CN109444959A - Full range high-precision interval velocity field method for building up - Google Patents

Full range high-precision interval velocity field method for building up Download PDF

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CN109444959A
CN109444959A CN201811296463.1A CN201811296463A CN109444959A CN 109444959 A CN109444959 A CN 109444959A CN 201811296463 A CN201811296463 A CN 201811296463A CN 109444959 A CN109444959 A CN 109444959A
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velocity
crp
speed
inversion
full range
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CN109444959B (en
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明治良
刘义
左玉
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Cogis Petroleum Technology Consulting (beijing) Co Ltd
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Cogis Petroleum Technology Consulting (beijing) Co Ltd
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    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V1/00Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/28Processing seismic data, e.g. for interpretation or for event detection
    • G01V1/30Analysis
    • G01V1/303Analysis for determining velocity profiles or travel times
    • GPHYSICS
    • G01MEASURING; TESTING
    • G01VGEOPHYSICS; GRAVITATIONAL MEASUREMENTS; DETECTING MASSES OR OBJECTS; TAGS
    • G01V2210/00Details of seismic processing or analysis
    • G01V2210/60Analysis
    • G01V2210/62Physical property of subsurface
    • G01V2210/622Velocity, density or impedance
    • G01V2210/6222Velocity; travel time

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  • Remote Sensing (AREA)
  • Physics & Mathematics (AREA)
  • Life Sciences & Earth Sciences (AREA)
  • Acoustics & Sound (AREA)
  • Environmental & Geological Engineering (AREA)
  • Geology (AREA)
  • General Life Sciences & Earth Sciences (AREA)
  • General Physics & Mathematics (AREA)
  • Geophysics (AREA)
  • Geophysics And Detection Of Objects (AREA)

Abstract

The present invention discloses full range high-precision interval velocity field method for building up, comprising: S1, basin grade compacting trend establish ultralow frequency speed trend;S2, CRP trace gather optimization processing;S3, fine grid residual velocity analysis;S4, the root mean sequare velocity of close CRP grid and residual mean square root speed are merged, dynamic correction is carried out to CRP trace gather with the speed, obtains evening up seismic channel set, speed progress DIX is converted to interval velocity after correcting;S5, seismic channel set progress partial stack will be evened up, and will obtain partial stack trace gather, carries out pre-stack elastic inversion;S6, carried out using a point lithology probability volume constraint and divide lithology velocity inversion and porosity inversion, form medium-high frequency section Interval Velocity Inversion data volume;S7, frequency dividing velocity field merge, the full range high-precision interval velocity field after being optimized.The present invention can meet the needs of subsequent conventional configurations, construct time and depth transfer, reservoir inversion by a narrow margin, track the geological researches such as prediction of formation pressure with brill geology very well.

