CN104898162B - Crack detection method in geological exploration - Google Patents

Crack detection method in geological exploration Download PDF

Info

Publication number
CN104898162B
CN104898162B CN201410079665.6A CN201410079665A CN104898162B CN 104898162 B CN104898162 B CN 104898162B CN 201410079665 A CN201410079665 A CN 201410079665A CN 104898162 B CN104898162 B CN 104898162B
Authority
CN
China
Prior art keywords
orientation
component
wave
data
crack
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.)
Active
Application number
CN201410079665.6A
Other languages
Chinese (zh)
Other versions
CN104898162A (en
Inventor
魏修成
谢飞
刘兰锋
季玉新
张雅勤
陈天胜
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
Sinopec Exploration and Production Research Institute
Original Assignee
China Petroleum and Chemical Corp
Sinopec Exploration and Production Research Institute
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, Sinopec Exploration and Production Research Institute filed Critical China Petroleum and Chemical Corp
Priority to CN201410079665.6A priority Critical patent/CN104898162B/en
Publication of CN104898162A publication Critical patent/CN104898162A/en
Application granted granted Critical
Publication of CN104898162B publication Critical patent/CN104898162B/en
Active legal-status Critical Current
Anticipated expiration legal-status Critical

Links

Landscapes

  • Geophysics And Detection Of Objects (AREA)

Abstract

The invention discloses a crack detection method in geological exploration. The method comprises the following steps: obtaining converted wave signals in each acquisition orientation; based on an Alford rotation method, educing an analytical expression of two-component data of the converted wave signals in each acquisition orientation expressed by assumed orthogonally-arranged four-component data, orthogonally-arranged azimuth angles being randomly-assumed angles; based on the analytical expression, associating the two-component data in each acquisition orientation and the assumed orthogonally-arranged four-component signals, and carrying out calculating to obtain the four-component data in orthogonally-arranged orientation; and obtaining crack azimuth angle according to the four-component data in orthogonally-arranged orientation obtained through calculating, and carrying out detection to obtain orientation and time difference of the generation of a crack. The method breaks the limitation of orthogonal arrangement in a convention four-component Alford rotation shear wave splitting algorithm, and realizes a non-orthorhombic multi-component Alford rotation shear wave splitting algorithm.

