区地震数据都能得到高保真的振幅补偿,消除了地表一致性振幅异常,同时在三分量地震勘探中保留了三个分量之间固有的能量比例关系,为后续的数据处理和解释反演提供了高质量的基础数据。At this point, the surface consistency amplitude compensation was performed on the seismic data of the whole region, and the non-surface consistency amplitude correction was also performed on a few seismic traces that did not satisfy the surface consistency amplitude test. Finally, after the treatment of the present invention, the seismic data of the whole region can obtain high-fidelity amplitude compensation, eliminating the surface amplitude anomaly, and retaining the inherent energy proportional relationship between the three components in the three-component seismic exploration. Provides high quality basic data for subsequent data processing and interpretation inversion.
本发明实施例还提供了一种共姿态道集地表一致性振幅补偿装置,如图12所示,包括:The embodiment of the present invention further provides a co-attack gather surface consistency amplitude compensation device, as shown in FIG. 12, including:
获取单元11,用于获取勘探工区中的地震数据及其对应的施工班报。The obtaining unit 11 is configured to acquire seismic data in the exploration work area and the corresponding construction work report.
第一计算单元12,用于计算获取单元11获取的地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量。The first calculating unit 12 is configured to calculate an average total energy of all components of each seismic data in the seismic data acquired by the acquiring unit 11 to obtain the seismic channel energy of the track.
具体的,第一计算单元12具体用于,根据公式
Figure PCTCN2015074246-appb-000016
计算每一道数据的所有分量的平均总能量,得到每一道的地震道能量。
Specifically, the first calculating unit 12 is specifically used according to the formula
Figure PCTCN2015074246-appb-000016
Calculate the average total energy of all components of each channel of data to obtain the seismic energy of each channel.
检验单元13,用于对经过第一计算单元12计算得到的每一道地震道能量进行地表一致性初步检验。The checking unit 13 is configured to perform a preliminary test of the surface consistency of each track energy calculated by the first calculating unit 12.
具体的,检验单元13包括:第一计算子单元,用于根据公式
Figure PCTCN2015074246-appb-000017
计算勘探工区中所有地震道能量的平均值和均方差,得到工区的平均值和均方差;其中,公式中M是整个工区的地震道总数。
Specifically, the checking unit 13 includes: a first calculating subunit for using a formula according to the formula
Figure PCTCN2015074246-appb-000017
Calculate the mean and mean square error of all seismic energy in the exploration area, and obtain the average and mean square error of the work area; where M is the total number of seismic traces in the entire work area.
第一确定单元14,用于将检验单元13的检验结果符合第一预设条件的所有地震道能量确定为具有代表性的数据体。The first determining unit 14 is configured to determine all the seismic energy of the inspection result of the verification unit 13 according to the first preset condition as a representative data volume.
具体的,第一确定单元14包括第一统计子单元和第一确定子单元,第一统计子单元用于统计与工区的平均值之差处于3倍工区均方差区域内的地震道能量;第一确定子单元,用于将第一统计子单元统计的地震道能量确定为具有代表性的数据体。Specifically, the first determining unit 14 includes a first statistical subunit and a first determining subunit, where the first statistical subunit is configured to calculate the seismic energy of the difference between the average value of the work area and the mean square error area of the work area; A determining subunit is configured to determine the seismic channel energy of the first statistical subunit as a representative data volume.
第二计算单元15,用于在第一确定单元14确定的具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,各项补偿因子至少包括震源项补偿因子。The second calculating unit 15 is configured to calculate each compensation factor corresponding to each track energy in the representative data body determined by the first determining unit 14, and each compensation factor includes at least a source term compensation factor.
抽取单元16,用于根据检波器的不同姿态,在勘探工区的共检波点道集中抽取共姿态道集。 The extracting unit 16 is configured to extract a common attitude gather in the common detection wave point gather of the exploration work area according to different postures of the detector.
第三计算单元17,用于在抽取单元16抽取的共姿态道集中计算检波器项补偿因子。The third calculating unit 17 is configured to calculate a detector term compensation factor in the common attitude track set extracted by the extracting unit 16.