Description

Full range high-precision interval velocity field method for building up
Technical field
The invention belongs to petroleum exploration domains, and in particular to full range high-precision interval velocity field method for building up.
Background technique
In the probing of field well location, the prediction of strata pressure is extremely important, it can instruct the reasonable employment of drilling mud, Make it that can neither lead to formation contaminant greatly very much, and too small cannot lead to the safety accidents such as blowout, can also make rational planning for construction Operation reduces drilling cost, is an essential job before probing.The widely used master of pre-drilling pressure forecasting at present Will be there are two types of method, one is the pressure using neighbouring drilling well with change in depth trend progress simple forecast, but precision is very low, It can only reflect the basic variation on big set stratum, and the cross directional variations of strata pressure can not be predicted;Another kind is to utilize ground Shake processing speed spectrum, when there are intense vertical petroleum migration, seismic velocity can due to rock matrix undercompaction and lead to speed Degree reduces.Common seismic data processing explains that density is lower (usually in the plane due to normal-moveout spectrum manual interpretation heavy workload 40cdp explains a point, mono- point of 200-300ms on longitudinal direction), and the effective band of normal-moveout spectrum causes to differentiate generally in 1-5Hz Rate is very low, directly affects the precision of prediction of velocity field, cause the precision of seismic processing to reduce, lineups offset distance direction not It can even up, earthquake reflection line-ups are apprehensive on full stacked section, which then will lead to pressure for prediction of formation pressure Prediction deviation is excessive, brings great risk to drilling operation.
Exist in many exploratory areas and largely construct by a narrow margin, oil reservoir Structural range is low, and the variation of shallow-layer speed will have a direct impact on The form and range of entire oil reservoir need to accurately calculate the incidence angle of seismic data in prestack inversion, these require full range High-precision interval velocity field.
Summary of the invention
In order to solve the above problems existing in the present technology, present invention aims at establish full range high-precision interval velocity field to build Cube method.
The technical scheme adopted by the invention is as follows:
Full range high-precision interval velocity field method for building up, includes the following steps;
S1, ultralow frequency speed trend is established according to basin grade compacting trend;
S2, CRP trace gather optimization processing;
S3, fine grid residual velocity analysis obtain the root mean sequare velocity and residual mean square root speed of close CRP grid;
S4, the root mean sequare velocity of close CRP grid and residual mean square root speed are merged, with the speed after merging to the road CRP Collection carries out dynamic correction, obtains evening up seismic channel set, and speed progress DIX is converted to interval velocity after correction;
S5, seismic channel set progress partial stack will be evened up, and will obtain partial stack trace gather, carries out pre-stack elastic inversion;
S6, carried out using a point lithology probability volume constraint and divide lithology velocity inversion and porosity inversion, form medium-high frequency section layer Velocity inversion data volume;
S7, frequency dividing velocity field merge, floor speed after the correction that deposition compaction rate model, the S4 in certain area formed S1 are formed The Mid Frequency Interval Velocity Inversion data volume that degree and S6 are formed is merged in frequency domain, the full range high-precision layer after being optimized Velocity field.
Preferably, the specific implementation process of the S1 is: utilizing certain area drilling data, built using Spline-Fitting The deposition compaction rate model in the area Li Gai forms ultralow frequency speed trend.
Preferably, the specific implementation process of the S2 is: suppressing random noise and regular noise, to multiple wave It is suppressed.
Effect is to improve normal-moveout spectrum point correlation energy degree of focus, improves the quality of speed spectrum analysis.
Preferably, it is described S3's the specific implementation process is as follows:
S301, conventional speeds are composed with progress three-dimensional interpolation, obtains the root mean sequare velocity of close CRP grid, CRP trace gather is carried out Dynamic correction obtains just initiating correction trace gather, carries out close CRP point residual velocity analysis to the first initiating correction trace gather, seeks residue Dynamic correction value;
Residual normal moveout is sought being the key that close residual velocity analysis, and the normal-moveout spectrum point manually picked up is longitudinal and horizontal To all seldom, the 3D velocity field that interpolation obtains is not fine enough, causes trace gather uneven, affects the accurately image of earthquake, at this time Such as formula (1):
vt=vo+vr=vo*(1+δ) (1)
Wherein, vtIt is accurate offset RMS velocity, voIt is conventional manual's pickup velocity, vrIt is residual NMO correction speed, δ is Velocity error percentage;
Such as formula (2), the dynamic correction value of each point at this time are as follows:
Wherein, tNMOxIt is the time at offset distance x after dynamic correction, txWhen being walked before dynamic correction when be offset distance being x, v0For Seismic processing root mean sequare velocity.
Due to the presence of residual NMO correction speed, t is causedNMOx≠t0, trace gather cannot smooth completely on different offset distances;
S302, seismic channel set is superimposed entirely, obtains base offset section, by each seismic channel and base offset section Hour window cross-correlation is carried out, the best time shift amount of each offset distance of each CRP at every point of time is acquired, such as formula (3):
