IP Library Granted Patent US 7,406,383
Granted Patent B2
US 7,406,383 · App. 10/565,403 · Granted Jul 29, 2008

Method of estimating the illumination fold in the migrated domain

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Quick Facts
Patent No.
US 7,406,383
App. No.
10/565,403
Granted
Jul 29, 2008
Kind
B2
Abstract

The invention relates to an estimate of the seismic illumination fold (x, p) in the migrated 3D domain at an image point x, for a dip of vector p characterized in that the illumination fold I (z, p; s, r) is estimated for each (source s, receiver r) pair in the seismic survey, by applying the following steps:—determination of the reflection travel time t r (·x r (p);s·r) from the source s to the specular reflection point z, on the plane reflector passing through the image point x and perpendicular to the dip vector p, and then return to the reflector r; starting from the diffraction travel time t d (·z;s·r) from the source to the said image point x and then return to the reflector r;—incrementing the said illumination fold I (X, p; s, r) related to the said (source s, receiver r) pair as a function of the difference between the diffraction travel time t d (x;s,r) and the reflection travel time tr(xr(p)issr).

Claims (343)

1. Method for estimating the seismic illumination fold |( x , p ) in the migrated 3D domain at least one image point x , for at least one dip of vector p , wherein the illumination fold I( x , p ; s , r ) for each (source s , receiver r ) pair in the seismic survey is estimated, by applying the following steps:

determination of the reflection travel time t r ( x r ( p ); s , r ) from the source s to the specular reflection point x r on the plane reflector passing through the image point x and perpendicular to the dip vector p and then returning to the reflector r ;

starting from the diffraction travel time t d ( x ; s , r ) from the source s to the said image point x and then returning to the reflector r ;

incrementing the said illumination fold I( x , p ; s , r ) related to the said (source s , receiver r ) pair as a function of the difference between the diffraction travel time t d ( x ; s , r ) and the reflection travel time t r ( x r ( p ); s , r ).

2. Method according to claim 1 , comprising the step of summating each of the said illumination folds I( x , p ; s , r ) related to a (source s , receiver r ) pair so as to determine the total illumination fold

I

(

x

_

,

p

_

)

=

s

_

p

_

I

(

x

_

,

p

_

;

s

_

,

r

_

)

.

3. Method according to claim 1 , wherein, during the incrementing step, the illumination fold I( x , p , s , r ) is incremented using an increment function i(t d ,t r ; s , r ) according to I( x , p )=I( x , p )+i(t d t r ; s , r ), the said increment function taking account of the difference between the diffraction travel time t d ( x ; s , r ) and the reflection travel time t r ( x r ( p ); s , r ).

4. Method according to claim 3 , wherein the increment function i is a function of the seismic wavelet s(t).

5. Method according to claim 4 , wherein the increment function i is expressed as a function of the derivative of the seismic wavelet s(t) according to:

i ( t d ,t r ; s , r )= s ( t d ( x ; s , r )− t r ( x r ( p ); s , r ).

6. Method according to claim 4 , wherein the increment function i is expressed as a function of the derivative s (t) of the seismic wavelet s(t) with respect to time according to:

i ( t d ,t r ; s , r )=( t d ( x ; s , r )− t r ( x r ( p ); s , r ).

7. Method according to any one of claims 3 to 6 , in which an a priori correction w( x , s , r ) of the illumination fold is taken into account by migration, comprising the step of incrementing the illumination fold I( x , p ; s , r ) related to a (source s , receiver r ) pair by i(t d t r ; s , r )·w( x ; s , r ).

8. Method according to claim 1 , wherein the determination step includes the second order Taylor series development of the diffraction travel time t d ( x ; s , r ) around the image point x :

t

d

(

x

_

;

s

_

,

r

_

)

=

t

d

(

x

_

;

s

_

,

r

_

)

+

(

_

x

t

d

(

x

_

;

s

_

,

r

_

)

)

T

·

(

x

_

r

-

x

_

)

+

1

2

(

x

_

r

-

x

_

)

T

·

Δ

x

,

x

t

d

(

x

_

;

s

_

,

r

_

)

·

(

x

_

r

-

x

_

)

.

9. Method according to claim 8 , wherein the specular reflection point x r ( p ) is determined along the length of the said reflector such that the diffraction travel time at the said specular reflection point x r ( p ) is stationary, according to the equation:

p T Λ( ∇ x t d ( x ; s , r )+(Δ x,x t d ( x ; s , r )·( x r ( p )− x ))= 0 .

10. Method according to claim 8 , wherein the specular reflection point x r and the reflection travel time t r ( x r ( p ); s , r ) are determined according to the following expressions:

x r ( p )= x −M·F −1 b

t r ( x r ( p ); s , r )= t d ( x ; s , r )−1/2· b r ·F −1 · b

where:

M is a (3×2) matrix described by two vectors extending along the length of the reflector, and therefore perpendicular to the dip vector p ;

b is a (2×1) vector of first order derivatives of the diffraction travel time along the reflection plane: b =M T ·( ∇ x t d );

F is a (2×2) matrix of second order derivatives of the diffraction travel time along the reflection plane: F=M T ·(Δ x,x t d )·M.

