CN105242304A - Seismic data gap compensation method based on frequency-space domain wave field continuation - Google Patents

Seismic data gap compensation method based on frequency-space domain wave field continuation Download PDF

Info

Publication number
CN105242304A
CN105242304A CN201410317628.4A CN201410317628A CN105242304A CN 105242304 A CN105242304 A CN 105242304A CN 201410317628 A CN201410317628 A CN 201410317628A CN 105242304 A CN105242304 A CN 105242304A
Authority
CN
China
Prior art keywords
data
infin
wave field
seismic data
continuation
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
CN201410317628.4A
Other languages
Chinese (zh)
Inventor
韩文功
冯德永
孙成禹
李红梅
梁鸿贤
谢俊法
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 Chemical Corp
Geophysical Research Institute of Sinopec Shengli Oilfield Co
Original Assignee
China Petroleum and Chemical Corp
Geophysical Research Institute of Sinopec Shengli Oilfield Co
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 Chemical Corp, Geophysical Research Institute of Sinopec Shengli Oilfield Co filed Critical China Petroleum and Chemical Corp
Priority to CN201410317628.4A priority Critical patent/CN105242304A/en
Publication of CN105242304A publication Critical patent/CN105242304A/en
Pending legal-status Critical Current

Links

Landscapes

  • Geophysics And Detection Of Objects (AREA)

Abstract

The invention provides a seismic data gap compensation method based on frequency-space domain wave field continuation, which comprises the steps of carrying out three-dimensional Fourier transform on three-dimensional seismic data, and converting seismic data of a (x, y, z) domain into to kx-ky-f domain; carrying out continuation on the wave field of non-deletion trace seismic data according to a wave field continuation relation in a time-space domain by using spatial coherence of seismic signals, acquiring wave field information of a deletion trace, and then carrying out three-dimensional Fourier transform so as to acquire compensation data of the (x, y, z) domain. According to the invention, three-dimensional Fourier transform belongs to orthogonal transform and has good amplitude preservation performance in the kx-ky-f domain and the (x, y, z) domain, so that signals before and after changes are enabled to be consistent in energy. The method provided by the invention carries out deletion seismic data compensation through wave filed continuation, and has specific geophysical significances. Meanwhile, the seismic data gap compensation method adopts fast Fourier transform, and has high computing efficiency.