Time and t at S303, the offset distance x obtained by estimation after dynamic correction0Time utilizes identical CRP phase With the time in the best time shift amount of different offset distances, is solved based on least square method, acquire each time velocity error of each CRP Percentage δ;
S304, target equation are offset distance [x1,x2,x3,...,xn]、v0And residual move out time [tNMO1,tNMO2, tNMO3,...,tNMOx] function, solve to obtain residual mean square root speed by least square method.
Preferably, progress pre-stack elastic inversion obtains residual mean square root speed and obtains p-wave impedance, shear wave in the S5 Impedance, density, vp/vs, Young's modulus, be based on Bayesian Decision, obtain sandstone probability data volume, mud stone probability data body and carbon Carbonate Rocks probability volume.
The invention has the benefit that
The present invention improves the quality of seismic channel set to CRP trace gather optimization processing, improves normal-moveout spectrum point correlation energy and focuses Degree, improves the quality of speed spectrum analysis, the full range high-precision interval velocity field after optimization can meet subsequent structure with lower amplitude very well The demand of time and depth transfer, reservoir inversion and prediction of formation pressure.
Detailed description of the invention
Fig. 1 is the present invention-embodiment method flow diagram.
Specific embodiment
With reference to the accompanying drawing and specific embodiment the present invention is further elaborated.
Embodiment:
As shown in Figure 1, the full range high-precision interval velocity field method for building up of the present embodiment, includes the following steps:
The first step establishes ultralow frequency speed trend according to basin grade compacting trend.
Detailed process are as follows: utilize certain area drilling data, the deposition compaction rate in the area is established using Spline-Fitting Model forms ultralow frequency speed trend.
Second step, CRP trace gather optimization processing.
Improve the quality of seismic channel set, it is necessary to carry out trace gather optimization processing.
Detailed process are as follows: random noise and regular noise are suppressed, multiple wave is suppressed, effect is to improve Normal-moveout spectrum point correlation energy degree of focus, improves the quality of speed spectrum analysis.
Third step, fine grid residual velocity analysis.
Detailed process are as follows: conventional speeds are composed and carry out three-dimensional interpolation, the root mean sequare velocity of close CRP grid are obtained, to the road CRP Collection carries out dynamic correction, obtains just initiating correction trace gather, carries out close CRP point residual velocity analysis to the first initiating correction trace gather, asks Take residual normal moveout.
Residual normal moveout is sought being the key that close residual velocity analysis, and the normal-moveout spectrum point manually picked up is longitudinal and horizontal To all seldom, the 3D velocity field that interpolation obtains is not fine enough, causes trace gather uneven, affects the accurately image of earthquake, at this time Such as formula (1):
vt=vo+vr=vo*(1+δ) (1)
Wherein, vtIt is accurate offset RMS velocity, voIt is conventional manual's pickup velocity, vrIt is residual NMO correction speed, δ is Velocity error percentage.
Such as formula (2), the dynamic correction value of each point at this time are as follows:
Wherein, tNMOxIt is the time at offset distance x after dynamic correction, txWhen being walked before dynamic correction when be offset distance being x, v0For Seismic processing root mean sequare velocity.
Due to the presence of residual NMO correction speed, t is causedNMOx≠t0, trace gather cannot smooth completely on different offset distances.
Then, seismic channel set is superimposed entirely, obtains base offset section, by each seismic channel and base offset section Hour window cross-correlation is carried out, the best time shift amount of each offset distance of each CRP at every point of time is acquired, such as formula (3):
The t at offset distance x obtained by estimationNMOxAnd t0Time, using identical CRP same time in different offsets Away from best time shift amount, based on least square method solve, acquire each time velocity error percentage δ of each CRP.
Formula (3) target equation is offset distance [x1,x2,x3,...,xn]、v0And residual move out time [tNMO1,tNMO2,tNMO3,…, tNMOx] function, solve to obtain residual mean square root speed by least square method.
4th step, the root mean sequare velocity for the close CRP grid that third step is obtained and residual mean square root speed merge, with the speed Degree carries out dynamic correction to CRP trace gather, obtains evening up seismic channel set, and speed progress DIX is converted to interval velocity after correction.
5th step will even up seismic channel set progress partial stack, obtain partial stack trace gather, carry out pre-stack elastic inversion, Obtain p-wave impedance, S-wave impedance, density, vp/vs, Young's modulus etc., be based on Bayesian Decision, obtain sandstone probability data volume, Mud stone probability data body and carbonate rock probability volume.
6th step is carried out using a point lithology probability volume constraint and divides lithology velocity inversion and porosity inversion, and medium-high frequency is formed Section Interval Velocity Inversion data volume.
7th step, frequency dividing velocity field merge, and the deposition compaction rate model in certain area that the first step is formed, the 4th step are formed Correction after the medium-high frequency section Interval Velocity Inversion data volume that is formed of interval velocity and the 6th step merged in frequency domain, obtain excellent Full range high-precision interval velocity field after change can meet subsequent time and depth transfer, complicated structure research, prestack inversion and stratum very well The demand of pressure prediction.
The present invention is not limited to above-mentioned optional embodiment, anyone can show that other are various under the inspiration of the present invention The product of form, however, make any variation in its shape or structure, it is all to fall into the claims in the present invention confining spectrum Technical solution, be within the scope of the present invention.

