Seismic exploration using exactly invertible discrete transformation into tau-p space

• US 4,760,563 A
• Filed: 01/09/1986
• Issued: 07/26/1988
• Est. Priority Date: 01/09/1986
• Status: Expired due to Term

• Current Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Original Assignee: Schlumberger Technology Corporation (Schlumberger NV)
• Inventors: Beylkin, Gregory
• Primary Examiner(s): Tarcza, Thomas H.
• Assistant Examiner(s): Pihulic, Daniel T.
• Application Number:
  US06/817,390
• Time in Patent Office: 929 Days
• Field of Search: 367/49, 367/43, 367/63, 367/73, 367/74, 367/40, 364/421, 364/422
• US Class Current: 367/73
• CPC Class Codes: G01V 1/32 Transforming one recording into another or one representation into another
• CPC Class Codes: G01V 1/364 Seismic filtering G01V1/37 takes precedence
• CPC Class Codes: G01V 2210/20 Trace signal pre-filtering to select, remove or transform specific events or signal components, i.e. trace-in/trace-out removing noise G01V2210/32
• CPC Class Codes: G01V 2210/40 Transforming data representation for pre-filtering purposes G01V2210/20
• CPC Class Codes: G01V 2210/47 Slowness, e.g. tau-pi

Abstract

Disclosed are a method and a system for discrete transformation of measurements such as seismic data into and out of tau-p space which is both exact and practical in terms of processing time. The measurements can be filtered or otherwise processed in tau-p space in ways which are not practical or possible in their original space. Since the transformations into and out of tau-p space are exact, the filtered and transformed measurements are free of errors and distortions that perturb known approximate transforms which can be performed in a reasonable time. When the transformation process is carried out in frequency space, it is done frequency-by-frequency, and when it is carried out in the spatial domain, it can utilize a transformation matrix having a block-circulant structure. In each case, the transformation process and matrix have a structure which substantially reduces storage and processing requirements as compared with known prior art.

Claims

1. A method of seismic exploration of subsurface formations comprising:

deriving a first seismogram of selected subsurface formations;

transforming said first seismogram to tau-p space through a discrete transformation process which permits exact discrete inverse-transformation and which in processing in the frequency domain can be completed frequency-by-frequency and in processing in the spatial domain can utilize a transformation matrix having a block-circulant structure;

processing the tau-p space seismogram to enhance desirable features thereof and effect an exact discrete inverse transformation from tau-p space to generate an improved seismogram; and

providing a tangible representation of the improved seismogram.

2. A method as in claim 1 in which said processing comprises processing the tau-p space seismogram to enhance desirable features thereof and thereby generate an improved tau-p space seismogram, and inverse-transforming said improved tau-p space seismogram using an exact discrete inverse transformation to generate said improved seismogram.

3. A method as in claim 2 including the step of providing a tangible representation of said improved tau-p space seismogram.

4. A method as in claim 1 including the step of performing a spectrum shift upon said first seismogram.

5. A method as in claim 4 in which said spectrum shift is incorporated in said transformation.

6. A method as in claim 1 in which the tangible representation of the improved seismogram is in the form of a visible display thereof.

7. A method as in claim 1 in which the inverse transformation transforms the improved tau-p space seismogram from tau-p space to the space in which said first seismogram was represented prior to its transformation into tau-p space.

8. A method as in claim 1 in which the transforming step comprises a transformation in which selected combinations of traces of said first seismogram and slopes of said tau-p space seismogram are weighted to enhance or suppress the effect of the corresponding portion of the tau-p space seismogram.

9. A method as in claim 1 in which the deriving step comprises deriving said first seismogram in time-offset space.

10. A method as in claim 1 in which the deriving step comprises deriving said first seismogram in time-depth space.

11. A method as in claim 1 in which the transforming step comprises a transformation in which selected curves of said first seismogram transform to points in tau-p space.

12. A method as in claim 11 in which said selected curves of said first seismogram are nonlinear.

13. A method of seismic exploration of subsurface formations comprising:

deriving a seismogram of subsurface formations which is in discrete form in a selected space;

transforming the seismogram through the use of a discrete form of a transform to generate a seismogram in tau-p space, in a process which comprises utilizing a transformation matrix having the property of being block circulant when represented in the spatial domain;

filtering the seismogram in tau-p space to generate a filtered seismogram;

inverse-transforming the filtered seismogram from tau-p space through the use of an exact discrete form of an inverse transform to thereby generate a filtered seismogram in the selected space; and

providing a tangible representation of the filtered seismogram in the selected space.

