CN106547027A - A kind of data processing method and device for obtaining dynamic(al) correction parameter - Google Patents

A kind of data processing method and device for obtaining dynamic(al) correction parameter Download PDF

Info

Publication number
CN106547027A
CN106547027A CN201710015203.1A CN201710015203A CN106547027A CN 106547027 A CN106547027 A CN 106547027A CN 201710015203 A CN201710015203 A CN 201710015203A CN 106547027 A CN106547027 A CN 106547027A
Authority
CN
China
Prior art keywords
similarity coefficient
spectrum
normalized
dynamic
anisotropic parameters
Prior art date
Legal status (The legal status is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the status listed.)
Pending
Application number
CN201710015203.1A
Other languages
Chinese (zh)
Inventor
任岩
蔡郁文
杨廷强
黄昱丞
王纯
Current Assignee (The listed assignees may be inaccurate. Google has not performed a legal analysis and makes no representation or warranty as to the accuracy of the list.)
China Petroleum and Natural Gas Co Ltd
Original Assignee
China Petroleum and Natural Gas Co Ltd
Priority date (The priority date is an assumption and is not a legal conclusion. Google has not performed a legal analysis and makes no representation as to the accuracy of the date listed.)
Filing date
Publication date
Application filed by China Petroleum and Natural Gas Co Ltd filed Critical China Petroleum and Natural Gas Co Ltd
Priority to CN201710015203.1A priority Critical patent/CN106547027A/en
Publication of CN106547027A publication Critical patent/CN106547027A/en
Pending legal-status Critical Current

Links

Classifications

    • 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. analysis, for interpretation, for correction
    • G01V1/36Effecting static or dynamic corrections on records, e.g. correcting spread; Correlating seismic signals; Eliminating effects of unwanted energy
    • G01V1/362Effecting static or dynamic corrections; Stacking
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V2210/00Details of seismic processing or analysis
    • G01V2210/50Corrections or adjustments related to wave propagation
    • G01V2210/52Move-out correction

Abstract

The application provides a kind of data processing method and device for obtaining dynamic(al) correction parameter.Methods described includes:Using the corresponding geological data of middle near migration range common midpoint gather reset, differential similarity coefficient operator is calculated;Using differential similarity coefficient operator, the similarity coefficient normal-moveout spectrum is normalized;Root mean sequare velocity is picked up from the normalized similarity coefficient normal-moveout spectrum;Preliminary dynamic(al) correction process is carried out using described root mean sequare velocity;Using the corresponding geological data of common midpoint gather after the preliminary dynamic(al) correction reset, corresponding differential similitude operator is calculated;Using the differential similarity coefficient operator, similarity coefficient anisotropic parameters spectrum is normalized, obtains normalized similarity coefficient anisotropic parameters spectrum;Anisotropic parameters is picked up from the normalized similarity coefficient anisotropic parameters spectrum.Using each embodiment in the application, the lateral resolution of the Parameter Spectrum can be effectively improved, and then effectively improves the precision of the dynamic(al) correction parameter.