Description

Based on the seismic data gap penalties method of territory, frequency space wave field extrapolation
Technical field
The present invention relates to exploration geophysics seismic data processing technology field, is a kind of method of the wave field extrapolation relational implementation seismic data gap penalties utilized in temporal-spatial field.
Background technology
In seismic data process, seismic trace disappearance and spatial sampling deficiency are very common, and it shows as dead trace or due to the trace record disallowable in preprocessing process containing strong noise.Like this, processing procedure based on multiple tracks Processing Algorithm will be subject to the impact lacking road, wherein most affectedly comprise wave equation migration, based on the method for the suppression surface-related multiple of wave equation, the processing procedures such as the elimination of the multiple reflection relevant with earth's surface and Power estimation.
Seismic data compensation method when not re-starting seismic data acquisition, can compensate the geological data of disappearance, ensures carrying out smoothly of subsequent treatment.Seismic data compensation method conventional at present mainly contains Sinc interpolation method, f-x territory interpolation method, t-x territory predicated error filter coefficients method and the Trace Interpolation method based on Radon converter technique.Although wherein Sinc interpolation method is carrying out Trace Interpolation hourly velocity soon, be easy to realize, correctly interpolation cannot having the seismic trace of spatial aliasing.Although the t-x territory predicated error filter coefficients method of the f-x territory Trace Interpolation method of Spitz and Claerbout correctly interpolation can have the seismic trace of spatial aliasing, but these method calculated amount are large especially, its practicality in real data is reduced greatly.Trace Interpolation method based on Radon converter technique may be used for the compensation of seismic data, but the method itself is not protect width, and geological data is after Radon direct transform and Radon inverse transformation, and data have small change.
In addition multiple reflection is the multiple reflections of subsurface reflector, also stratal configuration information has been contained, under extremely complicated geologic condition, even contain the subsurface information that primary reflection does not have, be used by suitable method and can obtain more abundant geological structure information, but this method is only applicable to marine data usually, the multiple reflection of most of land seismic data agensis.
Summary of the invention
The object of the invention is the defect for prior art, propose a kind of for improving seismic imaging quality, solving in 3-d seismic exploration causes seismic trace to lack because instrument failure or surface conditions affect, and causes the seismic data gap penalties method based on the wave field extrapolation of territory, frequency space of subsequent treatment difficulty.
Object of the present invention realizes by following technical measures:
(1) three-dimensional Fourier transform is carried out to 3D seismic data, (x, y, t) territory geological data is transformed into k x-k y-f territory;
(2) utilize the spatial coherence of seismic signal, according to the wave field extrapolation relation in temporal-spatial field, continuation is carried out to the wave field of non-disappearance road geological data, obtain the wave field information lacking road;
(3) carry out three-dimensional Fourier inversion, obtain the offset data in (x, y, t) territory.
Technical scheme of the present invention is optimized for further:
(1) three-dimensional Fourier transform is carried out to the 3D seismic data of input, (x, y, t) territory geological data is transformed into k x-k y-f territory, transformation for mula is;
A ( k x , k y , f ) = ∫ - ∞ ∞ dx ∫ - ∞ ∞ dy ∫ - ∞ ∞ u ( x , y , t ) e - i 2 π [ ft - ( k x x + k y y ) ] dt .
Wherein u (x, y, t) is the 3D seismic data of input, and prestack compensates can use various roads collection data, but usually selects common offset effect data better; Poststack compensates and is superposition of data; A (k x, k y, f) be the frequency space numeric field data after conversion.
(2) utilize the spatial coherence of seismic signal, according to the wave field extrapolation relation in temporal-spatial field, carry out continuation to the wave field of non-disappearance road geological data, continuation formula is:
A ( k ′ x , k ′ y , ω ) = A ( k x , k y , ω ) e i 2 π ( k x x 0 + k y y 0 ) ]
Wherein A (k' x, k' y, ω) for continuation obtain at (x+x 0, y+y 0) the frequency space numeric field data at place.
(3) carry out three-dimensional Fourier inversion, obtain the offset data in (x, y, t) territory, transformation for mula is.
u ( x + x 0 , y + y 0 , t ) = ∫ - ∞ ∞ dk ′ x ∫ - ∞ ∞ dk ′ y ∫ - ∞ ∞ A ( k ′ x , k ′ y , ω ) e i 2 π [ ωt - ( k ′ x x + k ′ y y ) ] df
