CN102692651A - Preliminary wave residual static correction method with space-variant velocity - Google Patents

Preliminary wave residual static correction method with space-variant velocity Download PDF

Info

Publication number
CN102692651A
CN102692651A CN2011100712286A CN201110071228A CN102692651A CN 102692651 A CN102692651 A CN 102692651A CN 2011100712286 A CN2011100712286 A CN 2011100712286A CN 201110071228 A CN201110071228 A CN 201110071228A CN 102692651 A CN102692651 A CN 102692651A
Authority
CN
China
Prior art keywords
arrival
static correction
data
speed
break time
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
CN2011100712286A
Other languages
Chinese (zh)
Inventor
刘超颖
杜书奎
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.)
BGP Inc
Original Assignee
BGP Inc
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 BGP Inc filed Critical BGP Inc
Priority to CN2011100712286A priority Critical patent/CN102692651A/en
Publication of CN102692651A publication Critical patent/CN102692651A/en
Pending legal-status Critical Current

Links

Images

Landscapes

  • Geophysics And Detection Of Objects (AREA)

Abstract

The present invention provides a preliminary wave residual static correction method with space-variant velocity. A linear correction and first-break picking are carried out on a single shot, data recorded in a preliminary wave is selected to a common midpoint gather area, according to a sequence of a line number and a common midpoint gather number and a line interval parameter, linear speed fitting is carried out according to a first break time of common midpoint gather, a speed analysis point velocity is obtained, space-variant linear velocity correction is carried out, residual static correction values of a shot point and a receiving point are solved on a corrected first break time, and static correction is carried out. The method can be applied to conditions that a data signal-to-noise ratio is poor, the first break time is not easy to acquire, and there is no reliable refractive layer data, the efficiency of the method is higher than that of a conventional refractive wave, tomographic static correction efficiency is high, a lot of time can be saved, an anti-noise capacity is strong, an application effect is stable, and the use of the method is convenient.