Description

A kind of data processing method and device for obtaining dynamic(al) correction parameter
Technical field
The application is related to seismic data processing technology field, more particularly to a kind of data processing side for obtaining dynamic(al) correction parameter Method and device.
Background technology
Travel time curve, also known as time curve, is between the time required for representing the distance of seimic wave propagation and propagating Relation curve.Travel time curve is the important foundation of Study of The Underground interface configuration.But, travel time curve is usually hyperbolic shape , wherein the echo time for only receiving at shot point represents the normal reflection time at interface, therefore each must be seen The time value of measuring point all becomes the normal reflection time of respective points, time curve or lineups form one just with subsurface interface Cause.This is accomplished by carrying out dynamic(al) correction process, eliminates the NMO (normal moveout) that seismic wave reaches each geophone station.During dynamic(al) correction is processed, move The precision of correction parameter, is the key factor for determining dynamic(al) correction treatment effect.
In prior art, at least there are the following problems:In prior art, dynamic(al) correction parameter is obtained, often joined from dynamic(al) correction Pickup in number spectrum obtains the dynamic(al) correction parameter.But, often there is energy group hangover in dynamic(al) correction Parameter Spectrum of the prior art Phenomenon, causes the lateral resolution of the dynamic(al) correction Parameter Spectrum relatively low, and then the precision of the dynamic(al) correction parameter that can cause to pick up It is relatively low.
The content of the invention
The purpose of the embodiment of the present application is to provide a kind of data processing method and device for obtaining dynamic(al) correction parameter
The embodiment of the present application provides what a kind of data processing method and device for obtaining dynamic(al) correction parameter was realized in:
A kind of data processing method for obtaining dynamic(al) correction parameter, methods described include:
M rearrangement is carried out to the middle shortcut in the common midpoint gather of pending geological data, obtains near during M groups are reset Road collection, controls there is the time difference, M >=1 between each pair neighboring track during rearrangement;
The corresponding geological data of middle near-trace gather reset using the M groups, is calculated M group differential similarity coefficient operators;
Using the M groups differential similarity coefficient operator, initial similarity coefficient-normal-moveout spectrum is normalized, is obtained Normalized similarity coefficient-normal-moveout spectrum;
Root mean sequare velocity is picked up from the normalized similarity coefficient-normal-moveout spectrum;
Preliminary dynamic(al) correction process is carried out to the pending geological data using described root mean sequare velocity, is tentatively moved Common midpoint gather after correction;
Whole roads in common midpoint gather after the preliminary dynamic(al) correction are carried out with R rearrangement, the road of R groups rearrangement is obtained Collection, controls there is the time difference, R >=1 between each pair neighboring track during rearrangement;
The corresponding geological data of road collection reset using the R groups, is calculated R group differential similitude operators;
Using the R groups differential similarity coefficient operator, place is normalized to initial similarity coefficient-anisotropic parameters spectrum Reason, obtains normalized similarity coefficient-anisotropic parameters spectrum;
Anisotropic parameters is picked up from the normalized similarity coefficient-anisotropic parameters spectrum;
Using the root mean sequare velocity and the anisotropic parameters as the dynamic(al) correction parameter.
In preferred embodiment, the mode for controlling to there is the time difference between each pair neighboring track during rearrangement, bag Include:
According to the skew in the middle near migration range road collection Huo and the common midpoint gather Zhong Ge roads after the preliminary dynamic(al) correction Away from size, the road collection is reset, realize there is the time difference between the control each pair neighboring track.
It is in preferred embodiment, described using the M groups differential similarity coefficient operator, the similarity coefficient-normal-moveout spectrum is entered The mode of row normalized, including being normalized to the similarity coefficient-normal-moveout spectrum using following formula, is returned One similarity coefficient-the normal-moveout spectrum changed:
In formula,Represent M group differential similarity coefficient operators;
V represents root mean sequare velocity;
ND TR DvSimilarity coefficient when table S shows that root mean sequare velocity is v.
It is in preferred embodiment, described using the R groups differential similarity coefficient operator, to the similarity coefficient-anisotropy The mode that Parameter Spectrum is normalized, is carried out including being composed to the similarity coefficient-anisotropic parameters using following formula Normalized, obtains normalized similarity coefficient-anisotropic parameters spectrum:
In formula,Represent R group differential similarity coefficient operators;
η represents anisotropic parameters;
NDTRDSηSimilarity coefficient when representing that anisotropic parameters is η.
In preferred embodiment, the acquisition modes of the initial similarity coefficient-normal-moveout spectrum, including:
It is using the geological data and non-double curve travel time curve of the middle near migration range road collection, bent when being walked according to the non-double curve The low order portion of line and the similarity coefficient computing formula, are calculated similarity coefficient-normal-moveout spectrum.
In preferred embodiment, the expression formula of the low order portion of the non-double curve travel time curve includes:
In formula, X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0.
In preferred embodiment, the similarity coefficient, including being calculated using following formula:
In formula, S represents similarity coefficient;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
In preferred embodiment, the mode of the initial similarity coefficient-anisotropic parameters spectrum, including:
Walked using the corresponding geological data in whole roads in the common midpoint gather after the preliminary dynamic(al) correction, and non-double curve When curve;
According to the non-double curve travel time curve and the similarity coefficient computing formula for having substituted into the root mean sequare velocity, calculate To similarity coefficient-anisotropic parameters spectrum
In preferred embodiment, the expression formula of the non-double curve travel time curve includes:
In formula:X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0;
η represents anisotropic parameters.
In preferred embodiment, the differential similarity coefficient operator, including being calculated using following formula:
In formula,Represent the differential similarity coefficient operator;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
t0Represent that offset distance is the corresponding propagation time at 0;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
A kind of data processing equipment for obtaining dynamic(al) correction parameter, described device include:
Middle near-trace gather reordering module, for the common midpoint gather to pending geological data in middle shortcut carry out M time Reset, obtain the middle near-trace gather of M groups rearrangement, control there is the time difference, M >=1 between each pair neighboring track during rearrangement;
Preliminary dynamic(al) correction module, for utilizing described root mean sequare velocity tentatively to move the pending geological data Correction process, obtains the common midpoint gather after preliminary dynamic(al) correction;
Common midpoint gather reordering module, for entering to the whole roads in the common midpoint gather after the preliminary dynamic(al) correction R rearrangement of row, obtains the road collection of R groups rearrangement, controls there is the time difference, R >=1 between each pair neighboring track during rearrangement;
Parameter Spectrum acquisition module, for the geological data according to the middle shortcut, is calculated similarity coefficient-normal-moveout spectrum, It is additionally operable to according to the corresponding earthquake in whole roads in the common midpoint gather after the root mean sequare velocity and the preliminary dynamic(al) correction Data, are calculated similarity coefficient-anisotropic parameters spectrum;
Normalized module, for using the M groups differential similarity coefficient operator, to initial similarity coefficient-normal-moveout spectrum It is normalized, obtains normalized similarity coefficient-normal-moveout spectrum, is additionally operable to using the R groups differential similarity coefficient operator, Initial similarity coefficient-anisotropic parameters spectrum is normalized, normalized similarity coefficient-anisotropic parameters is obtained Spectrum;
Parameter pickup model, for picking up root mean sequare velocity from the normalized similarity coefficient-normal-moveout spectrum, is additionally operable to Anisotropic parameters is picked up from the normalized similarity coefficient-anisotropic parameters spectrum;
Data generation module, for the root mean sequare velocity and the anisotropic parameters are joined as the dynamic(al) correction Number.
A kind of data processing method of the acquisition dynamic(al) correction parameter provided using the embodiment of the present application, can be by road collection Enter the mode of rearrangement, make there is the time difference between each pair neighboring track in the road collection of rearrangement, due to differential similarity coefficient operator over the ground Between shake road, the sensitivity of the time difference is higher, makes there is the time difference between each pair neighboring track, it is possible to so that differential similarity coefficient operator is most Bigization.And then using the differential similarity coefficient operator to initial similarity coefficient-normal-moveout spectrum and initial similarity coefficient-anisotropy Parameter Spectrum carries out one or many normalized, can effectively improve the lateral resolution of described two Parameter Spectrums.Using horizontal stroke Similarity coefficient-the normal-moveout spectrum improved to resolution and similarity coefficient-anisotropic parameters spectrum, the dynamic(al) correction parameter that pickup is obtained Precision is higher, effectively increases the precision of the root mean sequare velocity and two kinds of dynamic(al) correction parameters of anisotropic parameter.Utilize A kind of data processing equipment of acquisition dynamic(al) correction parameter that the embodiment of the present application is provided, can perform said method, automatically automatically Obtain the dynamic(al) correction parameter that simultaneously output accuracy is improved, it is not necessary to implement the excessive participation of personnel, it is convenient to operation, effectively improve Consumer's Experience.
Description of the drawings
In order to be illustrated more clearly that the embodiment of the present application or technical scheme of the prior art, below will be to embodiment or existing Accompanying drawing to be used needed for having technology description is briefly described, it should be apparent that, drawings in the following description are only this Some embodiments described in application, for those of ordinary skill in the art, in the premise for not paying creative labor Under, can be with according to these other accompanying drawings of accompanying drawings acquisition.
Fig. 1 is a kind of method flow of the data processing method of acquisition dynamic(al) correction parameter that the application one embodiment is provided Schematic diagram;
Fig. 2 is a kind of modular structure of the data processing equipment of acquisition dynamic(al) correction parameter that the application one embodiment is provided Schematic diagram;
Fig. 3 is the seismic channel set in the application one embodiment not through the seismic channel set reset and through resetting;
Fig. 4 be the seismic channel set of the pending geological data in the application one embodiment and get similarity coefficient- Normal-moveout spectrum;
Fig. 5 is the seismic channel set of the pending geological data in the application another embodiment and the similar system for getting Number-anisotropic parameters is composed.
Specific embodiment
The embodiment of the present application provides a kind of data processing method and device for obtaining dynamic(al) correction parameter.
In order that those skilled in the art more fully understand the technical scheme in the application, below in conjunction with the application reality The accompanying drawing in example is applied, the technical scheme in the embodiment of the present application is clearly and completely described, it is clear that described enforcement Example is only some embodiments of the present application, rather than the embodiment of whole.Based on the embodiment in the application, this area is common The every other embodiment obtained under the premise of creative work is not made by technical staff, should all belong to the application protection Scope.
Fig. 1 is that a kind of a kind of herein described method flow of embodiment of data processing method for obtaining dynamic(al) correction parameter shows It is intended to.Although this application provides such as following embodiments or method operating procedure shown in the drawings or apparatus structure, based on normal Rule can include more or less operating procedures or module in methods described or device without the need for performing creative labour Unit.In the step of there is no necessary cause effect relation in logicality or structure, the mould of the execution sequence or device of these steps Block structure is not limited to the embodiment of the present application or execution sequence shown in the drawings or modular structure.Described method or modular structure When device in practice or end product application, can carry out according to embodiment or method shown in the drawings or modular structure Order is performed or executed in parallel (environment of such as parallel processor or multiple threads, even including distributed treatment Implementation environment).
Specifically as described in Figure 1, a kind of one kind of the data processing method of acquisition dynamic(al) correction parameter that the application is provided is real Applying example can include:
S1:M rearrangement is carried out to the middle shortcut in the common midpoint gather of pending geological data, the rearrangement of M groups is obtained Middle near-trace gather, controls there is the time difference, M >=1 between each pair neighboring track during rearrangement.
