Method for depth imaging multicomponent seismic data

• US 4,766,574 A
• Filed: 03/31/1987
• Issued: 08/23/1988
• Est. Priority Date: 03/31/1987
• Status: Expired due to Term

• Current Assignee: Amoco Corporation Chicago Illinois
• Original Assignee: Amoco Corporation (BP PLC)
• Inventors: Whitmore, Norman D. Jr., Marfurt, Kurt J.
• Primary Examiner(s): Tarcza, Thomas H.
• Assistant Examiner(s): Lobo, Ian J.
• Application Number:
  US07/032,907
• Time in Patent Office: 511 Days
• Field of Search: 364/421, 367/40, 367/41, 367/50, 367/53, 367/54, 367/59, 367/75
• US Class Current: 367/50
• CPC Class Codes: G01V 1/286 Mode conversion
• CPC Class Codes: G01V 1/303 for determining velocity profiles or travel times

Abstract

The present invention relates generally to a method of geophysical exploration and more particularly to a novel method for imaging multicomponent seismic data to obtain better depth images of the earth'"'"'s subsurface geological structure as well as better estimates of compressional and shear wave interval velocities. In particular, measures are obtained of imparted seismic wavefields incident on reflecting interfaces in the earth'"'"'s subsurface and of resulting seismic wavefields scattered therefrom. The incident and scattered seismic wavefields are employed to produce time-dependent reflectivity functions representative of the reflecting interfaces. By migrating the time-dependent reflectivity functions, better depth images of the reflecting interfaces can be obtained. For a dyadic set of multicomponent seismic data, the dyadic set of multicomponent seismic data are partitioned so as to separate the variously coupled incident and reflected wavefields in the recorded multicomponent seismic data. The incident and reflected wavefields are cross-correlated to form time-dependent reflectivity functions. The time-dependent reflectivity functions are then iteratively migrated according to a model of wavefield velocities of propagation to obtain better estimates of the compressional and shear wave interval velocity. The migrated reflectivity functions can then be stacked to produce better depth images of the earth'"'"'s subsurface geological structures.

Claims

1. A method of geophysical exploration to obtain depth images of the earth'"'"'s subsurface geological structures, comprising the steps of:

(a) obtaining separate measures of compressional and shear wavefields incident on reflecting interfaces in the earth'"'"'s subsurface;

(b) obtaining measures of compressional and shear wavefields scattered from the reflecting interfaces;

(c) producing time-dependent reflectivity functions representative of the reflecting interfaces from the compressional and shear wavefields incident thereon and the compressional and shear wavefields scattered therefrom; and

(d) migrating the time-dependent reflectivity functions to obtain depth images of the reflecting interfaces in the earth'"'"'s subsurface.

2. The method of claim 1 wherein the step of obtaining separate measures of the compressional and shear wavefields incident on the reflecting interface comprises obtaining separate measures of the compressional and shear wavefields for seismic energy imparted into the earth'"'"'s subsurface by seismic sources and the step of obtaining measures of the compressional and shear wavefields scattered from the reflecting interfaces comprises partitioning a set of multicomponent seismic data recording the earth'"'"'s response to seismic energy imparted into the earth'"'"'s subsurface by the seismic sources to form reflected compressional and shear wavefields.

3. The method of claim 1 wherein the step of producing time-dependent reflectivity functions representative of reflecting interfaces includes separately cross-correlating the compressional and shear wavefields incident on reflecting interfaces with the compressional and shear wavefields scattered from the reflecting interfaces.

4. The method of claim 1 wherein the step of migrating the time-dependent reflectivity functions representative of the reflecting interfaces includes iteratively assuming velocities of propagation for the incident and scattered compressional and shear wavefields.

5. A method of imaging multicomponent seismic data to obtain depth images of the earth'"'"'s subsurface geological structures, comprising the steps of:

(a) beam forming the multicomponent seismic data into sets of plane wave seismograms;

(b) partitioning the plane wave seismograms into sets of compressional and shear wavefield seismograms;

(c) forming time-dependent reflectivity functions from the sets of compressional and shear wavefield seismograms; and

(d) migrating the time-dependent reflectivity functions to obtain depth images of the earth'"'"'s subsurface geological structures.