Description

The primary wave residual static corrections of speed space-variant
Technical field
The present invention relates to the geophysical survey seismic data processing technique, belong to the technological category of static correction in the seismic data processing procedure, is a kind of primary wave residual static corrections of speed space-variant specifically.
Background technology
Need be in the land earthquake data acquisition to the seismic data static corrections processing, present conventional first arrival refraction static correction method is at the enterprising line linearity correction of original single big gun, carries out first arrival then and picks up, first break time is charged to trace header, exports a first arrival file simultaneously.The first break time file has been arranged, just can carry out conventional first arrival refraction static correction, conventional first arrival refraction static correction generally is refractive wave static correction or chromatography static correction; For refractive wave static correction; The first break time from same refractor is picked up in requirement on the big gun collection, when directly calculating high-velocity bed speed and postponing according to refraction first break time and refraction wave whilst on tour formula, this method requires relatively harshness; Requirement has refraction wave; First arrival is picked up easily, and for complicated earth surface low signal-to-noise ratio data situation, this requirement is difficult to satisfy.For the chromatography static correction, except picking up accurate first break time, the more important thing is operational efficiency problem and inversion accuracy problem.
Especially by land in the earthquake data acquisition; Owing to reasons such as face of land complicacy and subsurface geologic structures, the geological data signal to noise ratio (S/N ratio) of collection is extremely low, and particularly the top layer lateral speed change is big; Cause first arrival complicated; Unstable refraction, a little less than reflected signal also reached, conventional first arrival refraction static correction method missed one's aim.
Summary of the invention
The object of the invention provides the primary wave residual static corrections of the speed space-variant that a kind of convenience is simple and direct, precision is high.
The present invention realizes through following steps:
1) acquiring seismic data carries out data analysis to original single big gun data, and affirmation need be done first arrival refraction static correction;
The described data analysis of step 1) is that original single big gun data and face of land elevation are together shown, analyzes the corresponding relation of elevation and first break time, and elevation change is big; The big data of face of land speed horizontal change; First arrival just changes greatly, and signal to noise ratio (S/N ratio) is low, need do first arrival refraction static correction.
2) pick up in the enterprising line linearity correction of single big gun, first arrival, will pick up the result and charge to trace header, keep the geological data that note has first break time;
Step 2) to pick up be to provide a fixing linear speed linearity correction is carried out in first arrival for described correction and first arrival, distributes according near the noise the first arrival and confirm the mode that first arrival is picked up.
The mode that described first arrival is picked up is that noise ratio is less before first arrival, and the primary wave energy is strong, selects the mode of picking up in batches; When noise is big, a little less than the primary wave energy, first arrival is unclear, picks up through interactive means.
3) be sorted into the CMP gather territory to the data of charging to the primary wave time, order and line spacing parameter by wire size and CMP gather number obtain CMP road collection;
The described CMP gather of step 3) is a big bin road collection.
4) do the linear speed match according to the first break time on the CMP gather, obtain the velocity analysis spot speed;
Described the picking up in the enterprising line speed match of first break time of step 4) is to choose straight line wantonly at the first arrival position of data; The method of employing fitting a straight line is obtained the linear speed of straight line; Carry out mutual linearity correction then, if smoothing, the speed of preserving each space-variant point.
5) to step 2) keep and remember that the geological data that first break time is arranged carries out the space-variant linear speed and proofreaies and correct;
The described space-variant linear speed of step 5) school is to proofread and correct with linear speed updating formula X/V, and X is an offset distance in the formula, and V is the space-variant spot speed after the match of step 4) speed.
6) first break time of carrying out after the space-variant linear speed is proofreaied and correct is found the solution the residual static correction amount of shot point and acceptance point with Gauss-Sai Deer alternative manner;
The residual static correction amount that step 6) is found the solution shot point and acceptance point adopts following method:
First break time is: T ' Ijk=S i+ R j+ G k+ K kX Ij
S wherein iBe the static correction value of i shot point, R jBe the static correction value of j acceptance point, G kBeing the structure item value of k CMP, is the DC component of static correction value in the CMP road collection, K kIt is the residue linear speed of k CMP; Utilize least square method to find the solution this equation, the travel-times of seismic first breaks T that is picked up then IjkWith model whilst on tour T ' IjkBetween the quadratic sum of difference minimum, obtain shot point and acceptance point residual static correction amount through iteration.
7) use shot point and the acceptance point residual static correction amount obtained of step raw data is carried out static correction.
The present invention is applicable to the data poor signal to noise, and first break time is difficult for picking up, and does not have under the reliable refractor data conditions, and big like surface relief, lateral speed change is big, and static correction value is asked for the place of difficulty.The conventional refraction wave of efficiency ratio of the present invention, chromatography static correction efficient is high, can save the plenty of time, and anti-noise ability is strong, and effect is stable, and is easy to use.