Wherein u (x+x 0, y+y 0, t) for continuation obtain at (x+x 0, y+y 0) place disappearance data.
Consider the scrambling that in three dimensions, seismic trace lacks in different directions, after considering three-dismensional effect, the actual seismic trace compensated should be:
u ~ ( x + x 0 , y + y 0 , t ) = ∫ B ( x 0 , y 0 ) u ( x + x 0 , y + y 0 , t ) d x 0 d y 0
Wherein B (x 0, y 0) be direction factor, its orientation with each road and the number of channels at every turn compensated relevant, the energy match factor between Ye Shi road. actual in (x+x for considering after three-dismensional effect 0, y+y 0) place compensate data.
The present invention is by seismic data gap penalties, and encryption space sampling frequency, effectively can prevent from alias appears in migrated section, improve signal to noise ratio (S/N ratio) simultaneously, for the process of latter earthquake data and explanation provide strong technical support; The present invention simultaneously well solves in 3-d seismic exploration, because instrument failure or surface conditions impact cause seismic trace to lack, cause the problem (as alias appears in imaging section, lateral resolution variation etc.) of subsequent treatment difficulty, and then improve seismic imaging quality.
Accompanying drawing explanation
Fig. 1 is the process flow diagram of a kind of exemplary embodiments of the present invention;
Fig. 2 is the raw data that track pitch is too large;
Fig. 3 is the frequency wavenumber spectrum of corresponding diagram 2;
Fig. 4 is through the frequency wavenumber spectrum after wave field extrapolation;
Data after Tu5Shi Ge road compensates;
Fig. 6 is vertical survey line number is section before the compensation of 3933;
Fig. 7 is vertical survey line number is section after the compensation of 3933;
The horizontal survey line of Fig. 8 number is section before the compensation of 1290;
The horizontal survey line of Fig. 9 number is section after the compensation of 1290;
Figure 10 compensates front 600ms time slice;
Figure 11 compensates rear 600ms time slice.
Embodiment
For making above and other object of the present invention, feature and advantage can become apparent, cited below particularly go out preferred embodiment, and coordinate institute's accompanying drawings, be described in detail below.
As shown in Figure 1, Fig. 1 is the process flow diagram of the seismic data gap penalties method based on the wave field extrapolation of territory, frequency space of the present invention.
In step 101, input three-dimensional data to be compensated, prestack compensates can use various roads collection data, but usually selects common offset effect data better; Poststack compensates and is superposition of data.Owing to have employed Fourier transform, therefore must according to uniform geophone offset grid arrangement.If geophone offset is uneven in input data, first regularization process should be carried out by trace interpolation technology.Then flow process enters into step 102.
In step 102, three-dimensional data is transformed into territory, frequency space, flow process enters into step 103.
In step 103, utilize the spatial coherence of seismic signal, according to the wave field extrapolation relation in temporal-spatial field, carry out continuation to the wave field of non-disappearance road geological data, obtain the wave field information lacking road, flow process enters into step 104.
In step 104, carry out three-dimensional Fourier inversion, frequency space numeric field data is transformed into time domain, and flow process enters into step 105.
In step 105, the output of data, only can export offset data as required, also raw data can be exported together with offset data.
By above flow process, can effective compensation disappearance geological data.Fig. 2 utilizes the big gun record of just drilling means and obtaining, and its track pitch is too large, needs to carry out compensating every road; Fig. 3 is the frequency wavenumber spectrum of corresponding diagram 2.By wave field extrapolation, obtain the frequency wavenumber spectrum after continuation (shown in Fig. 4), then convert back time domain, the data after being compensated.Data after compensation, compensation effect is better.
Fig. 6-Figure 11 is the embodiment of real data, Fig. 6 and Fig. 7 is vertical survey line number is section section rear with compensation before the compensation of 3933; Fig. 8 and Fig. 9 is horizontal survey line number is section section rear with compensation before the compensation of 1290; Can find out that from section gap portions is compensated, lineups continuously and maintain relative energy relationships.Figure 10 and Figure 11 is the 600ms time slice before compensating and after compensating, and also can find out to have good compensation effect.Just drilling data and real data all to demonstrate the present invention there is good compensation effect.