Description

Crack detection method in geological prospecting
Technical field
The present invention relates to geological prospecting and oil-gas field development, furthermore, it is related to the Crack Detection in geological prospecting Method.
Background technology
Current multicomponent seismic survey technology mainly p-wave source excites, three-component or four component cymoscopes receive. Compressional wave is descending run into reflecting interface after wave mode can be occurred under certain condition to change, compressional wave is converted to shear wave and is referred to as converted wave (PS).The up shear wave of conversion can occur shear wave splitting phenomenon when encountering fracture medium, and this phenomenon can be detected device record Get off, it can play an important role in fracture detection type oil-gas reservoir.In the reservoir of fracture development, the speed of longitudinal wave propagation Change with line direction with amplitude and change.But, this variable quantity maximum less than 3%, slightly error in data processes and explains This Orientation differences may be covered.
And shear wave can be split into different polarization direction after entering crack(Generally orthogonal)Two Shear Waves Splittings.This two horizontal strokes Ripple has various amplitude size and speed spread speed, and typically strong amplitude is fireballing to be referred to as fast transverse wave(S1), otherwise it is slow Shear wave(S2).The principal direction in crack is exactly the direction of fast transverse wave.In multi-component seismic data collection observation system, along survey line side The component obtaining to embedding cymoscope is referred to as X-component, and the component obtaining along the embedding cymoscope of cross line direction is referred to as For Y-component.The acquisition system coordinate being determined by X, Y-component and " natural coordinates "(The Fracture System being defined by S1 ripple and S2 ripple)It Between exist a unknown angle, θ.
For the oil-gas reservoir of fracture detection type and its crack main formula position and development degree of micro cracks in oil effectively, available shear wave splitting This wave phenomenon is estimating the angle between coordinate acquisition and natural coordinates, so that it is determined that the main formula position of fracture development.Seek The time difference between fast transverse wave and slow shear-wave can determine whether the development degree in crack.Currently exist multiple utilization shear wave splitting phenomenons The method in detection crack, the number of components according to being related to is basically divided into two components method and four components method.Wherein, compare Influential it is:The four component spinning solutions based on pure shear wave exploration of Alford proposition in 1986, it is commonly referred to Alford Spinning solution;Two component spinning solutions of Thomsen proposition in 1988;And, Harrison was based on waveform similarity in 1992 Property assume to propose the spinning solution of two components.Two components method are more suitable for Converted P-SV-Waves Exploration in theory, because converted wave cannot The data matrix of four components is built as Alford.However, Comparatively speaking, four components method are more stable.James E.Gaiser1997 gives the Alford spinning solution based on converted wave four componets data, and his method is extensive in industrial quarters Accepted.This method builds the data matrix of four components using the converted wave data of the mutually orthogonal collection in two orientation, uses Carry out the four componets data that approximately pure shear wave exploration obtains.
As described above, four component A lford spinning solutions of converted wave orthogonal arrangement receive two collection arrangements must be just The restriction handed over.Therefore, in actual data collection, substantial amounts of data is in fact non-orthogonal, they or do not exist strict Orthogonal two collection orientation, or meet the data of orthogonality condition and relatively will lack a lot.And, do not exist orthogonal yet Arrangement, therefore, these data can only be avoided in Crack Detection.And the data volume used in Crack Detection is less will necessarily The correctness of impact result.Therefore, in order to sufficiently using the multi-component data collecting it is necessary to break orthogonal restriction.
For this reason, it may be necessary to provide a kind of do not need gathered component data all to meet orthogonal property just can be according to Alford Circumgyration determines fracture azimuth thus the method that detects crack generation position.
Content of the invention
The present invention is directed to the deficiencies in the prior art it is proposed that a kind of crack detection method in geological prospecting, it include with Lower step:
Obtain the converted wave signal in each collection orientation;
Derived based on Alford circumgyration and any institute gathering orientation is represented by the four componets data of the orthogonal arrangement supposing State two component data Analytical Expression of converted wave signal, the wherein orientation angles of orthogonal arrangement are the angle of arbitrary assumption;
Based on described Analytical Expression by two component datas in each collection orientation with assume orthogonal arrangement orientation on four points Amount signal contact gets up, thus trying to achieve the four componets data in orthogonal arrangement orientation;
Fracture azimuth is obtained based on the four componets data in calculated orthogonal arrangement orientation, thus detection is split Orientation and the time difference that seam occurs.
According to one embodiment of present invention it is assumed that the orientation angles of two orthogonal arrangement are 0 degree and 90 degree, then arbitrarily adopt Collection orientation two analytical expressions between component data and the four componets data of orthogonal arrangement be:
Wherein,Represent two component datas in i-th collection orientation respectively, a1, a2, a3, a4 represent 0 respectively Four componets data in degree, 90 degree of orientation orthogonal arrangement, θiRepresent the angle between i-th collection orientation and 0 degree of orientation.Obtain 0 degree of angle selected by this formula does not provide constraints to the present invention.
In one embodiment, tried to achieve according to following Analytical Expression two component datas in N number of any collection orientation with The relation of the four componets data of orthogonal arrangement:
Wherein, a1, a2, a3, a4 represent the four componets data in orthogonal arrangement orientation respectively, Represent two component datas in N number of any collection orientation, θ respectively1……θNRepresent collection orientation respectively Azimuth.
In one embodiment of the invention, according to four componets data a1, a2, a3, the a4 in orthogonal arrangement orientation with split Stitch the fast transverse wave component data f of the shear wave splitting causing11、f12With slow shear-wave component data f21、f22Between rotation relationship, base Shear wave splitting in theoretical model is assumed to calculate fracture azimuth θ:
It is assumed that the cross stream component f of fast transverse wave in shear wave splitting is assumed12Cross stream component f with slow shear-wave21It is zero, or The cross stream component sum of hypothesis fast transverse wave and slow shear-wave is zero:
f12+f21=0.
In one embodiment of the invention, crack detection method also includes scanning to count according to angle and time shift further Calculate the division time difference of fracture development orientation and Shear Waves Splitting.
In one embodiment of the invention, determine fracture orientation according to capacity volume variance maximum, then using rotation Matrix rotates to the four componets data in shear wave splitting orientation in fracture orientation, thus based on mutual between fast transverse wave and slow shear-wave Related relation divides the time difference to determine.
In one embodiment of the invention, described converted wave signal includes the component data of orthogonal arrangement and nonopiate row The component data of row.
Present invention offers following beneficial effect:
The present invention can achieve non-orthogonal Alford rotation, its can make full use of the data collecting come more accurately true Determine fracture orientation and the Concerning With Fast-slow Waves time difference, and provide crack based on the rational shear wave splitting theory hypothesis assumed as theoretical model Azimuthal analytical expression.The method of the present invention has broken the orthogonal row that traditional four component A lford rotate shear wave splitting algorithm The restriction of row is it is achieved that non-orthogonal multi -components Alford rotates shear wave splitting algorithm.The collection number of permutations for any angle According to the crack angle calculation that can realize shear wave splitting.Additionally, the fracture orientation angle additionally providing angle rotation sweep calculates Method.
Other features and advantages of the present invention will illustrate in the following description, and partly become from description It is clear that or being understood by implementing the present invention.The purpose of the present invention and other advantages can be by wanting in description, right Structure specifically noted in book and accompanying drawing is asked to realize and to obtain.
Brief description
Fig. 1 shows Alford coordinate rotation schematic diagram;
Fig. 2 is the method flow diagram of one embodiment of the present of invention;
Fig. 3 is the picture of the input component data before implementing the present invention;And
Fig. 4 is the picture implementing the output component data after the present invention carries out Concerning With Fast-slow Waves TEC time error correction.
Specific embodiment
To describe embodiments of the present invention below with reference to accompanying drawing in detail, whereby to the present invention how application technology means To solve technical problem, and reach realizing process and fully understanding and implement according to this of technique effect.As long as it should be noted that Do not constitute conflict, each feature in various embodiments of the present invention and each embodiment can be combined with each other, the technical side being formed Case is all within protection scope of the present invention.
Shear wave splitting detects that the classical way Alford spin theory in crack is to propose based on pure shear wave exploration.It will The shear-wave generation of orthogonal arrangement and shear wave is asked to receive.Later, J.E.Gaiser et al. was expanded in Converted P-SV-Waves Exploration, equally It is two orthogonal arrangements of requirement.
As shown in figure 1, two dotted lines represent the converted-wave acquisition arrangement of two different azimuth, their orthogonal thereto passes respectively System.Four components are collected and on parallel fracture and vertical fracture orientation according to Alford theory any two orthogonal arrangement Four components collecting meet Alford rotation formula, such as formula(1):
The four componets data that any orthogonal arrangement of matrix representative on the wherein equation left side collects, the right represents in crack The four componets data collecting in orientation, it just can obtain the left side after the spin matrix rotation of shot point and geophone station and appoint Four components in meaning orthogonal orientation.Thus, it is supposed that parallel fracture orientation and vertical fracture orientation collect four components can To be represented by a1, a2, a3, a4, such as formula(2)Matrix in the middle of the right.θiRepresentative fracture orientation to be found and collection orientation Angle, θ 1 as shown in Figure 1.And formula(2)The matrix on the left side then represents actual orthogonal arrangement and collects four components.
