Method for aquiring and processing marine seismic data to extract and constructively use the up-going and down-going wave-fields emitted by the source(s)

• US 20100008184A1
• Filed: 06/02/2009
• Published: 01/14/2010
• Est. Priority Date: 06/02/2008
• Status: Active Grant

• Current Assignee: PGS Geophysical As (PGS ASA)
• Original Assignee: PGS Geophysical As (PGS ASA)
• Inventors: Parkes, Gregory Ernest, Hegna, Stian
• Granted Patent: US 8,345,510 B2
• Time in Patent Office: Days
• US Class Current: 367/21
• CPC Class Codes: G01V 1/36 Effecting static or dynamic corrections on records, e.g. correcting spread; Correlating seismic signals; Eliminating effects of unwanted energy
• CPC Class Codes: G01V 1/3808 Seismic data acquisition, e.g. survey design
• CPC Class Codes: G01V 2210/56 De-ghosting; Reverberation compensation

Abstract

A method for acquisition and processing of marine seismic signals to extract up-going and down- going wave-fields from a seismic energy source includes deploying at least two marine seismic energy sources at different depths in a body of water. These seismic energy sources are actuated with known time delays that are varied from shot record to shot record. Seismic signals from sources deployed at different depths are recorded simultaneously. Seismic energy corresponding to each of the sources is extracted from the recorded seismic signals. Up-going and down-going wave-fields are extracted from the sources deployed at different depths using the extracted seismic energy therefrom. A method includes the separated up-going and down-going wave-fields are propagated to a water surface or a common reference, the up-going or the down-going wave-field is 180 degree phase shifted, and the signals from these modified up-going and down-going wave-fields are summed.

Claims

1. A method for acquisition and processing of marine seismic signals to extract up-going and down- going wave-fields from a seismic energy source, the method comprising:

deploying at least two marine seismic energy sources at different depths in a body of water and at substantially a same longitudinal position from a seismic vessel;

actuating each of the seismic energy sources in a plurality of firing sequences, each sequence having a known, different time delay between firing each source and a start of seismic signal recording;

recording seismic signals corresponding to each firing sequence;

extracting seismic energy corresponding to each of the sources from the recorded seismic signals; and

;

extracting at least one of an up-going and a down-going wave-field using the extracted seismic energy therefrom.

2. The method of claim 1 wherein the time delays vary in at least one of a random, semi-random and systematic manner between firing sequences.

3. The method of claim 1 wherein the extracting seismic energy from each source comprises time aligning the recorded signals with respect to a firing time of each source and coherency filtering the time aligned signals with respect to the corresponding time aligned source firings.

4. The method of claim 1 further comprising correcting for the differences in signatures of the sources towed at different depths.

5. The method of claim 1 further comprising designing sources towed at different depths such that they have nearly identical signatures.

6. The method of claim 1 wherein the signals are measured using at least one of pressure sensors, pressure time gradient responsive sensors, pressure depth gradient responsive sensors, particle motion responsive sensors and combinations thereof.

7. The method of claim 1 further comprising propagating the separated up-going and down-going wave-fields from each source to at least one of a water surface and a common reference depth, 180 degree phase shifting one of the up-going and the down-going wave-field, and summing the propagated, phase shifted up-going and down-going wave-fields.

8. The method of claim 7 where the extracted up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent time shifts based on known source depths and emission angles.

9. The method of claim 7 where the extracted up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent linear phase shifts in the frequency domain.

10. A method for marine seismic surveying, comprising:

separating up-going and down-going wave-fields from seismic energy emitted by at least one marine seismic energy source;

propagating the separated up-going and down-going wave-fields from the at least one source to at least one of a water surface and a common reference depth;

180 degree phase shifting one of the up-going and down-going wave-field; and

summing the propagated, phase shifted up-going and down-going wave-fields.

11. The method of claim 10 where the separated up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent time shifts based on known source depths and emission angles.

12. The method of claim 10 where the separated up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent linear phase shifts in the frequency domain.

13. The method of claim 10 where one of the separated up-going and down-going wave-field is 180 degree phase shifted before propagating the wave-fields to at least one of a water surface and a common reference depth.

14. The method of claim 10 where the up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth before 180 degree phase shifting.

15. The method of claim 10 wherein the seismic energy is emitted by at least two sources operated at different depths and at substantially a same geodetic position.

16. A method for marine seismic surveying using at least two seismic energy sources operated at different depths and at substantially a same source geodetic position, comprising:

separating energy from each of the sources from the recorded signals;

separating up-going and down-going wave-fields corresponding to each source from the separated energy;

propagating the separated up-going and down-going wave-fields from each source to at least one of a water surface and a common reference depth;

180 degree phase shifting one of the propagated wave-fields; and

summing the phase shifted, propagated wave-fields.

17. The method of claim 16 where the separated up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent time shifts based on known source depths and emission angles.

18. The method of claim 16 where the separated up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth using angle dependent linear phase shifts in the frequency domain.

19. The method of claim 16 where one of the separated up-going and down-going wave-field is 180 degree phase shifted before propagating the wave-fields to at least one of a water surface and a common reference depth.

20. The method of claim 16 where the up-going and down-going wave-fields are propagated to at least one of a water surface and a common reference depth before 180 degree phase shifting.