Claims (3)

1., based on the seismic data gap penalties method of territory, frequency space wave field extrapolation, it is characterized in that comprising:
(1) three-dimensional Fourier transform is carried out to 3D seismic data, (x, y, t) territory geological data is transformed into k x-k y-f territory;
(2) utilize the spatial coherence of seismic signal, according to the wave field extrapolation relation in temporal-spatial field, continuation is carried out to the wave field of non-disappearance road geological data, obtain the wave field information lacking road;
(3) carry out three-dimensional Fourier inversion, obtain the offset data in (x, y, t) territory.
2. the seismic data gap penalties method based on the wave field extrapolation of territory, frequency space according to claim 1, is characterized in that:
(1) to the transformation for mula that the 3D seismic data of input carries out three-dimensional Fourier transform be
A ( k x , k y , f ) = ∫ - ∞ ∞ dx ∫ - ∞ ∞ dy ∫ - ∞ ∞ u ( x , y , t ) e - i 2 π [ ft - ( k x x + k y y ) ] dt
Wherein u (x, y, t) is the 3D seismic data of input, A (k x, k y, f) be the frequency space numeric field data after conversion;
(2) carry out continuation to the wave field of non-disappearance road geological data, continuation formula is
A ( k ′ x , k ′ y , ω ) = A ( k x , k y , ω ) e i 2 π ( k x x 0 + k y y 0 ) ]
Wherein A (k' x, k' y, ω) for continuation obtain at (x+x 0, y+y 0) the frequency space numeric field data at place.
(3) transformation for mula carrying out three-dimensional Fourier inversion is
u ( x + x 0 , y + y 0 , t ) = ∫ - ∞ ∞ dk ′ x ∫ - ∞ ∞ dk ′ y ∫ - ∞ ∞ A ( k ′ x , k ′ y , ω ) e i 2 π [ ωt - ( k ′ x x + k ′ y y ) ] df
Wherein u (x+x 0, y+y 0, t) for continuation obtain at (x+x 0, y+y 0) place disappearance data.
3. the seismic data gap penalties method based on the wave field extrapolation of territory, frequency space according to claim 1 and 2, is characterized in that also comprising in above-mentioned steps:
After three-dismensional effect, the actual seismic trace compensated should be
u ~ ( x + x 0 , y + y 0 , t ) = ∫ B ( x 0 , y 0 ) u ( x + x 0 , y + y 0 , t ) d x 0 d y 0
Wherein B (x 0, y 0) be direction factor, for actual in (x+x after three-dismensional effect 0, y+y 0) place compensate data.
CN201410317628.4A 2014-07-04 2014-07-04 Seismic data gap compensation method based on frequency-space domain wave field continuation Pending CN105242304A (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201410317628.4A CN105242304A (en) 2014-07-04 2014-07-04 Seismic data gap compensation method based on frequency-space domain wave field continuation

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201410317628.4A CN105242304A (en) 2014-07-04 2014-07-04 Seismic data gap compensation method based on frequency-space domain wave field continuation

Publications (1)

Publication Number Publication Date
CN105242304A true CN105242304A (en) 2016-01-13

Family

ID=55040004

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201410317628.4A Pending CN105242304A (en) 2014-07-04 2014-07-04 Seismic data gap compensation method based on frequency-space domain wave field continuation

Country Status (1)

Country Link
CN (1) CN105242304A (en)

Cited By (1)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107607946A (en) * 2017-07-24 2018-01-19 湖北工业大学 The three-dimensional bright temperature inversion method of uniform sampling synthetic aperture radiometer

Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102109612A (en) * 2009-12-23 2011-06-29 中国石油天然气集团公司 Seismic wave absorption and attenuation compensation method
CN102269822A (en) * 2010-06-02 2011-12-07 中国石油天然气集团公司 Mixed stratigraphic absorption compensation method
WO2011110917A3 (en) * 2010-03-11 2012-02-16 Geco Technology B.V. Processing geophysical data
CN103364825A (en) * 2012-03-28 2013-10-23 中国石油化工股份有限公司 Three-dimensional Fourier transform amplitude-preserving pre-stack channel interpolation method
CN103901469A (en) * 2014-03-18 2014-07-02 中国石油集团川庆钻探工程有限公司地球物理勘探公司 Seismic data recovery method
CN103901466A (en) * 2012-12-28 2014-07-02 中国石油天然气集团公司 Three-dimensional seismic data interpolation method

Patent Citations (6)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN102109612A (en) * 2009-12-23 2011-06-29 中国石油天然气集团公司 Seismic wave absorption and attenuation compensation method
WO2011110917A3 (en) * 2010-03-11 2012-02-16 Geco Technology B.V. Processing geophysical data
CN102269822A (en) * 2010-06-02 2011-12-07 中国石油天然气集团公司 Mixed stratigraphic absorption compensation method
CN103364825A (en) * 2012-03-28 2013-10-23 中国石油化工股份有限公司 Three-dimensional Fourier transform amplitude-preserving pre-stack channel interpolation method
CN103901466A (en) * 2012-12-28 2014-07-02 中国石油天然气集团公司 Three-dimensional seismic data interpolation method
CN103901469A (en) * 2014-03-18 2014-07-02 中国石油集团川庆钻探工程有限公司地球物理勘探公司 Seismic data recovery method