Claims (5)

1. full range high-precision interval velocity field method for building up, it is characterised in that: include the following steps;
S1, ultralow frequency speed trend is established according to basin grade compacting trend;
S2, CRP trace gather optimization processing;
S3, fine grid residual velocity analysis obtain the root mean sequare velocity and residual mean square root speed of close CRP grid;
S4, the root mean sequare velocity of close CRP grid and residual mean square root speed are merged, with the speed after merging to CRP trace gather into Action correction, obtains evening up seismic channel set, and speed progress DIX is converted to interval velocity after correction;
S5, seismic channel set progress partial stack will be evened up, and will obtain partial stack trace gather, carries out pre-stack elastic inversion;
S6, carried out using a point lithology probability volume constraint and divide lithology velocity inversion and porosity inversion, form medium-high frequency section interval velocity Inverting data volume;
S7, frequency dividing velocity field merge, by S1 formed certain area deposition compaction rate model, S4 formed correction after interval velocity with And the medium-high frequency section Interval Velocity Inversion data volume that S6 is formed is merged in frequency domain, the full range high-precision layer speed after being optimized Spend field.
2. full range high-precision interval velocity field according to claim 1 method for building up, it is characterised in that: the specific reality of the S1 Existing process is: utilizing certain area drilling data, the deposition compaction rate model in the area is established using Spline-Fitting, formed super Low-frequency velocity trend.
3. full range high-precision interval velocity field according to claim 1 method for building up, it is characterised in that: the specific reality of the S2 Existing process is: suppressing random noise and regular noise, suppresses multiple wave.
4. full range high-precision interval velocity field according to claim 1 method for building up, it is characterised in that: the specific reality of the S3 Existing process is as follows:
S301, conventional speeds are composed with progress three-dimensional interpolation, obtains the root mean sequare velocity of close CRP grid, dynamic school is carried out to CRP trace gather Just, just initiating correction trace gather is obtained, close CRP point residual velocity analysis is carried out to the first initiating correction trace gather, seeks remaining dynamic school Positive quantity;
S302, seismic channel set is superimposed entirely, obtains base offset section, each seismic channel and base offset section are carried out Hour window cross-correlation, acquires the best time shift amount of each offset distance of each CRP at every point of time;
Time and t at S303, the offset distance x obtained by estimation after dynamic correction0Time utilizes identical CRP same time In the best time shift amount of different offset distances, is solved based on least square method, acquire each time velocity error percentage of each CRP Than;
S304, it solves to obtain residual mean square root speed by least square method.
5. full range high-precision interval velocity field according to claim 1 method for building up, it is characterised in that: in the S5, carry out Pre-stack elastic inversion obtains residual mean square root speed and obtains p-wave impedance, S-wave impedance, density, vp/vs, Young's modulus, be based on shellfish Ye Si differentiates, obtains sandstone probability data volume, mud stone probability data body and carbonate rock probability volume.
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CN112444861A (en) * 2019-08-27 2021-03-05 中国石油化工股份有限公司 Speed model updating method, computer storage medium and computer system
CN112782756A (en) * 2019-11-08 2021-05-11 中国石油天然气集团有限公司 Constrained layer velocity inversion method and system based on self-adaptive construction constraint
CN112946742A (en) * 2021-03-17 2021-06-11 成都捷科思石油天然气技术发展有限公司 Method for picking up accurate superimposed velocity spectrum
CN114114399A (en) * 2021-11-26 2022-03-01 同济大学 Intelligent speed spectrum interpretation and modeling method based on Bayes statistical decision
CN114398816A (en) * 2022-01-18 2022-04-26 科吉思石油技术咨询(北京)有限公司 Quantitative interpretation and three-dimensional visualization method for full three-dimensional well velocity field inversion

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CN114114399B (en) * 2021-11-26 2023-06-23 同济大学 Intelligent speed spectrum interpretation and modeling method based on Bayes statistical decision
CN114398816A (en) * 2022-01-18 2022-04-26 科吉思石油技术咨询(北京)有限公司 Quantitative interpretation and three-dimensional visualization method for full three-dimensional well velocity field inversion

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