Correcting time shifts

US2016178773A1 · US · A1

Patent metadata
FieldValue
Publication numberUS-2016178773-A1
Application numberUS-201514728086-A
CountryUS
Kind codeA1
Filing dateJun 2, 2015
Priority dateDec 18, 2014
Publication dateJun 23, 2016
Grant date

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Abstract

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At least some of the example embodiments are methods including: performing Normal MoveOut (NMO) correction on a first Common Depth Point (CDP) gather, the NMO correction based on a reference velocity of sound in water, the NMO correction creates first NMO data with a plurality of traces; selecting a first estimated velocity that makes travel time represented in the traces substantially the same; calculating a zero-offset time shift that represents a difference in travel time as between the reference velocity and the first estimated velocity at a zero-offset trace; performing NMO correction on the first CDP gather based on a final estimated velocity to create second NMO data; adding the zero-offset time shift to each trace of the second NMO data; and then performing reverse NMO correction on the second NMO data to create corrected data.

First claim

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What is claimed is: 1 . A method of generating a geophysical data product, the method comprising: obtaining the geophysical data; and processing the data to generate the geophysical data product; wherein processing comprises: performing Normal MoveOut (NMO) correction on a first Common Depth Point (CDP) gather based on a reference velocity to create first NMO data comprising a plurality of traces; selecting a first estimated velocity that makes travel time represented in the traces of the first NMO data substantially the same; calculating a zero-offset time shift that represents a difference in travel time as between the reference velocity and the first estimated velocity at a zero-offset trace; performing NMO correction on the first CDP gather using a final estimated velocity to create second NMO data, the final estimated velocity selected based on the first estimated velocity; adding the zero-offset time shift to each trace of the second NMO data; and then performing reverse NMO correction on the second NMO data. 2 . The method of claim 1 further comprising, prior to performing NMO correction on the first CDP gather, adjusting location of a common depth point used for the first CDP gather, the adjusting to account for slope of the sea bed 3 . The method of claim 1 further comprising recording the geophysical data product on a tangible, non-volatile computer-readable medium suitable for importing onshore. 4 . The method of claim 1 further comprising performing geophysical data analysis onshore on the geophysical data product. 5 . The method of claim 1 wherein calculating the zero-offset time shift further comprises calculating using the following equation: Δ   t = 2 × Z WB × ( 1 v ref - 1 v est ) where Δt is the zero-offset time shift in seconds, Z WB is the depth of the water bottom in meters along at least a portion of a common depth point associated with the CDP gather, Vref is a reference water velocity in meters per second, and Vest is the final estimated velocity in meters per second. 6 . A method comprising: performing Normal MoveOut (NMO) correction on a first Common Depth Point (CDP) gather, the NMO correction based on a reference velocity, the NMO correction creates first NMO data comprising a plurality of traces; selecting a first estimated velocity that makes travel time represented in the traces of the first NMO data substantially the same; calculating a zero-offset time shift that represents a difference in travel time as between the reference velocity and the first estimated velocity at a zero-offset trace; performing NMO correction on the first CDP gather based on a final estimated velocity to create second NMO data, the final estimated velocity selected based on the first estimated velocity; adding the zero-offset time shift to each trace of the second NMO data; and then performing reverse NMO correction on the second NMO data to create corrected data. 7 . The method of claim 6 further comprising, prior to performing NMO correction on the first CDP gather, adjusting location of a common depth point used for the first CDP gather, the adjusting to account for slope of the sea bed. 8 . The method of claim 6 further comprising: performing NMO correction on a second CDP gather based on the reference velocity to create third NMO data comprising a plurality of traces, the second CDP gather along a sail line that includes the first CDP gather; selecting a second estimated velocity that makes travel time represented in the traces of the third NMO data substantially the same; selecting the final estimated velocity based on the first and second estimated velocity; performing NMO correction on the second CDP gather based on the final estimated velocity to create fourth NMO data; adding the zero-offset time shift to each trace of the fourth NMO data; and then performing reverse NMO correction on the fourth NMO data. 9 . The method of claim 8 further comprising, prior to performing NMO correction on the second CDP gather, adjusting location of a common depth point used for the second CDP gather, the adjusting to account for slope of the sea bed. 10 . The method of claim 8 wherein selecting the final estimated velocity further comprises filtering a representation of the first and second estimated velocities to create the final estimated velocity. 11 . The method of claim 6 wherein calculating the zero-offset time shift further comprises calculating using the following equation: Δ   t = 2 × Z WB × ( 1 v ref - 1 v est ) where Δt is the zero-offset time shift in seconds, Z WB is the depth of the water bottom in meters along at least a portion of a common depth point associated with the CDP gather, Vref is a reference water velocity in meters per second, and Vest is the final estimated velocity in meters per second. 12 . The method of claim 6 further comprising: analyzing the corrected data against earlier data collected during a marine geophysical survey performed at a different time than the corrected data; changing a hydrocarbon extraction technique based on the differences between the earlier data and the corrected data. 13 . A method comprising: performing, for each member Common Depth Point (CDP) gather of a set of CDP gathers along a sail line of a first marine survey, a series of steps comprising: performing migration on a member Common Depth Point (CDP) gather using a reference velocity to create a first member Normal MoveOut (NMO) data comprising a plurality of traces; and determining a member estimated velocity that makes travel time represented in the traces of the first member NMO data substantially the same; filtering the member estimated velocities to determine a final estimated velocity; calculating a zero-offset time shift representing a difference in travel time as between the reference

Assignees

Inventors

Classifications

  • Dynamic changes in statics, e.g. sea waves or tidal influences · CPC title

  • for determining velocity profiles or travel times · CPC title

  • Velocity; travel time · CPC title

  • G01V1/362Primary

    Effecting static or dynamic corrections; Stacking · CPC title

  • Move-out correction · CPC title

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What does patent US2016178773A1 cover?
At least some of the example embodiments are methods including: performing Normal MoveOut (NMO) correction on a first Common Depth Point (CDP) gather, the NMO correction based on a reference velocity of sound in water, the NMO correction creates first NMO data with a plurality of traces; selecting a first estimated velocity that makes travel time represented in the traces substantially the same…
Who is the assignee on this patent?
Pgs Geophysical As
What technology area does this patent fall under?
Primary CPC classification G01V1/362. Mapped technology areas include Physics.
When was this patent published?
Publication date Thu Jun 23 2016 00:00:00 GMT+0000 (Coordinated Universal Time) (A1). Legal status and post-grant events are not shown on this page.
What related patents are in patentsdb?
We list 8 related publications on this page (citations in our corpus or others sharing the same primary CPC).