Because the orientation in crack is unknown although the azimuth of collection is known in itself, we also cannot know and adopt Collection orientation and the angle of fracture orientation.Therefore, formula cannot be built in the case(2)In the spin matrix related to angle. According to formula(2), four components of our available Concerning With Fast-slow Waves represented by four components of any orthogonal arrangement, first by (2)Formula deforms and obtains(3)Formula:
Now θiAngle for i-th collection orientation and fracture orientation is it is assumed that i+1 collection orientation is pressed from both sides with fracture orientation Angle is θi+ Δ θ, then can get following relation by four component types in the four representation in components i+1 orientation in i-th orientation:
It is deformed further and can get following relational expression;
In relational expression(5)In only exist the cut angle of azimuths in known two collection orientation, and eliminate unknown crack Azimuthal factor.Therefore, in the case that fracture orientation is unknown, the component of any two groups of orthogonal arrangement can mutually represent. In one embodiment, one group of orthogonal arrangement can be arbitrarily designated.Represent other with four components of this group orthogonal arrangement orthogonal Four components of arrangement.Such as may specify the orthogonal arrangement of 0 degree and 90 degree composition.The invention is not restricted to this angle.In this example In, take the convenience that " 0 degree " is merely to illustrate that, and expression formula can also simplify further(Because θ -0 is equal to θ), from And do not obscure principle and the purport of the present invention.
After assume that 0 degree of angle, the orientation angles of any orthogonal arrangement of angle are its angle theta.Therefore, work as formula(2) The data matrix on the right be 0 degree with 90 degree of data when, we take two components of the first row of left side matrix, according to formula (2)Just formula can be obtained(6)And formula(7).
So far, just obtained how being obtained two components in any one orientation by four components of 0 degree and 90 orientation Expression formula.Now, if collect two component datas in N number of orientation again, and these data are not necessarily to meet orthogonal arrangement Requirement.According to formula(6)And formula(7), just can get formula(8)Such expression formula:
Wherein, two components in the N number of orientation collecting known to the 2N amount representative on the equation left side.The right is 2NX4 Matrix representative gather orientation calculating matrix related to fracture orientation angle, shown herein as azimuth and 0 degree of azimuthal folder Angle.
According to formula(8)Just the required orthogonal row of Alford rotation can be no longer limited to when shear wave splitting detects crack Arrange, non-orthogonal arrangement equally can calculate shear wave splitting problem.
According to orientation two component data collecting, build as formula(8)Such equation group.Solving equations can get a1、a2、a3、a4.Two components making the fast transverse wave of shear wave splitting being caused by crack are f11And f12, two points of slow shear-wave Measure as f21And f22, then can obtain:
Further, can derive,
a2+a3=(f11-f22)sin2θ+(f12+f21)cos2θ (10)
a1-a4=(f11-f22)cos2θ-(f12+f21)sin2θ (11)
Again according to wave theory, in the case of shear wave splitting, wave field is divided into parallel fracture to propagate and vertical fracture is propagated.Cause This, the cross stream component of fast wave and the cross stream component of slow wave should not have in theory.It is often really not so in practical situations both, But provide hypothesis below also dependent on theory,
f12+f21=0(12)
Thus can obtain,
Can also scan to calculate fracture development orientation and the speed wavefront splitting time difference according to angle and time shift.In specified time shift In the case of amount scope and angle rotating range, according to wave theory, postrotational main energetic concentrates on and involves on slow wave soon, It is exactly on leading diagonal composition.Therefore, the energy that criterion is the elements in a main diagonal can be provided maximum, or minor diagonal unit The energy of element is minimum, is more than slow wave energy according to the general fast wave energy of hypothesis, specially:
f11 2> f22 2(14)
Δ E=f11 2+f22 2-f12 2-f21 2(15)
When the time difference and angle meet inequality and energy difference for maximum, corresponding angle and time shift amount are exactly fracture orientation The time difference with Concerning With Fast-slow Waves.
Can certainly be it is not assumed that fast wave energy be more than slow wave energy.Now, can be first formula according to capacity volume variance maximum (15), determine a fracture orientation.Then, using spin matrix by data rotation to fracture orientation.Now, diagonal entry Necessarily have one be fast wave another be slow wave.Here, when which can to determine by cross-correlation be to involve Concerning With Fast-slow Waves soon Difference.Work as f22Fracture orientation angle for determining before during fast wave has one 90 degree of correction, f11Then there is no fracture orientation for fast wave Angle Correction Problemss.
Above-mentioned principle can be realized by devices such as computers.As shown in Fig. 2 the flow chart for the inventive method.
First, in step s 201, obtain the converted wave signal in each collection orientation.