具体的,第三计算单元具体用于,根据公式
Figure PCTCN2015074246-appb-000018
在共姿态道集中计算检波器项补偿因子;其中,Scaleα是与第A共姿态道集相关的补偿因子期望值,Nα是该共姿态道集中包括的所有地震数据的道数。
Specifically, the third calculating unit is specifically used according to the formula
Figure PCTCN2015074246-appb-000018
The detector term compensation factor is calculated in the co-statue track set; wherein Scale α is the compensation factor expectation value associated with the A-co-coordinate track set, and N α is the number of tracks of all seismic data included in the co-statue track set.
地表一致性振幅补偿单元18,用于根据第二计算单元15计算得到的各项补偿因子以及第三计算单元17计算得到的检波器项补偿因子构成的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿。The surface consistency amplitude compensation unit 18 is configured to perform seismic compensation data for the entire work area according to the total compensation factors formed by the compensation factors calculated by the second calculation unit 15 and the detector term compensation factors calculated by the third calculation unit 17 Surface consistency amplitude compensation.
具体的,地表一致性振幅补偿单元18包括第二计算子单元和地表一致性振幅补偿子单元;Specifically, the surface consistency amplitude compensation unit 18 includes a second calculation subunit and a surface consistency amplitude compensation subunit;
第二计算子单元,用于根据公式log(Scalem,s,α,o,c)=log(Sm,s)+log(Am,α)+log(Om,o)+log(Cm,c),计算各地震道数据的总补偿因子。a second calculation subunit for calculating according to the formula log(Scale m, s, α, o, c )=log(S m,s )+log(A m,α )+log(O m,o )+log( C m,c ), calculate the total compensation factor for each seismic trace data.
地表一致性振幅补偿子单元,用于根据第二计算子单元计算的总补偿因子,对整个工区的地震数据进行地表一致性振幅补偿。The surface consistency amplitude compensation sub-unit is configured to perform surface consistency amplitude compensation on the seismic data of the entire work area according to the total compensation factor calculated by the second calculation sub-unit.
其中,地表一致性振幅补偿单元18还用于,对疑似非地表一致性数据体进行地表一致性振幅补偿。The surface consistency amplitude compensation unit 18 is further configured to perform surface consistency amplitude compensation on the suspected non-surface consistent data volume.
进一步的,该装置还包括第二确定单元,用于将符合第二预设条件的所有地震道能量作为疑似非地表一致性数据体。Further, the apparatus further includes a second determining unit configured to use all of the seismic energy of the second predetermined condition as the suspected non-surface consistent data volume.
具体的,第二确定单元包括第二统计子单元和第二确定子单元;第二统计子单元,用于统计与工区的平均值之差处于3倍工区的均方差区域外的地震道能量;第二确定子单元,用于将统计得到的地震道能量确定为疑似非地表一致性数据体。Specifically, the second determining unit includes a second statistic subunit and a second deterministic subunit, and the second statistic subunit is configured to count the difference between the average value of the work area and the seismic trace energy outside the mean square error region of the work area; The second determining subunit is configured to determine the statistically obtained seismic trace energy as a suspected non-surface consistent data volume.
进一步的,该装置还包括第三确定单元,用于将共检波点道集中检波器不同布设时间内的地震道能量确定为对应的共姿态道集。Further, the apparatus further includes a third determining unit configured to determine the seismic channel energy of the common detection point concentrator detector in different deployment times as the corresponding common attitude gather.
具体的,第三确定单元具体用于,根据地震采集系统测量的三分量各自倾角的大小以及施工班报记录,在共检波点道集中抽取检波器不同布设时间内的地震道能量,并确定为对应的共姿态道集。Specifically, the third determining unit is specifically configured to: according to the size of the respective dip angles of the three components measured by the seismic acquisition system and the construction class report, extract the seismic energy of the detectors in different sets of time in the common detection wave track, and determine Corresponding common attitude gathers.
进一步,该装置还包括第四计算单元,用于根据高斯—赛德尔迭代方法,计算各项补偿因子和检波器项补偿因子;Further, the apparatus further includes a fourth calculating unit, configured to calculate each compensation factor and the detector term compensation factor according to the Gauss-Seidel iterative method;
进一步,该装置还包括:Further, the device further includes:
第五计算单元,用于计算补偿后的疑似非地表一致性数据体的地震道能量。A fifth calculating unit is configured to calculate the seismic energy of the compensated suspected non-surface consistent data volume.