Common midpoint gather after the preliminary dynamic(al) correction can be obtained by pending geological data is taken out road collection.
The middle shortcut includes seismic channel of the offset distance with the ratio of depth less than or equal to 1.5.
In the application one embodiment, the mode of the rearrangement is reset for definitiveness, and each pair phase is controlled during rearrangement There is the mode of the time difference between neighboring trace, can include:
According to the middle near-trace gather Huo and the offset distance size in the common midpoint gather Zhong Ge roads, to the middle shortcut Enter rearrangement, realize there is the time difference between the control each pair neighboring track.
It is by according to offset distance size, resetting to middle the being determined property of near-trace gather Zhong Ge roads, specifically, such as, false Road collection x of the Ding Yitiao roads number for N=2m, the output road collection after definitiveness road is resetFor [x1, xm+1, x2, xm+2..., xk, xm+k..., xm, xN], neighboring track is lined up by offset distance is differed larger road, it is possible to achieve deposit between control each pair neighboring track In the effect of the obvious time difference.
(a) figure in Fig. 3 is in the application one embodiment not through the seismic channel set reset, (b) in Fig. 3 Figure is to enter the rearrangement that rearrangement after obtain to the corresponding seismic channel set of (a) figure in Fig. 3 using the rearranged form described in this method Seismic channel set afterwards.In (a) figure and (b) figure in Fig. 3, abscissa all represents offset distance (offset, offset distance), vertical coordinate all tables Show the time, it can be seen that after definitiveness is reset, in the road collection after rearrangement, between neighboring track, be clearly present the time difference.
S2:The corresponding geological data of middle near-trace gather reset using the M groups, is calculated the calculation of M group differential similarity coefficient Son.
The M be more than or equal to 1, it is preferable that rearrangement more than twice can be carried out in the embodiment of the present application, obtain two groups with On differential similarity coefficient operator.
The differential similarity coefficient operator, can include being calculated using following formula:
In formula,Represent the differential similarity coefficient operator;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
t0Represent that offset distance is the corresponding propagation time at 0;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
S3:Using the M groups differential similarity coefficient operator, initial similarity coefficient-normal-moveout spectrum is normalized, is obtained To normalized similarity coefficient-normal-moveout spectrum.
The M is more than or equal to 1, it is preferable that in the embodiment of the present application, using two groups and differential similarity coefficient more than two Operator, is normalized to initial similarity coefficient-normal-moveout spectrum, can preferably improve spectral resolution, the differential phase of employing More like the group number of coefficient operator, resolution is higher.
In the application one embodiment, using the M groups differential similarity coefficient operator, to the similarity coefficient-normal-moveout spectrum The mode being normalized, can include being normalized the similarity coefficient-normal-moveout spectrum using following formula, Obtain normalized similarity coefficient-normal-moveout spectrum:
In formula,Represent M group differential similarity coefficient operators;
V represents root mean sequare velocity;
ND TR DvSimilarity coefficient when table S shows that root mean sequare velocity is v.
In the application another embodiment, the acquisition modes of the initial similarity coefficient-normal-moveout spectrum can include:
Using the geological data and non-double curve travel time curve of the middle near migration range road collection,
According to the low order portion and the similarity coefficient computing formula of the non-double curve travel time curve, similar system is calculated Number-normal-moveout spectrum.
The expression formula of the low order portion of the non-double curve travel time curve can include:
In formula, X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0.
The similarity coefficient formula is calculated can be included:
In formula, S represents similarity coefficient;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
(a) figure in Fig. 4 is CMP (CMP) road collection of the pending geological data in the application one embodiment, Wherein, vertical coordinate express time, abscissa represent offset distance.(b) figure in Fig. 4 is according to figure using existing Similar operator Similarity coefficient-normal-moveout spectrum that (a) figure in 4 gets.(c) figure, (d) figure, (e) figure in Fig. 4 be respectively carry out 1 time, 2 times, 3 After secondary rearrangement, through similarity coefficient-normal-moveout spectrum that normalized is obtained, in Fig. 4, v represents speed, and unit is metre per second (m/s).Can To find out, after rearrangement, spectral resolution is improved significantly, and the number of times reset is more, obtains after normalized The resolution of spectrum is higher.
S4:Root mean sequare velocity is picked up from the normalized similarity coefficient-normal-moveout spectrum.
The root mean sequare velocity can be used as the parameter of dynamic(al) correction.
The mode of the pickup root mean sequare velocity, can voluntarily be selected by enforcement personnel, and the application is not limited.
S5:Preliminary dynamic(al) correction process is carried out to the pending geological data using described root mean sequare velocity, is obtained just Common midpoint gather after step dynamic(al) correction.
The processing mode that the preliminary dynamic(al) correction is processed, enforcement personnel voluntarily can be selected, and concrete limit is not done in the application It is fixed.
S6:Whole roads in common midpoint gather after the preliminary dynamic(al) correction are carried out with R rearrangement, the rearrangement of R groups is obtained Road collection, during rearrangement control each pair neighboring track between there is the time difference, R >=1.
In the application one embodiment, the mode of the rearrangement is reset for definitiveness, and each pair phase is controlled during rearrangement There is the mode of the time difference between neighboring trace, can include:
According to the middle near-trace gather Huo and the offset distance size in the common midpoint gather Zhong Ge roads, to the middle shortcut Enter rearrangement, realize there is the time difference between the control each pair neighboring track.
By according to offset distance size, resetting to being determined property of the concentrically road collection Zhong Ge road.
S7:The corresponding geological data of road collection reset using the R groups, is calculated R group differential similitude operators.
The calculation of the differential similitude operator is with step S2.
S8:Using the R groups differential similarity coefficient operator, normalizing is carried out to initial similarity coefficient-anisotropic parameters spectrum Change is processed, and obtains normalized similarity coefficient-anisotropic parameters spectrum.
In the application one embodiment, using the R groups differential similarity coefficient operator, to the similarity coefficient-each to different The mode that property Parameter Spectrum is normalized, can be included using following formula to the similarity coefficient-anisotropic parameters Spectrum is normalized, and obtains normalized similarity coefficient-anisotropic parameters spectrum:
In formula,Represent R group differential similarity coefficient operators;
η represents anisotropic parameters;
NDTRDSηSimilarity coefficient when representing that anisotropic parameters is η.
In the application one embodiment, the acquisition modes of the initial similarity coefficient-anisotropic parameters spectrum can be wrapped Include:
Walked using the corresponding geological data in whole roads and non-double curve in the common midpoint gather after the preliminary dynamic(al) correction When curve, according to the non-double curve travel time curve and the similarity coefficient computing formula for having substituted into the root mean sequare velocity, calculate To similarity coefficient-anisotropic parameters spectrum.
In the application another embodiment, the expression formula of the non-double curve travel time curve can include:
In formula:X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0;
η represents anisotropic parameters.
(a) figure in Fig. 5 is CMP (CMP) road collection of the geological data containing residual normal moveout, wherein, vertical coordinate Express time, abscissa represent offset distance.(b) figure in Fig. 5 be got using existing conventional Similar operator frequency- Anisotropic parameters compose, (c) figure, (d) figure, (e) figure in Fig. 5 be respectively carried out 1 time, 3 times, 6 times reset after, carry out normalizing Change processes the frequency-anisotropic parameters frequency dispersion spectrum for obtaining, and in Fig. 5, η represents anisotropic parameters.It can be seen that sharp The frequency got with conventional Similar operator-anisotropic parameters spectrum, the poor difference of mid-deep strata energy group focusing, affecting parameters Pickup precision.After entering rearrangement, when it is 1 to reset number of times, in the spectrum for getting, energy group focusing makes moderate progress, and resolution is obtained To effectively improving.Rearrangement number of times is higher, and energy group focusing can more be improved, and resolution is higher.Illustrate to utilize the application Methods described can effectively improve the lateral resolution of frequency-anisotropic parameters spectrum, higher such that it is able to pick up precision Anisotropic parameters.
S9:Anisotropic parameters is picked up from the normalized similarity coefficient-anisotropic parameters spectrum.
The anisotropic parameters can be used as the parameter of dynamic(al) correction.
Herein described anisotropic parameters is equivalent anisotropic parameters, and its expression formula includes:
In formula, ε represents compressional wave anisotropic parameters;
δ represents the parameter for affecting compressional wave velocity magnitude in nearly vertical direction.
The mode of the pickup anisotropic parameters, can voluntarily be selected by enforcement personnel, and the application is not limited.
S10:Using the root mean sequare velocity and the anisotropic parameters as the dynamic(al) correction parameter.
Preliminary dynamic(al) correction can be carried out to travel time curve using the root mean sequare velocity.
Further high-order NMO can be carried out to travel time curve using the anisotropic parameters.
A kind of data processing method of the acquisition dynamic(al) correction parameter provided using the various embodiments described above, can be by road collection Enter the mode of rearrangement, make there is the time difference between each pair neighboring track in the road collection of rearrangement, due to differential similarity coefficient operator over the ground Between shake road, the sensitivity of the time difference is higher, makes there is the time difference between each pair neighboring track, it is possible to so that differential similarity coefficient operator is most Bigization.And then using the differential similarity coefficient operator to initial similarity coefficient-normal-moveout spectrum and initial similarity coefficient-anisotropy Parameter Spectrum carries out one or many normalized, can effectively improve the lateral resolution of described two Parameter Spectrums.Using horizontal stroke Similarity coefficient-the normal-moveout spectrum improved to resolution and similarity coefficient-anisotropic parameters spectrum, the dynamic(al) correction parameter that pickup is obtained Precision is higher, effectively increases the precision of the root mean sequare velocity and two kinds of dynamic(al) correction parameters of anisotropic parameter.
Based on the data processing method for obtaining dynamic(al) correction parameter described herein, the application provides a kind of acquisition dynamic(al) correction The data processing equipment of parameter, described device can be integrated in dynamic(al) correction component, carry out dynamic(al) correction process.Fig. 2 is the application The modular structure schematic diagram of the data processing equipment of the acquisition dynamic(al) correction parameter provided in one embodiment.Specifically, such as Fig. 2 institutes Show, described device can include:
Middle near-trace gather reordering module 101, the middle shortcut that can be used in the common midpoint gather to pending geological data M rearrangement is carried out, the middle near-trace gather of M groups rearrangement is obtained, controls there is the time difference between each pair neighboring track during rearrangement, M≥1。
Preliminary dynamic(al) correction module 102, can be used for entering the pending geological data using described root mean sequare velocity The preliminary dynamic(al) correction of row is processed, and obtains the common midpoint gather after preliminary dynamic(al) correction.
Common midpoint gather reordering module 103, can be used in the common midpoint gather after the preliminary dynamic(al) correction Whole roads carry out R rearrangement, obtain the road collection of R groups rearrangement, control during rearrangement it is equal between each pair neighboring track in the presence of Difference, R >=1.
Parameter Spectrum acquisition module 104, can be used for the geological data according to the middle shortcut, be calculated similarity coefficient- Normal-moveout spectrum, is additionally operable to corresponding according to the whole roads in the common midpoint gather after the root mean sequare velocity and the preliminary dynamic(al) correction Geological data, be calculated similarity coefficient-anisotropic parameters spectrum;
Normalized module 105, can be used for using the M groups differential similarity coefficient operator, to initial similarity coefficient- Normal-moveout spectrum is normalized, and obtains normalized similarity coefficient-normal-moveout spectrum, can be also used for using the R groups differential phase Like coefficient operator, initial similarity coefficient-anisotropic parameters spectrum is normalized, obtain normalized similarity coefficient- Anisotropic parameters is composed.
Parameter pickup model 106, can be used for root-mean-square speed is picked up from the normalized similarity coefficient-normal-moveout spectrum Degree, can be also used for picking up anisotropic parameters from the normalized similarity coefficient-anisotropic parameters spectrum.
Data generation module 107, can be used for the root mean sequare velocity and the anisotropic parameters are moved as described Correction parameter.