14. A method as in claim 13 in which said tangible representation is in the form of a visible display.

15. A method as in claim 13 in which the transforming step comprises a transformation in which selected combinations of traces of the seismogram which is in said selected space and slopes of the seismogram in tau-p space are weighted to enhance or suppress the effect of the corresponding portion of the tau-p seismogram.

16. A method as in claim 13 in which the transforming step comprises a transformation in which selected curves of the seismogram which is in said selected space transform to points in tau-p space.

17. A method as in claim 16 in which said selected curves are nonlinear.

18. A method of seismic exploration of subsurface formations comprising:

deriving an original seismogram of selected subsurface formations which is represented as a set of traces each comprising discrete samples of a selected seismic parameter over time for a selected spatial parameter;

transforming the original seismogram into tau-p space by transforming the original seismogram into the frequency domain, multiplying the frequency domain version of the original seismogram by selected transformation matrices for respective frequencies to derive respective product arrays, and inverse transforming the product arrays out of the frequency domain to derive a representation of the original seismogram in discrete form in tau-p space and allowing exact discrete inverse-transformation; and

providing a tangible representation of the seismogram in tau-p space in form suitable for modifying or display in tau-p space.

19. A method as in claim 18 including modifying the seismogram in tau-p space to thereby derive a modified seismogram in tau-p space.

20. A method as in claim 19 including transforming the modified seismogram into the frequency domain, multiplying the frequency domain version of the modified seismogram by the adjoint matrices of said transformation matrices to derive respective adjoint product arrays, using the adjoint matrices and the transformation matrices to derive selected matrices for filtering, solving for the array a linear relationship between the array and adjoint product arrays and said matrices for filtering, and inverse-transforming the last recited array out of frequency space to thereby generate a seismogram of said selected subsurface formations which corresponds to said modified seismogram in tau-p space but is represented as a set of traces each comprising discrete samples of a selected seismic parameter over time.

21. A method as in claim 18 including weighting selected combinations of traces of the original seismogram and slopes of the seismogram in tau-p space to enhance or suppress the effect of the corresponding portion of the tau-p seismogram.

22. A method as in claim 18 in which the transforming step comprises a transformation in which selected curves of the original seismogram transform to points in tau-p space.

23. A method as in claim 22 in which said selected curves are nonlinear.

28. A method as in claim 21 wherein the modifying step comprises inverse-transforming the array y_j (k+1) out of frequency space to derive the array y_j (n) and to represent it as a seismogram in (j,n) space allowing exact discrete inverse-transformation, and modifying the array y_j (n) to derive a modified seismogram, and including transforming the modified array y_j (n) into the frequency domain to generate said modified array y_j (k+1).

24. A method comprising:

deriving a two-dimensional array x_l (n) of seismic traces in (l,n) space, where l is an integer index which identifies a respective one of (2L+l) traces which are rows in the array and ranges from -L to +L, L being an integer, each row of the array comprises discrete samples of a selected seismic parameter, each sample being identified by an index n=1, 2, . . . , N, and x_l (n) is a periodic sequence with the period N, N being an integer;

deriving transformation matrices R_jl (k), where j is an integer index which identifies a respective one of (2J+l) rows of a transform matrix and ranges from -J to +J, l is an integer index which identifies a respective one of (2L+l) columns of a transformation matrix and ranges from -L to +L, and where k is a frequency index and J and L are integers;

transforming the array x_l (n) into the frequency domain to derive the array x_l (k+1);

matrix-multiplying the array x_l (k+1) by the matrices R_jl (k) to derive the array y_j (k+1) allowing exact discrete inverse-transformation; and

modifying the array y_j (k+1) to derive a modified array.

25. A method as in claim 24 in which the transformation matrices R_jl (k) are at least in part a function of the array x_l (n) and have the property of having a block-circulant structure when represented in the spatial domain.