Description of drawings
Fig. 1 is original single big gun and elevation curve display;
Fig. 2 is the single big gun that has first break time;
Fig. 3 is the linear speed analysis site location drawing;
Fig. 4 is that linear speed is picked up;
Fig. 5 is the linear speed correction test;
Fig. 6 is that the single big gun after the static correction shows.
Embodiment
Specify the present invention below in conjunction with accompanying drawing.
1) acquiring seismic data carries out data analysis to original single big gun data, and affirmation need be done first arrival refraction static correction;
Data shown in Figure 1 are that original single big gun data and face of land elevation (top curve) are together shown; Through analyzing the corresponding relation of elevation and first break time; The discovery elevation change is big, and the discrepancy in elevation reaches the big data of 200 meter indicated airspeed degree horizontal change, and first arrival just changes greatly; Signal to noise ratio (S/N ratio) is low, need do first arrival refraction static correction.
2) pick up in the enterprising line linearity correction of single big gun, first arrival, will pick up the result and charge to trace header, keep the geological data that note has first break time, the first break time that first arrival is picked up is so long as primary wave gets final product, and it is to select according to the data situation that first arrival is picked up, as:
Noise ratio is less before the first arrival of Fig. 1, and the primary wave energy is strong, so select the mode of picking up in batches.
Fig. 2 is the result who picks up in batches, and what the figure mid point was represented is first break time, and first break time is charged in the trace header.
The first arrival program of picking up provides a fixing linear speed linearity correction is carried out in first arrival, selects the first arrival pick-up method according near the noise distribution situation the first arrival, if noise ratio is less before the first arrival, the primary wave energy is strong, selects to pick up in batches to get final product.
3) be sorted into the CMP gather territory to single big gun data of charging to the primary wave time, order and line spacing parameter by wire size and CMP gather number obtain common midpoint (CMP) road collection;
Position shown in Fig. 3 intersection point is the CMP gather position.Order by wire size and CMP number is read in, and the line spacing parameter and the CMP spacing parameter that provide according to the user carry out sorting, can obtain the CMP road collection that needs.Described CMP road collection is a big bin road collection.
4) do the linear speed match according to the first break time on the CMP gather, obtain each analysis site speed.
In the enterprising line speed match of first break time is optional straight line at the first arrival position of data, and the method for employing fitting a straight line is obtained the linear speed of straight line, carries out mutual linearity correction then, if smoothing, the speed of preserving each space-variant point.
5) to step 2) geological data that keeps note and have first break time puts linear speed with space-variant and proofreaies and correct the speed linear interpolation between the space-variant point.Like Fig. 4, Fig. 5.
It is to proofread and correct with linear speed updating formula X/V that the described space-variant linear speed of step 5) is proofreaied and correct, and X is an offset distance in the formula, and V is the space-variant spot speed after the match of step 4) speed.
The step 4) linear speed not is that all data are carried out the linear speed analysis when analyzing, but on the given road collection of user, carries out, and this step will be carried out linearity correction to all data, as the input in the 6th step.
6) first break time of carrying out after the space-variant linear speed is proofreaied and correct is found the solution the residual static correction amount of shot point and acceptance point with Gauss-Sai Deer alternative manner;
The residual static correction amount that step 6) is found the solution shot point and acceptance point adopts following method:
First break time is: T ' Ijk=S i+ R j+ G k+ K kX Ij
S wherein iBe the static correction value of i shot point, R jBe the static correction value of j acceptance point, G kBeing the structure item value of k CMP, is the DC component of static correction value in the CMP road collection, K kIt is the residue linear speed of k CMP; Utilize least square method to find the solution this equation, the travel-times of seismic first breaks T that is picked up then IjkWith model whilst on tour T ' IjkBetween the quadratic sum of difference minimum, obtain shot point and acceptance point residual static correction amount through iteration.
Least square method is found the solution this equation process:
E = Σ ijk ( T ijk ′ - T ijk ) 2 → Min
Respectively to S i, R j, G k, K kAsk local derviation
∂ E ∂ S = ∂ E ∂ R = ∂ E ∂ G = ∂ E ∂ K = 0
Can be write following formula as following form:
G k ( v ) = Σ i , j , k { T ijk - S i ( v - 1 ) - R j ( v - 1 ) - K i ( v - 1 ) X ij } N k
K k ( v ) = Σ i , j , k { T ijk - S i ( v - 1 ) - R j ( v - 1 ) - G k ( v ) } * X ij N i Σ X ij 2
S i ( v ) = Σ j , k , i { T ijh - R j ( v - 1 ) - G k ( v ) - K i ( v ) X ij } N i
R j ( v ) = Σ i , k , j { T ijh - S i ( v ) - G k ( v ) - K i ( v ) X ij } N j
Wherein (v) being the v time iteration result, (v-1) is the v-1 time iteration result, i.e. the v time last iteration result.
7) use shot point and the acceptance point residual static correction amount obtained of step original shot gather data is carried out static correction.
The present invention is applicable to the data poor signal to noise, and first break time is difficult for picking up, and does not have under the reliable refractor data conditions, and big like surface relief, lateral speed change is big, and static correction value is asked for the place of difficulty.With Fig. 1 contrast, Fig. 6 static correction effect is fine.
The conventional refraction wave of efficiency ratio of the present invention, chromatography static correction efficient is high, can save the plenty of time.The present invention adopts main road collection match first arrival speed, and anti-noise ability is strong, and effect is stable, and is easy to use.