第六计算单元,用于计算地表一致性振幅补偿后的具有代表性的数据体的所有地震道能量的平均值和均方差。The sixth calculating unit is configured to calculate an average value and a mean square error of all the seismic energy of the representative data volume after the surface consistency amplitude compensation.
验证单元,用于根据第六计算单元计算得到的平均值和均方差对疑似非地表一致性数据体的地震道能量进行验证,得到验证结果。 The verification unit is configured to verify the seismic energy of the suspected non-surface consistent data volume according to the average value and the mean square error calculated by the sixth calculating unit, and obtain the verification result.
保留单元,用于当确定验证单元的验证结果符合第一预设条件时,保留经过地表一致性振幅补偿的疑似非地表一致性数据体。And a retaining unit, configured to retain the suspected non-surface consistent data volume that passes through the surface consistency amplitude compensation when determining that the verification result of the verification unit meets the first preset condition.
非地表一致性振幅补偿单元,用于在确定验证结果符合第二预设条件时,对疑似非地表一致性数据体进行非地表一致性振幅补偿。The non-surface consistency amplitude compensation unit is configured to perform non-surface consistency amplitude compensation on the suspected non-surface consistent data volume when determining that the verification result meets the second preset condition.
剔除单元,用于在确定验证单元的验证结果符合第二预设条件时,对疑似非地表一致性数据体进行剔除。The culling unit is configured to cull the suspected non-surface consistent data body when determining that the verification result of the verification unit meets the second preset condition.
进一步的,非地表一致性振幅补偿单元包括:Further, the non-surface consistency amplitude compensation unit comprises:
第三计算子单元,按照公式
Figure PCTCN2015074246-appb-000019
计算整个工区的具有代表性的数据体对应地震数据经过地表一致性振幅补偿之后的期望值,其中,公式中K是具有代表性的数据体中地震道的总数;
The third calculation subunit, according to the formula
Figure PCTCN2015074246-appb-000019
Calculating the expected value of the representative data volume of the entire work area corresponding to the seismic data after the seismic data is compensated by the surface consistency amplitude, where K is the total number of seismic traces in the representative data volume;
第四计算子单元,用于按照公式Scalem=Expect/Engm,计算其对应的非地表一致性补偿因子作为最终的补偿因子;a fourth calculating subunit, configured to calculate a corresponding non-surface consistency compensation factor as a final compensation factor according to the formula Scale m = Expect/Eng m ;
非地表一致性振幅补偿子单元,根据第四计算子单元计算得到的最终的补偿因子,对疑似非地表一致性数据体进行非地表一致性振幅补偿。The non-surface consistency amplitude compensation sub-unit performs non-surface consistency amplitude compensation on the suspected non-surface consistent data volume according to the final compensation factor calculated by the fourth calculation sub-unit.
本发明提供的共姿态道集地表一致性振幅补偿装置,在振幅补偿过程中,除了做地表一致性振幅补偿外,还对检验不合格的地震道进行非地表一致性振幅差异进行校正,使得对地震道数据的校正和补偿结果更加准确。The common attitude road set surface consistency amplitude compensation device provided by the invention, in addition to the surface consistency amplitude compensation in the amplitude compensation process, corrects the non-surface consistency amplitude difference of the unqualified seismic track, so that The correction and compensation results of the seismic trace data are more accurate.
以上,仅为本发明的具体实施方式,但本发明的保护范围并不局限于此,任何熟悉本技术领域的技术人员在本发明揭露的技术范围内,可轻易想到变化或替换,都应涵盖在本发明的保护范围之内。因此,本发明的保护范围应以权利要求的保护范围为准。 The above is only the specific embodiment of the present invention, but the scope of the present invention is not limited thereto, and any person skilled in the art can easily think of changes or substitutions within the technical scope of the present invention. It is within the scope of the invention. Therefore, the scope of protection of the present invention should be determined by the scope of the claims.