A kind of data processing equipment of the acquisition dynamic(al) correction parameter provided using above-described embodiment, can perform this Shen automatically Please methods described, automatically derive and output accuracy improve dynamic(al) correction parameter, it is not necessary to implement the excessive participation of personnel, operation side Just it is quick, effectively increase Consumer's Experience.
It is in the data processing equipment for obtaining dynamic(al) correction parameter, described to enter rearrangement to road collection, be calculated differential phase It is normalized like coefficient operator, to initial similarity coefficient-normal-moveout spectrum, initial similarity coefficient-anisotropic parameters is composed Be normalized, from the normalized similarity coefficient-normal-moveout spectrum pick up root mean sequare velocity, from the normalized phase Like anisotropic parameters is picked up in coefficient-anisotropic parameters spectrum to the root mean sequare velocity and the anisotropic parameters are made Extension for the embodiment of the dynamic(al) correction parameter is referred to the associated description of preceding method.
Although the data processing methods of different acquisition dynamic(al) correction parameters are mentioned in teachings herein, from weight is carried out to road collection Row, be calculated differential similarity coefficient operator, initial similarity coefficient-normal-moveout spectrum be normalized, to initial similar system Number-anisotropic parameters spectrum is normalized, root-mean-square speed is picked up from the normalized similarity coefficient-normal-moveout spectrum Degree, anisotropic parameters is picked up from the normalized similarity coefficient-anisotropic parameters spectrum to by the root mean sequare velocity With the anisotropic parameters as the various sequential manners of the dynamic(al) correction parameter, data acquisition/process/way of output etc. Description, but, the application is not limited to be industry standard or the situation described by embodiment etc., some industry standards or Person can also realize above-mentioned reality using embodiment amended slightly on the practice processes of self-defined mode or embodiment description Apply example it is identical, equivalent or it is close, or deformation after foreseeable implementation result.Using these modification or deform after data acquisition, The embodiment of process, output, judgment mode etc., within the scope of still may belong to the optional embodiment of the application.
Although this application provides the method operating procedure as described in embodiment or flow chart, is based on routine or noinvasive The means of the property made can include more or less operating procedures.The step of enumerating in embodiment order is only numerous steps A kind of mode in execution sequence, does not represent unique execution sequence.When device or client production in practice is performed, can To perform or executed in parallel (such as at parallel processor or multithreading according to embodiment or method shown in the drawings order The environment of reason, even distributed data processing environment).Term " including ", "comprising" or its any other variant are intended to contain Lid nonexcludability is included, so that a series of process, method, product or equipment including key elements not only will including those Element, but also including other key elements being not expressly set out, or also include for this process, method, product or equipment Intrinsic key element.In the absence of more restrictions, it is not excluded that including the process of the key element, method, product or Also there are other identical or equivalent elements in person's equipment.
Device that above-described embodiment is illustrated or module etc., specifically can be realized by computer chip or entity, or by having There is the product of certain function to realize.For convenience of description, it is divided into various modules with function when describing apparatus above to retouch respectively State.Certainly, the function of each module can be realized in same or multiple softwares and/or hardware when the application is implemented, The module for realizing same function can be realized by the combination of multiple submodule etc..Device embodiment described above is only Schematically, for example, the division of the module, only a kind of division of logic function can have other drawing when actually realizing Point mode, such as multiple module or components can with reference to or be desirably integrated into another system, or some features can be ignored, Or do not perform.
It is also known in the art that in addition to realizing controller in pure computer readable program code mode, it is complete Entirely can by by method and step carry out programming in logic cause controller with gate, switch, special IC, may be programmed The form of logic controller and embedded microcontroller etc. is realizing identical function.Therefore this controller is considered one kind Hardware component, and the device for realizing various functions included to its inside can also be considered as the structure in hardware component.Or Person even, can be used for realizing that the device of various functions be considered as not only being the software module of implementation method but also being hardware Structure in part.
The application can be described in the general context of computer executable instructions, such as program Module.Usually, program module includes execution particular task or realizes the routine of particular abstract data type, program, object, group Part, data structure, class etc..The application is put into practice in a distributed computing environment can also, in these distributed computing environment, Task is performed by the remote processing devices connected by communication network.In a distributed computing environment, program module can With positioned at including in the local and remote computer-readable storage medium including storage device.
As seen through the above description of the embodiments, those skilled in the art can be understood that the application can By software plus required general hardware platform mode realizing.Based on such understanding, the technical scheme essence of the application On part that in other words prior art is contributed can be embodied in the form of software product, the computer software product Can be stored in storage medium, such as ROM/RAM, magnetic disc, CD etc., use so that a computer equipment including some instructions (can be personal computer, mobile terminal, server, or network equipment etc.) performs each embodiment of the application or enforcement Method described in some parts of example.
Each embodiment in this specification is described by the way of progressive, same or analogous portion between each embodiment Divide mutually referring to what each embodiment was stressed is the difference with other embodiment.The application can be used for crowd In more general or special purpose computing system environments or configuration.For example:Personal computer, server computer, handheld device or Portable set, laptop device, multicomputer system, set based on the system of microprocessor, set top box, programmable electronics Standby, network PC, minicomputer, mainframe computer, including the distributed computing environment etc. of any of the above system or equipment.
Although depicting the application by embodiment, it will be appreciated by the skilled addressee that the application have it is many deformation and Change is without deviating from spirit herein, it is desirable to which appended claim includes these deformations and changes without deviating from the application's Spirit.