Non-Patent Citations (3)

* Cited by examiner, † Cited by third party
Title
张军华等: "在f-k域实现三维波场道内插", 《石油地球物理勘探》 *
张文颖: "保幅性三维傅里叶变换叠前道内插技术研究", 《中国优秀硕士学位论文全文数据库 基础科学辑》 *
王金龙等: "三维锥形滤波方法研究及应用", 《石油地球物理勘探》 *

Cited By (2)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN107607946A (en) * 2017-07-24 2018-01-19 湖北工业大学 The three-dimensional bright temperature inversion method of uniform sampling synthetic aperture radiometer
CN107607946B (en) * 2017-07-24 2020-03-17 湖北工业大学 Three-dimensional uniform sampling synthetic aperture radiometer brightness temperature inversion method

Similar Documents

Publication Publication Date Title
Hennenfent et al. Nonequispaced curvelet transform for seismic data reconstruction: A sparsity-promoting approach
Duquet et al. Kirchhoff modeling, inversion for reflectivity, and subsurface illumination
de Ridder et al. Ambient seismic noise eikonal tomography for near-surface imaging at Valhall
CN108037526A (en) Reverse-time migration method based on all-wave wave field VSP/RVSP seismic datas
EP3529640B1 (en) Generating subterranean imaging data based on vertical seismic profile data and ocean bottom sensor data
WO2015160652A1 (en) Generating subterranean imaging data based on vertical seismic profile data
US11754744B2 (en) Surface wave prospecting method for jointly extracting Rayleigh wave frequency dispersion characteristics by seismoelectric field
CN113805237B (en) Method and system for offset land crossrange seismic using compressed sensing models
CN104570116A (en) Geological marker bed-based time difference analyzing and correcting method
CN111257939B (en) Time-lapse seismic virtual source bidirectional wave field reconstruction method and system
Wang et al. High-resolution wave-equation AVA imaging: Algorithm and tests with a data set from the Western Canadian Sedimentary Basin
Jones et al. Full waveform inversion in a complex geological setting-a narrow azimuth towed streamer case study from the Barents Sea
Zhang et al. Interval Q inversion based on zero-offset VSP data and applications
Fu et al. Imaging the ice sheet and uppermost crustal structures with a dense linear seismic array in the Larsemann Hills, Prydz Bay, East Antarctica
CN105242304A (en) Seismic data gap compensation method based on frequency-space domain wave field continuation
Zhou et al. High angle prestack depth migration with absorption compensation
Giustiniani et al. P and S reflection and P refraction: An integration for characterising shallow subsurface
Gu et al. Passive Seismic Structure Imaging of a Coal Mine by Ambient Noise Seismic Interferometry on a Dense Array
Zhang et al. Near-surface bedrock profiling using urban ambient noise: An autocorrelation approach
Cai et al. Passive multiple reverse time migration imaging based on wave decomposition and normalized imaging conditions
Yang et al. Joint reverse-time imaging condition of seismic towed-streamer and OBN data
Chen et al. Research on vertical cable seismic interferometry imaging
Askari et al. Estimation of near surface shear wave velocity using CMP cross-correlation of surface waves (CCSW)
Wang et al. The method of interbed multiple suppression and application in fault identification
Wu et al. Ambient noise surface wave tomography of Quaternary structures derived from a high-density array in the central Hebei Depression, North China

Legal Events

Date Code Title Description
C06 Publication
PB01 Publication
C10 Entry into substantive examination
SE01 Entry into force of request for substantive examination
RJ01 Rejection of invention patent application after publication
RJ01 Rejection of invention patent application after publication

Application publication date: 20160113