In step S202, derived based on Alford circumgyration and represent any by the four componets data of the orthogonal arrangement supposing The Analytical Expression of two component datas of described converted wave signal in collection orientation, the wherein orientation angles of orthogonal arrangement are arbitrarily false Fixed angle.Assume two orthogonal arrangement orientation angles be 0 degree and 90 degree, then arbitrarily gather orientation two component datas and Analytical expression between the four componets data of orthogonal arrangement is above-mentioned formula(6)And formula(7).In this formula,Respectively represent i-th collection orientation on two component datas, a1, a2, a3, a4 represent respectively 0 degree, 90 degree of orientation just Hand over the four componets data in arrangement, θiRepresent the angle between i-th collection orientation and 0 degree of orientation.
In step S203, based on above-mentioned Analytical Expression by two component datas in each collection orientation with assume orthogonal arrangement Four component signals in orientation are associated, thus trying to achieve the four componets data in orthogonal arrangement orientation.This four componets data meter Calculate formula such as formula(8).
In step S204, fracture azimuth is obtained based on the four componets data in calculated orthogonal arrangement orientation, Thus detection obtains orientation and the time difference of crack generation.
Specifically, divided according to the shear wave that four componets data a1, a2, a3, the a4 in orthogonal arrangement orientation and crack cause The fast transverse wave component data f splitting11、f12With slow shear-wave component data f21、f22Between rotation relationship, the horizontal stroke based on theoretical model Wavefront splitting is assumed to come by above formula(13)Calculate fracture azimuth θ:
It is assumed that the cross stream component f of fast transverse wave in shear wave splitting is assumed12Cross stream component f with slow shear-wave21It is zero, or The cross stream component sum of hypothesis fast transverse wave and slow shear-wave is zero, i.e. above-mentioned formula(12):
f12+f21=0.
First, the present invention has broken the restriction of orthogonal arrangement it is achieved that non-orthogonal Alford spinning solution.Secondly, exist The value of four components is calculated, such as formula under the constraint of all bearing datas collecting(8)Shown.Finally, at this four points Crack main formula position and Concerning With Fast-slow Waves time shift amount are calculated on amount.Now, can according to rotation method calculate fracture orientation, simultaneously this The bright fracture orientation computing formula that give also parsing.
Because Crack Detection includes the time difference and the orientation in detection crack, and the present invention mainly emphasizes to break through in Crack Detection The orthogonal precondition of original ALFORD method, it is achieved that the crack detection method of nonopiate arrangement ALFORD.And For TEC time error correction, generally the time difference can be asked using scanning and correlation.Also really can obtain after TEC time error correction more preferably Seismic profile.Those of ordinary skill in the art can carry out various deformation on the principle of the present invention, such as using various existing There is any TEC time error correction disclosed in technology all can realize the purpose of the present invention to some extent.Therefore the scope of the present invention Claim related content of having the right is defined.
In an experiment, devise one four layers of theoretical model.Wherein, table 1 gives the depth of model layer, fracture development Orientation and the time difference of Concerning With Fast-slow Waves.
Table 1
Layer position T0 (millisecond) Fracture orientation (is spent) Time delay(Millisecond)
1 90 30 15
2 150 95 10
3 250 280 12
4 310 170 8
Based on this theoretical model, each layer of fracture orientation and Concerning With Fast-slow Waves can be calculated well using the present invention The time difference.Can find out that from accompanying drawing the theoretical record as input result in imaging effect very because Concerning With Fast-slow Waves mix Difference is so that there is obvious sine wave phenomenon in R component.Calculate fracture development main formula position and the Concerning With Fast-slow Waves time difference through the present invention Afterwards, the R of input, T component are corrected, the R component image quality after correction significantly improves.Additionally, on lineups also not There is time delay again, T component assumes 90 degree of polarity inversion phenomenon, indicate the growth orientation in crack exactly.
The picture as the R inputting, T component data is given in Fig. 3 and 4.Because, before shear wave splitting corrects, speed is horizontal Ripple is concurrently present in R, on T component, and there is the time difference in Concerning With Fast-slow Waves, just occur in that the sine in R component is existing in itself after being therefore superimposed As.
Calculating the orientation of each slabbing seam and the when after the recovery of Concerning With Fast-slow Waves, input data is being corrected.In rotation To after Concerning With Fast-slow Waves, the time difference of correction Concerning With Fast-slow Waves, by slow wave be corrected to fast wave time consistency after re-rotate to R, on T component, This is the R of output, T component.
Although disclosed herein embodiment as above, described content is only to facilitate understanding the present invention and adopting Embodiment, is not limited to the present invention.Technical staff in any the technical field of the invention, without departing from this On the premise of the disclosed spirit and scope of invention, any modification and change can be made in the formal and details implemented, But the scope of patent protection of the present invention, still must be defined by the scope of which is defined in the appended claims.