Claims (11)

1. it is a kind of obtain dynamic(al) correction parameter data processing method, it is characterised in that methods described includes:
M rearrangement is carried out to the middle shortcut in the common midpoint gather of pending geological data, the middle shortcut of M groups rearrangement is obtained Collection, controls there is the time difference, M >=1 between each pair neighboring track during rearrangement;
The corresponding geological data of middle near-trace gather reset using the M groups, is calculated M group differential similarity coefficient operators;
Using the M groups differential similarity coefficient operator, initial similarity coefficient-normal-moveout spectrum is normalized, normalizing is obtained Similarity coefficient-the normal-moveout spectrum of change;
Root mean sequare velocity is picked up from the normalized similarity coefficient-normal-moveout spectrum;
Preliminary dynamic(al) correction process is carried out to the pending geological data using described root mean sequare velocity, preliminary dynamic(al) correction is obtained Common midpoint gather afterwards;
Whole roads in common midpoint gather after the preliminary dynamic(al) correction are carried out with R rearrangement, the road collection of R groups rearrangement is obtained, Control there is the time difference, R >=1 between each pair neighboring track during rearrangement;
The corresponding geological data of road collection reset using the R groups, is calculated R group differential similitude operators;
Using the R groups differential similarity coefficient operator, initial similarity coefficient-anisotropic parameters spectrum is normalized, Obtain normalized similarity coefficient-anisotropic parameters spectrum;
Anisotropic parameters is picked up from the normalized similarity coefficient-anisotropic parameters spectrum;
Using the root mean sequare velocity and the anisotropic parameters as the dynamic(al) correction parameter.
2. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that described to reset During control between each pair neighboring track, the presence of the mode of the time difference, including:
It is big according to the offset distance of the middle near migration range road collection Huo and the common midpoint gather Zhong Ge roads after the preliminary dynamic(al) correction It is little, the road collection is reset, realizes there is the time difference between the control each pair neighboring track.
3. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that the utilization institute State M group differential similarity coefficient operators, the mode being normalized to the similarity coefficient-normal-moveout spectrum, including using following Formula is normalized to the similarity coefficient-normal-moveout spectrum, obtains normalized similarity coefficient-normal-moveout spectrum:
In formula,Represent M group differential similarity coefficient operators;
V represents root mean sequare velocity;
ND TRDvSimilarity coefficient when table S shows that root mean sequare velocity is v.
4. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that the utilization institute R group differential similarity coefficient operators are stated, the mode is normalized by the similarity coefficient-anisotropic parameters spectrum, including The similarity coefficient-anisotropic parameters spectrum is normalized using following formula, obtain normalized similarity coefficient- Anisotropic parameters is composed:
In formula,Represent R group differential similarity coefficient operators;
η represents anisotropic parameters;
NDTRDSηSimilarity coefficient when representing that anisotropic parameters is η.
5. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that the initial phase Like the acquisition modes of coefficient-normal-moveout spectrum, including:
Using the geological data and non-double curve travel time curve of the middle near migration range, according to the low order of the non-double curve travel time curve Part and the similarity coefficient computing formula, are calculated similarity coefficient-normal-moveout spectrum.
6. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 5, it is characterised in that the non-double curve The expression formula of the low order portion of travel time curve includes:
In formula, X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0.
7. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 5, it is characterised in that the similar system Number formula is calculated and is included:
In formula, S represents similarity coefficient;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
8. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that the initial phase Like the acquisition modes of coefficient-anisotropic parameters spectrum, including:
According to the corresponding geological data in whole roads in the common midpoint gather after the preliminary dynamic(al) correction, when acquisition non-double curve is walked Curve;
According to the non-double curve travel time curve and the similarity coefficient computing formula for having substituted into the root mean sequare velocity, phase is calculated Like coefficient-anisotropic parameters spectrum.
9. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 8, it is characterised in that the non-double curve The expression formula of travel time curve includes:
In formula:X represents offset distance;
T (X) represents the offset distance X corresponding propagation times;
V represents root mean sequare velocity;
t0Represent that offset distance is the corresponding propagation time at 0;
η represents anisotropic parameters.
10. a kind of data processing method for obtaining dynamic(al) correction parameter as claimed in claim 1, it is characterised in that the differential Similarity coefficient operator, including being calculated using following formula:
In formula,Represent the differential similarity coefficient operator;
N represents the corresponding total road number of geological data;
xiRepresent the offset distance in the i-th road;
Window width when λ is represented;
t0Represent that offset distance is the corresponding propagation time at 0;
d(t,xi) represent t time points, offset distance xiThe amplitude at place.
11. a kind of data processing equipments for obtaining dynamic(al) correction parameter, it is characterised in that described device includes:
Middle near-trace gather reordering module, for the common midpoint gather to pending geological data in middle shortcut carry out M time rearrangement, The middle near-trace gather of M groups rearrangement is obtained, controls there is the time difference, M >=1 between each pair neighboring track during rearrangement;
Preliminary dynamic(al) correction module, for utilizing described root mean sequare velocity to carry out preliminary dynamic(al) correction to the pending geological data Process, obtain the common midpoint gather after preliminary dynamic(al) correction;
Common midpoint gather reordering module, for carrying out R to the whole roads in the common midpoint gather after the preliminary dynamic(al) correction Secondary rearrangement, obtains the road collection of R groups rearrangement, controls there is the time difference, R >=1 between each pair neighboring track during rearrangement;
Parameter Spectrum acquisition module, for the geological data according to the middle shortcut, is calculated similarity coefficient-normal-moveout spectrum, also uses The corresponding geological data in whole roads in common midpoint gather after according to the root mean sequare velocity and the preliminary dynamic(al) correction, It is calculated similarity coefficient-anisotropic parameters spectrum;
Normalized module, for using the M groups differential similarity coefficient operator, carrying out to initial similarity coefficient-normal-moveout spectrum Normalized, obtains normalized similarity coefficient-normal-moveout spectrum, is additionally operable to using the R groups differential similarity coefficient operator, to first Beginning similarity coefficient-anisotropic parameters spectrum is normalized, and obtains normalized similarity coefficient-anisotropic parameters spectrum;
Parameter pickup model, for picking up root mean sequare velocity from the normalized similarity coefficient-normal-moveout spectrum, is additionally operable to from institute Anisotropic parameters is picked up in stating normalized similarity coefficient-anisotropic parameters spectrum;
Data generation module, for using the root mean sequare velocity and the anisotropic parameters as the dynamic(al) correction parameter.
CN201710015203.1A 2017-01-10 2017-01-10 A kind of data processing method and device for obtaining dynamic(al) correction parameter Pending CN106547027A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201710015203.1A CN106547027A (en) 2017-01-10 2017-01-10 A kind of data processing method and device for obtaining dynamic(al) correction parameter