6. The method of claim 5 wherein the step of beam forming the multicomponent seismic data includes forming sets of plane wave seismograms for a plurality of beamed angles.

7. The method of claim 6 wherein the step of partitioning the sets of plane wave seismograms includes forming sets of compressional and shear wavefield seismograms for the plurality of beamed angles.

8. The method of claim 7 wherein the step of forming time-dependent reflectivity functions includes forming a plurality of reflectivity functions for the plurality of beamed angles.

9. The method of claim 8 wherein the step of migrating the time-dependent reflectivity functions includes migrating the time-dependent reflectivity functions for each of the plurality of beamed angles and stacking the migrated time-dependent reflectivity functions for the plurality of beamed angles to form depth images of the earth'"'"'s subsurface geological structures.

27. The method of claim 5 further including the step of:

(a) iteratively migrating the time-dependent reflectivity functions for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images of the earth'"'"'s subsurface geological structures.

10. A method for imaging the earth'"'"'s subsurface geological structures, comprising the steps of:

(a) collecting a set of multicomponent seismic data with seismic sources having at least one linearly independent line of action and receivers having at least two linearly independent lines of action;

(b) sorting the set of multicomponent seismic data into incident angle ordered gathers;

(c) partitioning the incident angle ordered gathers of the set of multicomponent seismic data into compressional and shear wavefields; and

(d) migrating the compressional and shear wavefields to obtain a depth image of the earth'"'"'s subsurface geological structures.

11. The method of claim 10 wherein the step of sorting the set of multicomponent data includes the step of beam forming the set of multicomponent seismic data for a plurality of beamed angles.

12. The method of claim 10 further including the steps of:

(a) transforming the set of multicomponent seismic data into the frequency domain;

(b) partitioning the frequency domain set of multicomponent seismic data into a plurality of wavefield potentials; and

(c) transforming the plurality of compressional and shear wavefields to the time domain.

13. The method of claim 11 wherein the step of partitioning includes forming a plurality of compressional and shear wavefields incident upon reflecting interfaces in the earth'"'"'s subsurface and resulting compressional and shear wavefields scattered from the reflecting interfaces.

14. The method of claim 13 further including the step of cross-correlating the incident and scattered compressional and shear wavefields to form time-dependent reflectivity functions representative of reflecting interfaces in the earth'"'"'s subsurface.

15. The method of claim 14 wherein the step of migrating the compressional and shear wavefields includes migrating the time-dependent reflectivity functions to obtain depth images of the earth'"'"'s subsurface geological structures.

16. The method of claim 15 further including the step of stacking the plurality of migrated compressional and shear wavefields to form depth images of the earth'"'"'s subsurface geological structures.

28. The method of claim 10 further including the step of:

(a) iteratively migrating the time-dependent reflectivity functions for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images of the earth'"'"'s subsurface geological structures.

17. A method for imaging the earth'"'"'s subsurface geological structures, comprising the steps of:

(a) collecting a set of multicomponent seismic data;

(b) partitioning the set of multicomponent seismic data so as to separate and decouple compressional and shear wavefield potentials in the set of multicomponent seismic data;

(c) iteratively migrating the separated and decoupled compressional and shear wavefields for a plurality of assumed compressional and shear interval velocities; and

(d) selecting from the plurality of assumed compressional and shear wave and shear interval velocities, the compressional interval velocities which produce coherent migrated wavefields.

18. The method of claim 17 wherein the step of partitioning includes obtaining a measure of the compressional and shear wavefields incident upon reflecting interfaces and resulting compressional and shear wavefields scattered therefrom.

19. The method of claim 18 further including the step of cross-correlating the compressional and shear wavefields incident and scattered from reflecting interfaces to obtain a reflectivity functions representative of the reflecting interfaces.

20. The method of claim 19 wherein the step of iteratively migrating the compressional and shear wavefields includes iteratively migrating the shear and compressional wavefields of the incident and scattered compressional and shear wavefields according to a model of the compressional and shear wave velocities of propagation in the earth'"'"'s subsurface.