Claims (7)

1. the crack detection method in a kind of geological prospecting is it is characterised in that comprise the following steps:
Obtain the converted wave signal in each collection orientation;
Derived based on Alford circumgyration and any institute gathering orientation is represented by the four componets data in the orthogonal arrangement orientation assumed State the Analytical Expression of two component datas of converted wave signal, the orientation angles of wherein orthogonal arrangement are any angle assumed;
Based on described Analytical Expression, two component datas in each collection orientation are believed with four components in the orthogonal arrangement orientation assumed Number it is associated, thus trying to achieve the four componets data in orthogonal arrangement orientation;
Fracture azimuth is obtained based on the four componets data in calculated orthogonal arrangement orientation, thus detection obtains crack and sends out The orientation educated and the time difference.
2. crack detection method as claimed in claim 1 it is characterised in that
Assume that the orientation angles of two orthogonal arrangement are 0 degree and 90 degree, then arbitrarily gather two component datas in orientation and orthogonal row Analytical expression between the four componets data in row orientation is:
Wherein,Represent two component datas in i-th collection orientation, a respectively1、a2、a3、a4Respectively represent 0 degree, 90 Four componets data in degree orientation orthogonal arrangement, θiRepresent the angle between i-th collection orientation and 0 degree of orientation.
3. crack detection method as claimed in claim 2 it is characterised in that try to achieve N number of any according to following Analytical Expression The relation of the four componets data in two component datas in collection orientation and orthogonal arrangement orientation:
Wherein, a1、a2、a3、a4Represent the four componets data in orthogonal arrangement orientation respectively, Table respectively Show two component datas in N number of any collection orientation, θ1……θNRepresent the azimuth in collection orientation respectively.
4. crack detection method as claimed in claim 3 is it is characterised in that according to the four componets data in orthogonal arrangement orientation a1、a2、a3、a4The fast transverse wave component data f of the shear wave splitting causing with crack11、f12With slow shear-wave component data f21、f22Between Rotation relationship, the shear wave splitting based on theoretical model assumes calculating fracture azimuth θ:
It is assumed that the cross stream component f of fast transverse wave in shear wave splitting is assumed12Cross stream component f with slow shear-wave21It is zero, or assume The cross stream component sum of fast transverse wave and slow shear-wave is zero:
f12+f21=0.
5. crack detection method as claimed in claim 4 is it is characterised in that also include being scanned according to angle and time shift further To calculate the time difference in fracture development orientation and Shear Waves Splitting.
6. crack detection method as claimed in claim 4 is it is characterised in that determine crack side according to capacity volume variance maximum Position, is then rotated to the four componets data in shear wave splitting orientation in fracture orientation using spin matrix, thus being based on fast transverse wave The relation of the cross-correlation and slow shear-wave between is determining the time difference.
7. the crack detection method as any one of claim 1-6 is it is characterised in that described converted wave signal is just included Hand over the arrangement component data in orientation and the component data in nonopiate arrangement orientation.
CN201410079665.6A 2014-03-06 2014-03-06 Crack detection method in geological exploration Active CN104898162B (en)