Claims (10)

  1. 一种共姿态道集地表一致性振幅补偿方法,其特征在于,包括:A common attitude gather set surface consistency amplitude compensation method, which is characterized in that:
    获取勘探工区中的地震数据及该地震数据对应的施工班报;Obtaining seismic data in the exploration work area and the construction work report corresponding to the seismic data;
    计算所述地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量;Calculating an average total energy of all components of each seismic data in the seismic data to obtain seismic trace energy of the track;
    对各个所述地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体;Performing a preliminary test of surface consistency for each of the seismic energy, and determining all seismic energy of the first predetermined condition as a representative data volume;
    在所述具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,所述各项补偿因子至少包括震源项补偿因子;Calculating, in the representative data body, each compensation factor corresponding to each track energy, the compensation factors including at least a source term compensation factor;
    根据检波器的预设姿态,在所述勘探工区的地震数据的共检波点道集中抽取共姿态道集,并在所述共姿态道集中计算检波器项补偿因子;And extracting a common attitude gather from the common detection track points of the seismic data of the exploration area according to a preset posture of the detector, and calculating a detector item compensation factor in the common attitude track set;
    根据所述各项补偿因子以及所述检波器项补偿因子构成的总补偿因子,对所述整个工区的地震数据进行地表一致性振幅补偿。And performing surface consistency amplitude compensation on the seismic data of the entire work area according to the compensation factors and the total compensation factor formed by the detector term compensation factor.
  2. 根据权利要求1所述的方法,其特征在于,所述地震数据包括单分量地震数据和三分量地震数据;The method of claim 1 wherein said seismic data comprises single component seismic data and three component seismic data;
    计算所述地震数据中每一道地震数据的所有分量的平均总能量包括:Calculating the average total energy of all components of each seismic data in the seismic data includes:
    根据公式
    Figure PCTCN2015074246-appb-100001
    计算所述地震道数据中每一道数据的所有分量的平均总能量,得到每一道的地震道能量;
    According to the formula
    Figure PCTCN2015074246-appb-100001
    Calculating an average total energy of all components of each of the data in the seismic trace data to obtain seismic trace energy for each track;
    公式中T为时窗长度,N为地震数据的分量个数,Cn,t为第n分量在时窗内第t采样点的振幅值。In the formula, T is the length of the time window, N is the number of components of the seismic data, and C n,t is the amplitude of the t-th sample at the t-th sample in the time window.
  3. 根据权利要求2所述的方法,其特征在于,所述方法还包括:The method of claim 2, wherein the method further comprises:
    对各个所述地震道能量进行地表一致性初步检验,并将符合第二预设条件的所有地震道能量构成疑似非地表一致性数据体;Performing a preliminary check on the surface consistency of each of the seismic energy, and constructing all the seismic energy of the second preset condition to constitute a suspected non-surface consistent data volume;
    对各个所述地震道能量进行地表一致性初步检验,并将符合第一预设条件的所有地震道能量确定为具有代表性的数据体包括:Performing a preliminary test of surface consistency for each of the seismic energy, and determining all seismic energy of the first predetermined condition as a representative data volume includes:
    分别根据公式
    Figure PCTCN2015074246-appb-100002
    计算所述勘探工区中所有地震道能量的平均值和均方差,得到工区的平均值和均方差;其中,公式中M是整个勘探工区的地震道总数;
    According to the formula
    Figure PCTCN2015074246-appb-100002
    Calculating the mean and mean square error of all seismic energy in the exploration area, and obtaining the mean and mean square error of the work area; wherein, in the formula, M is the total number of seismic traces of the entire exploration work area;
    统计与所述工区的平均值之差处于3倍所述工区的均方差区域内的地震道能量,并将该地震道能量作为具有代表性的数据体;The difference between the statistics and the average value of the work area is three times the seismic energy in the mean square error region of the work area, and the seismic energy is taken as a representative data body;
    对各个所述地震道能量进行地表一致性初步检验,并将符合第二预设条件的所有地震道能量构成疑似非地表一致性数据体,包括:A preliminary test of surface consistency is performed on each of the seismic energy, and all seismic energy corresponding to the second predetermined condition constitutes a suspected non-surface consistent data body, including:
    统计与所述工区的平均值之差处于3倍所述工区的均方差区域外的地震道能量,并将该地震道能量作为疑似非地表一致性数据体。 The difference between the statistics and the average value of the work area is three times the seismic energy outside the mean square error region of the work area, and the seismic energy is regarded as a suspected non-surface consistency data body.
  4. 根据权利要求2所述的方法,其特征在于,所述各项补偿因子还包括:炮检距项补偿因子和构造项补偿因子。The method according to claim 2, wherein the compensation factors further comprise: a offset term compensation factor and a construction term compensation factor.