Claims (8)

1. the primary wave residual static corrections of a speed space-variant, characteristics are to realize through following steps:
1) acquiring seismic data carries out data analysis to original single big gun data, and affirmation need be done first arrival refraction static correction;
2) pick up in the enterprising line linearity correction of single big gun, first arrival, will pick up the result and charge to trace header, keep the geological data that note has first break time;
3) be sorted into the CMP gather territory to the data of charging to the primary wave time, order and line spacing parameter by wire size and CMP gather number obtain CMP road collection;
4) do the linear speed match according to the first break time on the CMP gather, obtain the velocity analysis spot speed;
5) to step 2) keep and remember that the geological data that first break time is arranged carries out the space-variant linear speed and proofreaies and correct;
6) first break time of carrying out after the space-variant linear speed is proofreaied and correct is found the solution the residual static correction amount of shot point and acceptance point with Gauss-Sai Deer alternative manner;
7) use shot point and the acceptance point residual static correction amount obtained of step raw data is carried out static correction.
2. method according to claim 1; Characteristics are that the described data analysis of step 1) is that original single big gun data and face of land elevation are together shown, analyze the corresponding relation of elevation and first break time, and elevation change is big; The big data of face of land speed horizontal change; First arrival just changes greatly, and signal to noise ratio (S/N ratio) is low, need do first arrival refraction static correction.
3. method according to claim 1, characteristics are steps 2) described correction and first arrival are picked up is to provide a fixing linear speed linearity correction is carried out in first arrival, and distribute according near the noise the first arrival and confirm the mode that first arrival is picked up.
4. method according to claim 3, characteristics are that the mode that described first arrival is picked up is that noise ratio is less before first arrival, and the primary wave energy is strong, selects the mode of picking up in batches; When noise is big, a little less than the primary wave energy, first arrival is unclear, picks up through interactive means.
5. method according to claim 1, characteristics are that the described CMP gather of step 3) is a big bin road collection.
6. method according to claim 1; Characteristics are that described the picking up in the enterprising line speed match of first break time of step 4) is to choose straight line wantonly at the first arrival position of data; The method of employing fitting a straight line is obtained the linear speed of straight line; Carry out mutual linearity correction then, if smoothing, the speed of preserving each space-variant point.
7. method according to claim 1, characteristics are that the described space-variant linear speed correction of step 5) is to proofread and correct with linear speed updating formula X/V, and X is an offset distance in the formula, and V is the space-variant spot speed after the match of step 4) speed.
8. method according to claim 1, characteristics are that the residual static correction amount that step 6) is found the solution shot point and acceptance point adopts following method:
First break time is: T ' Ijk=S i+ R j+ G k+ K kX Ij
S wherein iBe the static correction value of i shot point, R jBe the static correction value of j acceptance point, G kBeing the structure item value of k CMP, is the DC component of static correction value in the CMP road collection, K kIt is the residue linear speed of k CMP; Utilize least square method to find the solution this equation, the travel-times of seismic first breaks T that is picked up then IjkWith model whilst on tour T ' IjkBetween the quadratic sum of difference minimum, obtain shot point and acceptance point residual static correction amount through iteration.
CN2011100712286A 2011-03-24 2011-03-24 Preliminary wave residual static correction method with space-variant velocity Pending CN102692651A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN2011100712286A CN102692651A (en) 2011-03-24 2011-03-24 Preliminary wave residual static correction method with space-variant velocity

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN2011100712286A CN102692651A (en) 2011-03-24 2011-03-24 Preliminary wave residual static correction method with space-variant velocity

Publications (1)

Publication Number Publication Date
CN102692651A true CN102692651A (en) 2012-09-26

Family

ID=46858229

Family Applications (1)

Application Number Title Priority Date Filing Date
CN2011100712286A Pending CN102692651A (en) 2011-03-24 2011-03-24 Preliminary wave residual static correction method with space-variant velocity

Country Status (1)

Country Link
CN (1) CN102692651A (en)

Cited By (7)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN103499836A (en) * 2013-07-18 2014-01-08 中国石油集团西北地质研究所 High-precision residual static correction method with combination between space variation and a plurality of time windows
CN103728666A (en) * 2012-10-16 2014-04-16 中国石油化工股份有限公司 Method for determining replacement speed of static correction middle reference plane
CN105093324A (en) * 2014-05-21 2015-11-25 中国石油化工股份有限公司 Residual static correction method
CN107219554A (en) * 2017-05-05 2017-09-29 北京大学 The automatic obtaining method of the Value of residual static correction of land seismic data
CN111624655A (en) * 2019-02-27 2020-09-04 中国石油天然气集团有限公司 Method and device for determining residual static correction value of first-motion wave
CN112394413A (en) * 2020-11-02 2021-02-23 中国石油天然气集团有限公司 Three-dimensional first-motion wave residual static correction method and device
CN112666606A (en) * 2019-10-15 2021-04-16 中国石油天然气集团有限公司 Method and device for determining anisotropic speed of near-surface azimuth

