Method of conducting a seismic survey

• US 9,030,909 B2
• Filed: 02/06/2007
• Issued: 05/12/2015
• Est. Priority Date: 02/06/2006
• Status: Active Grant

• Current Assignee: Statoil Petroleum As (Asa Equinor)
• Original Assignee: Statoil Petroleum As (Asa Equinor)
• Inventors: Hogstad, Kai, Fotland, Bente, Gerea, Constantin
• Primary Examiner(s): Murphy, Daniel L
• Application Number:
  US12/278,446
• Publication Number:
  US 20090219783A1
• Time in Patent Office: 3,017 Days
• Field of Search: 102/23, 102/301, 114/244, 114/253, 181/104, 181/106, 181/111, 181/112, 340/7.R, 340/25.5 R, 367/20, 367/53, 367/57, 367/154, 702/6, 702/14
• US Class Current: 367/20
• CPC Class Codes: G01V 1/02 Generating seismic energy G01V1/003 takes precedence

Abstract

A method of conducting a seismic survey of an area including a region of high seismic velocity regimes in a shallow overburden. According to the method, a zone is identified in which the boundary of the high seismic velocity region has a substantially constant critical angle and a course is plotted through the identified zone. A zone based directional seismic source is applied sequentially, with a directivity angle equal to or close to the measured critical angle. The response is detected using receivers.

Claims

1. A method of conducting a seismic survey of a geological feature comprising a plurality of zones, the method comprising applying a directional seismic source to each zone of the feature with a directivity angle equal to or close to a measured critical angle of the respective zone of the feature, wherein for each zone, the source directivity angle is constant and tuned to the critical angle of the respective zone, whereby the seismic source is a zone-based directional source, and wherein the seismic source comprises a series of seismic guns with different directivities tuned to different critical angles.

2. A method according to claim 1, for conducting a seismic survey of an area including a region of high seismic velocity regimes in a shallow overburden, comprising the steps of:

i.) identifying a zone in which a boundary of the high seismic velocity region has a substantially constant measured critical angle;

ii.) plotting a course through the identified zone, and;

iii.) sequentially applying the zone-based directional seismic source with a directivity angle equal to or close to the measured critical angle of the identified zone.

3. A method according to claim 2, including the further step of identifying a plurality of zones, in each of which the boundary of the high seismic velocity region has a substantially constant measured critical angle range and performing steps ii. and iii. in each identified zone.

4. A method according to claim 1, wherein the seismic guns are fired selectively along a course, so that the directivity of the guns is optimized to the geological feature under consideration.

5. A method according to claim 4, wherein the course followed by a vessel towing the source is substantially straight, for at least a portion of its extent.

6. A method according to claim 1, wherein the directivity angle is +/−

20°

of the critical angle of the respective zone.

7. A method according to claim 6, wherein the directivity angle is +/−

5% of the critical angle of the respective zone.

8. A method according to claim 1, wherein a response to the applied seismic source is detected by means of a plurality of receivers.

9. A method according to claim 8, wherein the receivers are towed behind the same vessel that tows the source.

10. A method according to claim 9, wherein the vessel towing the source and the receivers is arranged to follow a course which corresponds to a predefined constant critical angle zone.

11. A method according to claim 8, wherein the receivers are mounted on streamers extending behind a vessel.

12. A method according to claim 11, wherein the streamers are steerable.

13. A method according to claim 8, wherein the source directivity and a directivity of any streamers carrying receivers, are respectively tuned to the spatial variation of the actual critical angle in the overburden.

14. An apparatus for carrying out a method as claimed in claim 1, the apparatus comprising a seismic source with flexibility in directivity and a seismic receiver.

15. An apparatus according to claim 14, comprising a 3D acquisition system, utilizing a source with a variable directivity, tuned to varying critical angles in the overburden.

16. Apparatus according to claim 14, comprising a plurality of receivers operated on streamers, the streamers having steering and navigational positioning equipment.