  5. 根据权利要求3或4所述的方法,其特征在于,所述方法还包括:The method according to claim 3 or 4, wherein the method further comprises:
    对于单分量地震数据,在所述共检波点道集中将所述施工班报记录的检波器不同布设时间内的地震道能量,作为对应的共姿态道集;For the single-component seismic data, the seismic energy of the detectors recorded in the construction class report is set to be a corresponding common attitude gather in the common detection track gather;
    对于三分量地震数据,根据地震采集系统测量的三个分量各自倾角的大小以及施工班报记录,在所述共检波点道集中抽取检波器不同布设时间内的地震道能量,构成对应的共姿态道集。For the three-component seismic data, according to the magnitudes of the respective dip angles of the three components measured by the seismic acquisition system and the construction shift report, the seismic trace energy of the detectors in different sets of time is extracted from the common detection point gathers to form a corresponding common attitude. Taoist set.
  6. 根据权利要求5所述的方法,其特征在于,在所述共姿态道集中计算检波器项补偿因子,包括:The method according to claim 5, wherein calculating the detector term compensation factor in the common attitude track set comprises:
    根据公式
    Figure PCTCN2015074246-appb-100003
    在所述共姿态道集中计算检波器项补偿因子;其中,Scaleα是与第A共姿态道集相关的补偿因子期望值,Nα是该共姿态道集中包括的所有地震数据的道数。
    According to the formula
    Figure PCTCN2015074246-appb-100003
    A detector term compensation factor is calculated in the common attitude track set; wherein Scale α is a compensation factor expectation value associated with the A-co-coordinate track set, and N α is a number of tracks of all seismic data included in the common attitude track set.
  7. 根据权利要求6所述的方法,其特征在于,所述方法还包括:根据高斯—赛德尔迭代方法,计算所述各项补偿因子和所述检波器项补偿因子;其中所述高斯—赛德尔迭代方法包括公式:The method according to claim 6, wherein the method further comprises: calculating the compensation factors and the detector term compensation factor according to a Gauss-Seidel iterative method; wherein the Gauss-Seidel The iterative method includes the formula:
    Figure PCTCN2015074246-appb-100004
    Figure PCTCN2015074246-appb-100004
    式中,Ss、Aα、Oo和Cc分别为所述震源项补偿因子、检波器项补偿因子、炮检距项补偿因子和构造项补偿因子,Scalem,s,α,o,c为所述总补偿因子。Where S s , A α , O o and C c are the source term compensation factor, the detector term compensation factor, the offset term compensation factor and the structural term compensation factor, Scale m, s, α, o, respectively. c is the total compensation factor.
  8. 根据权利要求7所述的方法,其特征在于,对所述整个工区的地震数据进行地表一致性振幅补偿,包括:The method of claim 7 wherein the seismic data of the entire work area is subjected to surface consistency amplitude compensation, comprising:
    根据公式log(Scalem,s,α,o,c)=log(Sm,s)+log(Am,α)+log(Om,o)+log(Cm,c),计算各地震道数据的总补偿因子;Calculate each according to the formula log(Scale m, s, α, o, c )=log(S m,s )+log(A m,α )+log(O m,o )+log(C m,c ) Total compensation factor for seismic trace data;
    根据所述总补偿因子,对所述整个工区的地震数据进行地表一致性振幅补偿;Performing surface consistency amplitude compensation on the seismic data of the entire work area according to the total compensation factor;
    所述方法还包括:The method further includes:
    对疑似非地表一致性数据体进行地表一致性振幅补偿,并计算补偿后的所述疑似非地表一致性数据体的地震道能量; Performing surface consistency amplitude compensation on the suspected non-surface consistent data volume, and calculating the seismic trace energy of the compensated suspected non-surface consistent data volume;
    计算地表一致性振幅补偿后的所述具有代表性的数据体的所有地震道能量的平均值和均方差,并根据该平均值和均方差对所述疑似非地表一致性数据体的地震道能量进行验证,得到验证结果;Calculating an average value and a mean square error of all seismic energy of the representative data volume after the surface consistency amplitude compensation, and calculating the seismic energy of the suspected non-surface consistent data volume according to the average value and the mean square error Verify and get the verification result;
    在确定所述验证结果符合第一预设条件时,保留所述疑似非地表一致性数据体中的对应地震道数据并对其进行地表一致性振幅补偿;When it is determined that the verification result meets the first preset condition, retaining corresponding seismic trace data in the suspected non-surface consistent data volume and performing surface consistency amplitude compensation thereon;
    在确定所述验证结果符合第二预设条件时,剔除所述疑似非地表一致性数据体中对应地震道数据或者对其进行非地表一致性振幅补偿。When it is determined that the verification result meets the second preset condition, the corresponding seismic trace data in the suspected non-surface consistent data volume is eliminated or non-surface consistency amplitude compensation is performed.