Non-Patent Citations (1)

* Cited by examiner, † Cited by third party
Title
陈启元等: "复杂山区的静校正方法探讨", 《石油物探》 *

Cited By (10)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN103728666A (en) * 2012-10-16 2014-04-16 中国石油化工股份有限公司 Method for determining replacement speed of static correction middle reference plane
CN103499836A (en) * 2013-07-18 2014-01-08 中国石油集团西北地质研究所 High-precision residual static correction method with combination between space variation and a plurality of time windows
CN103499836B (en) * 2013-07-18 2016-04-06 中国石油集团西北地质研究所 Space-variant-window fusion of many times high precision residual static corrections
CN105093324A (en) * 2014-05-21 2015-11-25 中国石油化工股份有限公司 Residual static correction method
CN105093324B (en) * 2014-05-21 2017-06-16 中国石油化工股份有限公司 A kind of residual static corrections
CN107219554A (en) * 2017-05-05 2017-09-29 北京大学 The automatic obtaining method of the Value of residual static correction of land seismic data
CN111624655A (en) * 2019-02-27 2020-09-04 中国石油天然气集团有限公司 Method and device for determining residual static correction value of first-motion wave
CN112666606A (en) * 2019-10-15 2021-04-16 中国石油天然气集团有限公司 Method and device for determining anisotropic speed of near-surface azimuth
CN112394413A (en) * 2020-11-02 2021-02-23 中国石油天然气集团有限公司 Three-dimensional first-motion wave residual static correction method and device
CN112394413B (en) * 2020-11-02 2024-07-26 中国石油天然气集团有限公司 Three-dimensional first-arrival wave residual static correction method and device

Similar Documents

Publication Publication Date Title
CN104570125B (en) Method for improving imaging speed model precision by using well data
CN102692651A (en) Preliminary wave residual static correction method with space-variant velocity
CN102540250B (en) Azimuth fidelity angle domain imaging-based fractured oil and gas reservoir seismic exploration method
CN105607124B (en) Seismic wave near surface interval quality factors compensation method and device
CN102901985B (en) A kind of Depth Domain interval velocity modification method being applicable to relief surface
CN102112894A (en) Estimation of soil properties using waveforms of seismic surface waves
CN102841375A (en) Method for tomography velocity inversion based on angle domain common imaging gathers under complicated condition
CN101598811A (en) A kind of method of calculating shot-static correction for two-dimensional vertical seismic section data
CN101561512A (en) Multi-scale crosshole SIRT tomography method
CN101520516A (en) Method for pre-stack like-two-dimensional transform of three-dimensional seismic record
CN102073067A (en) Method for increasing automatic pickup efficiency of geological data first-motion waves
CN104570076A (en) Automatic seismic wave first-arrival picking method based on dichotomy
CN104142518A (en) Method for analyzing pre-stack time migration response of seismological observation system
CN102053260B (en) Method for acquiring azimuth velocity of primary wave and method for processing earthquake data
CN104932021A (en) Constrained tomography speed modeling method based on reverse ray tracing
CN109765615A (en) Stratum quality factor inversion method and device
CN101201409A (en) Method for revising temblor data phase-conversion bit
CN107678057A (en) Determined in 3-D seismics or optimize wave detector or equipment investment amount and the method for arrangement
CN105093319A (en) Ground micro-seismic static correction method based on three-dimensional seismic data
CN102053262B (en) Method for acquiring azimuth velocity of seismic converted wave and method for processing seismic data
CN104570116A (en) Geological marker bed-based time difference analyzing and correcting method
Godfrey et al. Shear-wave velocity structure of the Tongariro Volcanic Centre, New Zealand: fast Rayleigh and slow Love waves indicate strong shallow anisotropy
CN103576197A (en) Method for extracting converted wave angle channel set
CN104133244B (en) A kind of near surface static corrections processing method of focus shear wave exploration
CN101609163B (en) Multi-scale seismic data joint imaging method based on fluctuation theory

Legal Events

Date Code Title Description
C06 Publication
PB01 Publication
C10 Entry into substantive examination
SE01 Entry into force of request for substantive examination
C02 Deemed withdrawal of patent application after publication (patent law 2001)
WD01 Invention patent application deemed withdrawn after publication

Application publication date: 20120926