21. A method of geophysical exploration to obtain depth images of the earth'"'"'s subsurface geological structures from multicomponent seismic data U_ij, wherein seismic energy is imparted into the earth with seismic sources having at least one linearly independent line of action i and the earth'"'"'s response thereto is recorded by receivers having at least two linearly independent lines of action j, comprising steps of:

(a) obtaining separate measures of compressional and shear wavefields generated by the seismic energy imparted into the earth which are incident on reflecting interfaces in the earth'"'"'s subsurface;

(b) obtaining separate measures of compressional and shear wavefields scattered from reflecting interfaces in the earth'"'"'s subsurface from the multicomponent seismic data U_ij ; and

(c) migrating the incident and scattered compressional and shear wavefields to obtain depth images of the earth'"'"'s subsurface geological structures.

22. The method of claim 21 further including a step of:

separately cross-correlating the incident compressional and shear wavefields with the scattered compressional and shear wavefields to produce a plurality of time-dependent reflectivity functions representative of reflecting interfaces in the earth'"'"'s subsurface.

23. The method of claim 22 further including the step of:

migrating the plurality of time-dependent reflectivity functions to obtain depth images of the reflecting interfaces and the earth'"'"'s subsurface.

29. The method of claim 21 further including the step of:

(a) iteratively migrating the incident scattered compressional and shear wavefields for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images of the earth'"'"'s subsurface geological structures.

24. A method of imaging multicomponent seismic data U_ij, wherein seismic energy is imparted into the earth with seismic sources having at least one linearly independent line of action i and the earth'"'"'s response thereto is recorded by receivers having at least two linearly independent lines of action j, comprising the steps of:

(a) radon transforming the multicomponent seismic data U_ij ;

(b) partitioning the radon transform multicomponent seismic data U_ij to separate and decouple measures of compressional and shear wavefields scattered from reflecting interfaces in the earth'"'"'s subsurface;

(c) partitioning the seismic energy imparted into the earth to separate the decouple measures of compressional and shear wavefields incident on the reflecting interfaces in the earth'"'"'s subsurface; and

(d) migrating the compressional and shear wavefields incident on reflecting interfaces and the compressional and shear wavefields scattered from the reflecting interfaces to obtain depth images of the earth'"'"'s subsurface geological structures.

30. The method of claim 24 further including the step of:

(a) iteratively migrating the incident scattered compressional and shear wavefields for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images of the earth'"'"'s subsurface geological structures.

25. A method for imaging the earth'"'"'s subsurface geological structures, comprising the steps of:

(a) obtaining a set of multicomponent seismic data U_ij, wherein seismic energy is imparted into the earth with seismic sources having at least one linearly independent line of action i and recording the earth'"'"'s response thereto with receivers having at least two linearly independent lines of action j;

(b) partitioning the multicomponent seismic data U_ij so as to separate and decouple compressional and shear wavefields measured by the set of multicomponent seismic data U_ij and

(c) migrating the separated and decoupled compressional and shear wavefields so as to obtain depth images of the earth'"'"'s subsurface geological structures.

31. The method of claim 25 further including the step of:

(a) iteratively migrating the incident scattered compressional and shear wavefields for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images of the earth'"'"'s subsurface geological structures.

26. A method for imaging the earth'"'"'s subsurface geological structures with multicomponent seismic data U_ij, wherein the multicomponent seismic data U_ij is obtained by imparting seismic energy into the earth with seismic sources having at least one linearly independent line of action i and recording the earth'"'"'s response thereto with receivers having at least two linearly independent lines of action j, comprising the steps of:

(a) radon transforming the multicomponent seismic data U_ij to obtain sets of plane wave seismograms, wherein each set of plane wave seismograms includes plane wave seismograms for a plurality of incident angles;

(b) partitioning each set of plane wave seismograms to separate and decouple compressional and shear wavefields scattered from reflecting interfaces in the earth'"'"'s subsurface;

(c) partitioning the seismic energy imparted into the earth to separate and decouple measures of compressional and shear wavefields incident on reflecting interfaces in the earth'"'"'s subsurface

(d) cross correlating the incident and reflecting compressional and shear wavefields to obtain a plurality of time-dependent reflectivity functions; and

(e) iteratively migrating the plurality of time-dependent reflectivity functions for a plurality of compressional and shear wavefield interval velocities to determine the compressional and shear wavefield interval velocities which produce spatially consistent depth images.