Seismic data processing method

• US 6,317,695 B1
• Filed: 03/30/2000
• Issued: 11/13/2001
• Est. Priority Date: 03/30/2000
• Status: Expired due to Term

• Current Assignee: TGS-NOPEC Geophysical Company
• Original Assignee: NuTec Sciences, Inc.
• Inventors: Zhou, Zheng-Zheng, Stein, Jaime A., Keehan, Michael S.
• Primary Examiner(s): McElheny, Jr., Donald E.
• Application Number:
  US09/539,143
• Time in Patent Office: 593 Days
• Field of Search: 702/14, 702/17, 702/18, 702/16, 367/73, 367/53, 367/45
• US Class Current: 702/17
• CPC Class Codes: G01V 1/28 Processing seismic data, e.g. for interpretation or for event detection G01V1/48 takes precedence
• CPC Class Codes: G01V 2210/51 Migration

Abstract

A method for migrating seismic data is disclosed in which seismic traces recorded by a plurality of receivers are separated into offset bands according to the offsets of the traces. The data in each offset band is then migrated according to a downward continuation method. The downward continuation method includes the calculation of a constant that is not dependent on the value of the wave field. The constant is used to calculated the wave field for all offset bands for a given z level, thereby reducing time and computation resources consumed by the migration of the offset bands. Following the downward continuation, an imaging condition may be applied to produce a seismic image.

Claims

1. A method for migrating seismic traces generated by a shot, comprising the steps of:

grouping the seismic traces into a number of offset bands;

migrating the data represented by the seismic traces of each offset band; and

assigning an offset to the migrated data of each offset band.

2. The method for migrating seismic traces of claim 1, wherein the step of grouping the seismic traces comprises the step of grouping the seismic traces into no fewer than ten offset bands.

3. The method for migrating seismic traces of claim 1, further comprising the step of applying an image condition to the migrated data of each offset band to produce an image.

4. The method for migrating seismic traces of claim 1, wherein the step of migrating the data comprises the step of performing a downward continuation on the data of each offset band.

5. The method for migrating seismic traces of claim 4, wherein the step of performing a downward continuation comprises solving an approximation of the full wave equation.

6. The method for migrating seismic traces of claim 5, wherein the step of performing a downward continuation comprises solving for a constant that can be used for the downward continuation across multiple offset bands at the same depth level.

7. The method for migrating seismic traces of claim 5, wherein the step of performing a downward continuation comprises the step of performing a error correction following a predetermined number of downward continuation steps.

8. The method for migrating seismic traces of claim 5, wherein the step of performing a downward continuation comprises the steps of:

solving for a constant that can be used for the downward continuation across multiple offset bands at the same depth level; and

performing an error correction following a predetermined number of downward continuation steps.

9. A method for performing a downward continuation function on a grouping of traces selected according to the offset of the traces, comprising the steps of:

collecting data representative of an up going wave field in the z direction at zero depth;

calculating a first intermediate value on the basis of data representative of the up going wave field at zero depth;

calculating a constant in the x direction, the value of the constant being independent of the value of the wave field;

calculating in the x direction a second intermediate value, the value being dependent on the first intermediate value and the constant in the x direction;

calculating a constant in the y direction, the value of the constant being independent of the value of the wave field;

calculating in the y direction the final value of the wave field at the next depth level based on the second intermediate value and the constant in the y direction;

repeating the above calculation steps to calculate the wave field at each successive depth level.

10. The method of claim 9, further comprising the step of performing an error correction function following the calculation of the wave field.

11. The method of claim 9, wherein the error correction function is performed following a predetermined number of downward continuation steps.

12. A method for migrating seismic traces, comprising the steps of:

recording a series of seismic traces at a number of receivers;

grouping the seismic traces into a number of offset bands;

migrating the data represented by the seismic traces of each offset band according to a wave equation based downward continuation method;

assigning an offset to the migrated data of each offset band that is equal to the midpoint of each offset band; and

applying an image condition to the migrated data.

13. The method for migrating seismic traces of claim 12, wherein the downward continuation method performed on each offset band comprises the following steps:

calculating a first intermediate value on the basis of data representative of the up going wave field at zero depth;

calculating a constant in the x direction, the value of the constant being independent of the value of the wave field;

calculating in the x direction a second intermediate value, the value being dependent on the first intermediate value and the constant in the x direction;

calculating a constant in the y direction, the value of the constant being independent of the value of the wave field;

calculating in the y direction the final value of the wave field at the next depth level based on the second intermediate value and the constant in the y direction;

repeating the above calculation steps to calculate the wave field at each successive depth level.

14. The method for migrating seismic traces of claim 13, wherein the constant in the x direction and the constant in the y direction may be used for the downward continuation for each offset band for a defined depth level.

15. The method for migrating seismic traces of claim 14, further comprising the step of performing an error correction function on a calculated wave field following a predetermined number of downward continuation steps.

16. The method for migrating seismic traces of claim 12, wherein the number of offset bands is selected to provide for sufficient resolution in the resulting image gathers.

17. A method for migrating seismic traces recorded at a series of receivers, comprising the steps of:

grouping the traces into a series of offset bands;

migrating each offset band separately;

wherein the migration for each offset band is accomplished according to a downward continuation in which the value of each following wave field in an x and y grid is determined on the basis of the value of the wave field in the preceding x and y grid and a constant that is not dependent on the value of the wave field; and

wherein the constant is used for the downward continuation of all bands, thereby reducing the computational time and resources required for migration.

18. The method for migrating seismic traces of claim 17, further comprising the step of performing an error correction function on the calculated wave field following a number of downward continuation steps.

19. The method for migrating seismic traces of claim 17, further comprising the step of performing an image condition on the migrated offset bands.