11. Method according to claim 10 , wherein the determination step uses isochronic migration maps t d ( x ; s , r ) specified for each (source s , receiver r ) pair involved in the migration at each image point x in the migrated 3D domain.

12. Method according to any one of the preceding claims, wherein the seismic illumination fold I( x , p ) in the migrated 3D domain is estimated during the Kirchoff summation migration of seismic data recorded during the 3D seismic prospecting.

13. Method for correction of seismic data amplitudes recorded during 3D seismic prospecting in order to compensate for the effect of non-uniform illumination of sub soil reflectors, comprising the steps of:

estimating the illumination fold I( x , p ) using the method according to claim 1 ,

using the inverse I −1 ( x , p ) of the said ratio as a weighting factor to be applied to each of the said seismic data amplitudes.

14. Method for selection of an acquisition geometry among a plurality of acquisition geometries as a function of the target of 3D seismic prospecting, comprising the steps of:

determining the illumination fold I( x , p ) by the method according to claim 1 , for each of the acquisition geometries considered,

selecting the acquisition geometry providing the optimum illumination fold as a function of the target.

15. Method according to claim 2 , wherein, during the incrementing step, the illumination fold I( x , p ; s , r ) is incremented using an increment function i(t d ,t r ; s , r ) according to I( x , p )=I( x , p )+i(t d ,t r ; s , r ), the said increment function taking account of the difference between the diffraction travel time t d ( x ; s , r ) and the reflection travel time t r ( x r ( p ); s , r ).

16. Method according to claim 15 , in which an a priori correction w ( x , s , r ) of the illumination fold is taken into account by migration, comprising the step of incrementing the illumination fold I( x , p ; s , r ) related to a (source s , receiver r ) pair by i(t d ,t r ; s , r )·w( x ; s , r ).

17. Method according to claim 16 , wherein the determination step includes the second order Taylor series development of the diffraction travel time (x; s, r) around the image point x:

t

d

(

x

_

;

s

_

,

r

_

)

=

t

d

(

x

_

;

s

_

,

r

_

)

+

(

_

t

d

x

(

x

_

;

s

_

,

r

_

)

)

T

·

(

x

_

r

-

x

_

)

+

1

2

(

x

_

r

-

x

_

)

T

·

Δ

x

,

t

d

x

(

x

_

;

s

_

,

r

_

)

·

(

x

_

r

-

x

_

)

18. Method according to claim 17 , wherein the specular reflection point x r ( p ) is determined along the length of the said reflector such that the diffraction travel time at the said specular reflection point x r ( p ) is stationary, according to the equation:

p T Λ( ∇ x t d ( x ; s , r )+(Δ x,x t d ( x ; s , r )·( x r ( p )− x ))= 0 .

19. Method according to claim 18 , wherein the specular reflection point x r and the reflection travel time t r ( x r ( p ); s , r ) are determined according to the following expressions:

x

_

r

(

p

_

)

-

x

_

-

M

·

F

-

1

·

b

_

t

r

(

x

_

r

(

p

_

)

;

s

_

,

r

_

)

=

t

d

(

x

_

;

s

_

,

r

_

)

-

)

1

2

·

b

_

r

·

F

-

1

·

b

_

where:

M is a (3×2) matrix described by two vectors extending along the length of the reflector, and therefore perpendicular to the dip vector p ;

b is a (2×1) vector of first order derivatives of the diffraction travel time along the reflection plane: b =M T ·( b =M T ·( ∇ x t d );

F is a (2×2) matrix of second order derivatives of the diffraction travel time along the reflection plane: F=M T ·(Δ x,x t d )·M.

20. Method according to claim 19 , wherein the determination step uses isochronic migration maps t d ( x ; s , r ) specified for each (source s , receiver r ) pair involved in the migration at each image point x in the migrated 3D domain.

21. Method according to claim 20 , wherein the seismic illumination fold I( x , p ) in the migrated 3D domain is estimated during the Kirchoff summation migration of seismic data recorded during the 3D seismic prospecting.

Assignments (3)
CHANGE OF NAME Recorded Aug 6, 2008
From: COMPAGNIE GENERALE DE GEOPHYSIQUE
To: COMPAGNIE GENERALE DE GEOPHYSIQUE - VERITAS
Reel/Frame 021339/0757 →
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Aug 6, 2008
From: COMPAGNIE GENERALE DE GEOPHYSIQUE - VERITAS
To: CGGVERITAS SERVICES SA
Reel/Frame 021339/0764 →
ASSIGNMENT OF ASSIGNOR'S INTEREST Recorded Mar 8, 2006
From: HERMANN, PHILLPPE; BOUSQUIE, NICOLAS
To: COMPAGNIE GENERALE DE GEOPHYSIQUE
Reel/Frame 017646/0218 →