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201710015203.1A CN106547027A (en) 2017-01-10 2017-01-10 A kind of data processing method and device for obtaining dynamic(al) correction parameter

Publications (1)

Publication Number Publication Date
CN106547027A true CN106547027A (en) 2017-03-29

Family

ID=58396416

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201710015203.1A Pending CN106547027A (en) 2017-01-10 2017-01-10 A kind of data processing method and device for obtaining dynamic(al) correction parameter

Country Status (1)

Country Link
CN (1) CN106547027A (en)

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107957594A (en) * 2017-11-15 2018-04-24 中国石油集团东方地球物理勘探有限责任公司 The oval bearing calibration of seismic data, dynamic bearing calibration and normal-moveout spectrum computational methods

Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US5982706A (en) * 1997-03-04 1999-11-09 Atlantic Richfield Company Method and system for determining normal moveout parameters for long offset seismic survey signals
CN1797033A (en) * 2004-12-29 2006-07-05 中国石油天然气集团公司 Method for raising precision of shifted image before superposition by using root mean square velocity
CN101750628A (en) * 2008-12-11 2010-06-23 中国石油天然气股份有限公司 Two-dimensional correction method for closing error of stacking velocity and root-mean-square velocity field
CN102073064A (en) * 2009-11-25 2011-05-25 中国石油天然气集团公司 Method for improving velocity spectrum resolution by using phase information
CN101776768B (en) * 2009-01-09 2012-01-11 中国石油天然气股份有限公司 Anisotropy speed analysis and dynamic correction method

Patent Citations (5)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US5982706A (en) * 1997-03-04 1999-11-09 Atlantic Richfield Company Method and system for determining normal moveout parameters for long offset seismic survey signals
CN1797033A (en) * 2004-12-29 2006-07-05 中国石油天然气集团公司 Method for raising precision of shifted image before superposition by using root mean square velocity
CN101750628A (en) * 2008-12-11 2010-06-23 中国石油天然气股份有限公司 Two-dimensional correction method for closing error of stacking velocity and root-mean-square velocity field
CN101776768B (en) * 2009-01-09 2012-01-11 中国石油天然气股份有限公司 Anisotropy speed analysis and dynamic correction method
CN102073064A (en) * 2009-11-25 2011-05-25 中国石油天然气集团公司 Method for improving velocity spectrum resolution by using phase information

Non-Patent Citations (1)

* Cited by examiner, † Cited by third party
Title
任岩 等: "基于确定性道重排法的非双曲线走时速度及等效各向异性参数分析", 《北京大学学报(自然科学版)》 *

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107957594A (en) * 2017-11-15 2018-04-24 中国石油集团东方地球物理勘探有限责任公司 The oval bearing calibration of seismic data, dynamic bearing calibration and normal-moveout spectrum computational methods

Similar Documents

Publication Publication Date Title
CN104375188B (en) Seismic wave transmission attenuation compensation method and device
CN111164462B (en) Artificial source surface wave exploration method, surface wave exploration device and terminal equipment
CN103454686B (en) Small scale sedimentary facies based on strata slicing carries out the method and system of reservoir prediction
CN105487117B (en) A kind of 3 D seismic observation system optimization method and device
CN104155691B (en) Converted wave anisotropic velocity analysis method and device
CN105277978A (en) Method and device for determining near-ground-surface speed model
CN108318937A (en) Geologic interpretation method and apparatus
CN109188520A (en) Thin reservoir thickness prediction method and device
CN107193040A (en) The determination method and apparatus of Depth Domain synthetic seismogram
CN107390266A (en) Speed update method and pre-stack depth migration velocity modeling method based on angle gathers
CN106199704B (en) A kind of Three-dimendimal fusion submarine cable seismic data velocity modeling method
CN105093319A (en) Ground micro-seismic static correction method based on three-dimensional seismic data
CN108415073A (en) Angle domain back scattering offset imaging method and device
CN104865597A (en) Modeling method of depth domain interval velocity initial model
CN105467445B (en) The method for building up and device of a kind of 3 D seismic observation system
NO870389L (en) PROCEDURE FOR SEISMIC DATA MIGRATION.
CN106443791B (en) The method for asking for tilted stratum or anisotropic formation shear wave Value of residual static correction
CN108107471A (en) The acquisition methods and device of a kind of point of orientation first arrival data volume
CN108508481B (en) A kind of method, apparatus and system of longitudinal wave converted wave seismic data time match
CN106547027A (en) A kind of data processing method and device for obtaining dynamic(al) correction parameter
CN106054252A (en) Pre-stack time migration method and device
CN105487106B (en) A kind of benefit big gun method based on the illumination of Gaussian ray bundle target zone energy
CN106257309A (en) Post-stack seismic data body processing method and processing device
CN106842316B (en) Crack determines method and apparatus
CN106443773B (en) A kind of method and device for suppressing coal seam screen effect in seismic profile data

Legal Events

Date Code Title Description
PB01 Publication
PB01 Publication
SE01 Entry into force of request for substantive examination
SE01 Entry into force of request for substantive examination
WD01 Invention patent application deemed withdrawn after publication

Application publication date: 20170329

WD01 Invention patent application deemed withdrawn after publication