System for estimating azimuthal variations in seismic data

• US 6,681,184 B2
• Filed: 05/15/2001
• Issued: 01/20/2004
• Est. Priority Date: 05/15/2001
• Status: Expired due to Term

• Current Assignee: Input/Output Incorporated
• Original Assignee: Input/Output Incorporated
• Inventors: Jenner, Edward Louis, Williams, Martin Carroll
• Primary Examiner(s): Barlow, John
• Assistant Examiner(s): Le, Toan M
• Application Number:
  US09/855,925
• Publication Number:
  US 20030018435A1
• Time in Patent Office: 980 Days
• Field of Search: 702/14, 367/51, 367/50, 367/40, 367/46
• US Class Current: 702/14
• CPC Class Codes: G01V 1/303 for determining velocity profiles or travel times
• CPC Class Codes: G01V 1/362 Effecting static or dynamic corrections; Stacking
• CPC Class Codes: G01V 2210/53 Statics correction, e.g. weathering layer or transformation to a datum

Abstract

The invention comprises a system for processing seismic data to estimate time shift resulting from velocity anisotropy in the earth'"'"'s subsurface. A gather of seismic data traces is formed and selected seismic data traces included in said gather within selected time windows are cross-correlated to estimate the time shift in the seismic data traces included in said gather resulting from velocity anisotropy in the earth'"'"'s subsurface.

Claims

1. A method for processing seismic data comprising:

forming a gather of seismic data traces;

selecting a plurality of time windows in said seismic data gather;

within each selected time window, successively selecting seismic data traces in said gather and determining a time shift for each selected seismic data trace that achieves maximum correlation of the selected seismic data trace with a pilot trace formed by summing a plurality of traces within a spatial window of said gather of seismic data traces, said spatial window being spatially related to the selected seismic data trace; and

utilizing the time shifts determined for said selected seismic data traces in each selected time window to adjust said selected seismic data traces for velocity anisotropy in the earth'"'"'s subsurface.

2. The method of claim 1 further comprising utilizing a least squares method independently of knowledge of the angle between a predetermined zero azimuth direction and the maximum amplitude versus offset gradient direction to perform an amplitude variation with incidence angle analysis on said adjusted seismic data traces.

3. The method of claim 1 further comprising utilizing a least squares method independently of knowledge of the angle between a predetermined zero azimuth direction and the maximum amplitude versus offset gradient direction to perform an amplitude variation with azimuth analysis on said adjusted seismic data traces.

4. The method of claim 2 further comprising utilizing a least squares analysis to estimate errors associated with the calculation of amplitude variation in said selected seismic data traces.

5. The method of claim 1 wherein said gather is a common midpoint gather.

6. The method of claim 1 wherein said gather is a common reflection point gather.

7. The method of claim 1 wherein each selected time window is between 100 milliseconds and 300 milliseconds long.

8. The method of claim 1 wherein the element of utilizing the determined time shifts further comprises:

within selected time windows of said seismic data, adjusting the center point of seismic data traces included in said gather in accordance with the determined time shift and adjusting other locations in seismic data traces included in said gather by interpolation between the center points.

9. The method of claim 1 wherein the element of utilizing the determined time shifts further comprises:

within selected time windows of said seismic data utilizing the determined time shifts to calculate velocity variation for seismic data traces included in said gather as a function of azimuth and reflection angle;

within selected time windows of said seismic data adjusting the time positions of seismic data traces included in said gather in accordance with the calculated velocity variation.

10. The method of claim 1 further comprising performing a surface consistent statics solution on said adjusted traces.

11. The method of claim 1 further comprising:

performing a surface consistent statics solution on said adjusted traces; and

repeating the acts of

(a) within each selected time window, successively selecting seismic data traces in said gather and determining a time shift for each selected seismic data trace that achieves maximum correlation of the selected seismic data trace with a pilot trace formed by summing a plurality of traces within a spatial window of said gather of seismic data traces, said spatial window being spatially related to the selected seismic data trace and utilizing the time shifts determined for said selected seismic data traces in each selected time window to adjust said selected seismic data traces for velocity anisotropy in the earth'"'"'s subsurface, and

(b) performing a surface consistent statics solution on said adjusted traces until convergence of the determined time shifts has occurred.

12. The method of claim 8 further comprising utilizing a least squares analysis to estimate errors associated with the calculation of time shift variation in said selected seismic data traces.

13. The method of claim 9 further comprising utilizing a least squares analysis to estimate errors associated with the calculation of velocity variation in said selected seismic data traces.

14. A digital computer programmed to utilize seismic data traces obtained over a region of the earth'"'"'s subsurface to perform a process comprising the steps of:

forming a gather of seismic data traces;

selecting a plurality of time windows in said seismic data gather;

within each selected time window, successively selecting seismic data traces in said gather and determining a time shift for each selected seismic data trace that achieves maximum correlation of the selected seismic data trace with a pilot trace formed by summina a plurality of traces within a spatial window of said gather of seismic data traces, said spatial window beina spatially related to the selected seismic data trace; and

utilizing the time shifts determined for said selected seismic data traces in each selected time window to adjust said selected seismic data traces for velocity anisotropy in the earth'"'"'s subsurface.

15. A device which is readable by a digital computer having instructions defining the following process and instructions to the computer to perform said process:

forming a gather of seismic data traces;

selecting a plurality of time windows in said seismic data gather;

within each selected time window, successively selecting seismic data traces in said gather and determining a time shift for each selected seismic data trace that achieves maximum correlation of the selected seismic data trace with a pilot trace formed by summing a plurality of traces within a spatial window of said gather of seismic data traces, said spatial window being spatially related to the selected seismic data trace; and

utilizing the time shifts determined for said selected seismic data traces in each selected time window to adjust said selected seismic data traces for velocity anisotropy in the earth'"'"'s subsurface.

16. The device of claim 15 wherein said device is selected from the group consisting of a magnetic tape a magnetic disk, an optical disk and a CD-ROM.