  9. 根据权利要求8所述的方法,其特征在于,对所述疑似非地表一致性数据体中对应地震道数据进行非地表一致性振幅补偿包括:The method of claim 8 wherein performing non-surface consistency amplitude compensation on the corresponding seismic trace data in the suspected non-surface consistent data volume comprises:
    按照公式
    Figure PCTCN2015074246-appb-100005
    计算所述具有代表性的数据体中对应地震数据经过地表一致性振幅补偿之后的期望值,其中,公式中K是所述具有代表性的数据体中地震道的总数;
    According to the formula
    Figure PCTCN2015074246-appb-100005
    Calculating an expected value of the corresponding seismic data in the representative data volume after the surface consistency amplitude compensation, wherein K is the total number of seismic traces in the representative data volume;
    按照公式Scalem=Expect/Engm,计算非地表一致性补偿因子作为最终的补偿因子;Calculate the non-surface consistency compensation factor as the final compensation factor according to the formula Scale m =Expect/Eng m ;
    根据所述最终的补偿因子,对所述疑似非地表一致性数据体中对应地震道数据进行非地表一致性振幅补偿。And performing non-surface consistency amplitude compensation on the corresponding seismic trace data in the suspected non-surface consistent data volume according to the final compensation factor.
  10. 一种共姿态道集地表一致性振幅补偿装置,其特征在于,包括:A common attitude gather surface consistency amplitude compensation device, comprising:
    获取单元,用于获取勘探工区中的地震数据及其对应的施工班报;An acquisition unit, configured to acquire seismic data in a exploration work area and a corresponding construction work report;
    第一计算单元,用于计算所述获取单元获取的所述地震数据中每一道地震数据的所有分量的平均总能量,得到该道的地震道能量;a first calculating unit, configured to calculate an average total energy of all components of each piece of seismic data in the seismic data acquired by the acquiring unit, to obtain a seismic channel energy of the track;
    检验单元,用于对各个所述第一计算单元计算得到的所述地震道能量进行地表一致性初步检验;a verification unit, configured to perform a preliminary test of surface consistency on the seismic energy calculated by each of the first computing units;
    第一确定单元,用于将符合第一预设条件的所有地震道能量确定为具有代表性的数据体;a first determining unit, configured to determine all seismic energy of the first predetermined condition as a representative data volume;
    第二计算单元,用于在所述第一确定单元确定的所述具有代表性的数据体中计算每一道地震道能量对应的各项补偿因子,所述各项补偿因子至少包括震源项补偿因子;a second calculating unit, configured to calculate, according to the representative data body determined by the first determining unit, each compensation factor corresponding to each track energy, where the compensation factors include at least a source term compensation factor ;
    抽取单元,用于根据检波器的不同姿态,在所述勘探工区的共检波点道集中抽取共姿态道集;Extracting unit, configured to extract a common attitude gather in the common detection wave point of the exploration work area according to different postures of the detector;
    第三计算单元,用于在所述抽取单元抽取的所述共姿态道集中计算检波器项补偿因子;a third calculating unit, configured to calculate a detector term compensation factor in the common attitude track set extracted by the extracting unit;
    地表一致性振幅补偿单元,用于根据所述第二计算单元计算得到的所述各项补偿因子以及所述第三计算单元计算得到的检波器项补偿因子构成的总补偿因子,对所述整个工区的地震数据进行地表一致性振幅补偿。 a surface consistency amplitude compensation unit, configured to calculate, according to the compensation factors calculated by the second calculating unit, a total compensation factor formed by the detector term compensation factor calculated by the third calculating unit, for the whole Seismic data from the work area is used for surface consistency amplitude compensation.
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