Priority Applications (1)

Application Number Priority Date Filing Date Title
CN201410079665.6A CN104898162B (en) 2014-03-06 2014-03-06 Crack detection method in geological exploration

Applications Claiming Priority (1)

Application Number Priority Date Filing Date Title
CN201410079665.6A CN104898162B (en) 2014-03-06 2014-03-06 Crack detection method in geological exploration

Publications (2)

Publication Number Publication Date
CN104898162A CN104898162A (en) 2015-09-09
CN104898162B true CN104898162B (en) 2017-02-15

Family

ID=54030922

Family Applications (1)

Application Number Title Priority Date Filing Date
CN201410079665.6A Active CN104898162B (en) 2014-03-06 2014-03-06 Crack detection method in geological exploration

Country Status (1)

Country Link
CN (1) CN104898162B (en)

Families Citing this family (4)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
CN106168678B (en) * 2016-07-15 2018-08-17 中国矿业大学(北京) The separation method and system of shear wave are propagated in a kind of crack
CN107132575B (en) * 2017-05-12 2019-03-29 中国地质大学(北京) Method based on shear wave polarographic analysis prediction fracture azimuth
CN107678063B (en) * 2017-09-25 2019-11-29 中国石油集团东方地球物理勘探有限责任公司 A kind of multi-component converted wave crack prediction method based on Rank correlation
CN110426739B (en) * 2019-08-02 2021-07-16 中铁第四勘察设计院集团有限公司 Geological exploration detection method and device and storage medium

Family Cites Families (3)

* Cited by examiner, † Cited by third party
Publication number Priority date Publication date Assignee Title
US5610875A (en) * 1995-09-29 1997-03-11 Western Atlas International, Inc. 3-D converted shear wave rotation with layer stripping
AU2003203024B2 (en) * 2002-01-15 2005-11-03 Westerngeco, L.L.C. Layer stripping converted reflected waveforms for dipping fractures
CN102053277A (en) * 2009-10-30 2011-05-11 中国石油化工股份有限公司 Method for detecting reservoir fissure development direction by utilizing seismic data

Also Published As

Publication number Publication date
CN104898162A (en) 2015-09-09

Similar Documents

Publication Publication Date Title
CN104155691B (en) Converted wave anisotropic velocity analysis method and device
CN104730579B (en) A kind of joint static correcting method of ripple in length and breadth based on calculation of near surface shear velocity inverting
CN104898162B (en) Crack detection method in geological exploration
CN106249295B (en) A kind of borehole microseismic P, S wave joint method for rapidly positioning and system
CN104570079A (en) Time matching method of longitudinal wave and converted shear wave seismic data
CN105093281B (en) A kind of Seismic Multi-wave modeling method under inverting framework
CN105116448B (en) A kind of converted wave azimuthal anisotropy bearing calibration and device
CN102879817B (en) Control method for acquiring underground crack information on basis of ground earthquake data
CN102053261A (en) Method for processing seismic data
Li et al. Radial anisotropy beneath northeast T ibet, implications for lithosphere deformation at a restraining bend in the K unlun fault and its vicinity
CN105629303A (en) Prestack crack quantitative forecast method and system based on rock physics
CN105588883B (en) Three-dimensional rock mechanical parameter acquisition method and system
CN106468782B (en) It is a kind of based on crack prediction method of the ceiling capacity than method
Hardebeck Seismotectonics and fault structure of the California Central Coast
CN104199103B (en) Static correction method and static correction device for converted wave
CN104570110A (en) Multi-component data joint speed analysis method based on longitudinal and horizontal wave matching
CN105954797A (en) Fracture identification method and fracture identification device of seismic data
CN105242313B (en) A kind of bearing calibration of elastic wave reverse-time migration polarity inversion and system
CN102053260B (en) Method for acquiring azimuth velocity of primary wave and method for processing earthquake data
CN107894616B (en) Multi-component converted wave crack prediction method
CN106468781A (en) A kind of crack prediction method based on minimum entropy circumgyration
CN102830170B (en) Control method and control device for obtaining coal sample transverse wave signal based on ultrasonic test
CN103869366B (en) Method and device for determining fracture strike
CN104914469B (en) Static correcting method and device in a kind of converted shear wave
CN105425287B (en) The prestack separation method of seismic wave

Legal Events

Date Code Title Description
C06 Publication
PB01 Publication
C10 Entry into substantive examination
SE01 Entry into force of request for substantive examination
C14 Grant of patent or utility model
GR01 Patent grant