26. A method as in claim 24 in which the modifying step comprises inverse-transforming the array y_j (k+1) out of frequency space to derive the array y_j (n) and to represent it as a seismogram in (j,n) space allowing exact discrete inverse-transformation, and modifying the array y_j (n) to derive a modified seismogram.

27. A method as in claim 24 including:

matrix-multiplying the modified array y_j (k+1) with adjoints of said transformation matrices to generate an array z_l (k+1);

generating matrices H_ll'"'"' (k) by matrix multiplying said transform and adjoint matrices, where l'"'"' is an integer index and ranges from -L to L, L being an integer;

solving the systems z_l (k+1)=H_ll'"'"' (k)x_l'"'"' (k+1) for the array x_l'"'"' (k+1), wherein said systems are linear; and

inverse-transforming the array x_l'"'"' (k+1) out of the frequency domain and into (l'"'"',n) space to derive a modified array x_l'"'"' (n) and to represent same as a modified seismogram in (l'"'"',n) space.

29. A method as in claim 24 including weighting selected combinations of traces of the seismogram in (l,n) space and slopes of the seismogram in (j,n) space to enhance or suppress the effect of the corresponding portion of the seismogram in (j,n) space.

32. A method comprising:

deriving an original record of measurements of a selected parameter of energy propagating in a medium and sampled in time and in space;

transforming the original record to a record in tau-p space through a discrete transformation process which permits exact discrete inverse-transformation and which in processing in the frequency domain can be completed frequency-by-frequency and in processing in the spatial domain can utilize a transformation matrix having a block-circulant structure;

processing the tau-p space record to enhance desirable features thereof and effect an exact discrete inverse transformation from tau-p space to generate an improved record; and

providing a tangible representation of the improved record.

30. A method as in claim 34 in which selected curves of the seismogram in (l,n) space transform to points in the seismogram in (j,n) space.

31. A method as in claim 30 in which said selected curves are nonlinear.

33. A method as in claim 32 in which said processing comprises processing the tau-p space record to enhance desirable features thereof and thereby generate an improved tau-p record to enhance desirable features thereof and thereby improved tau-p space record using an exact discrete inverse transformation to generate said improved record.

34. A method as in claim 33 including the step of providing a tangible representation of said improved tau-p space record.

35. A method as in claim 32 including the step of performing a spectrum shift upon said first record.

36. A method as in claim 35 in which said spectrum shift is incorporated in said transformation.

37. A method as in claim 32 in which the inverse transformation transforms the improved tau-p space record from the tau-p space to the space of the original record.

38. A method as in claim 32 including weighting selected combinations of traces of the original record and slopes of the record in tau-p space to enhance or suppress the effect of the corresponding portion of the tau-p space record.

39. A method as in claim 32 in which the transforming step comprises a transformation in which selected curves of the original record transform to points in the record in tau-p space.

40. A method as in claim 39 in which said selected curves of the original record are nonlinear.

41. A method comprising:

deriving an original record of data for a selected parameter sampled with respect to two independent variables defining an original domain;

transforming the original record to a record in a different domain in which each point results from a sum of values of said parameter taken over a corresponding pattern in said original domain, through a discrete transformation which permits exact discrete inverse-transformation and which in processing in a frequency domain corresponding to one of said independent variables can be completed frequency-by-frequency and in processing in said original domain with respect to the other of said independent variables can utilize a transformation matrix having a block-circulant structure;

processing said different domain record to enhance desirable features thereof and effect an exact discrete inverse transformation from said different domain to generate an improved record; and

providing a tangible representation of the improved record.

42. A method as in claim 41 in which said processing comprises processing said different domain record to enhance desirable features thereof and thereby generate an improved different domain record, and inverse-transforming said improved different domain record using an exact discrete inverse transformation to generate said improved record.

43. A method as in claim 42 including the step of providing a tangible representation of said improved different domain record.

44. A method as in claim 41 in which the inverse transformation transforms the improved different domain record from said different domain to said original domain.

45. A method as in claim 41 in which the transforming step comprises a transformation in which selected combinations of values of said original record and slopes of said different domain record are weighted to enhance or suppress the effect of the corresponding portion of the different domain record.

46. A method as in claim 41 in which said pattern is non-linear.

47. A method as in claim 41 in which said pattern is disjoint.