The patent badge is an abbreviated version of the USPTO patent document. The patent badge does contain a link to the full patent document.

The patent badge is an abbreviated version of the USPTO patent document. The patent badge covers the following: Patent number, Date patent was issued, Date patent was filed, Title of the patent, Applicant, Inventor, Assignee, Attorney firm, Primary examiner, Assistant examiner, CPCs, and Abstract. The patent badge does contain a link to the full patent document (in Adobe Acrobat format, aka pdf). To download or print any patent click here.

Date of Patent:
Aug. 17, 2021

Filed:

Sep. 21, 2018
Applicant:

Pgs Geophysical As, Lysaker, NO;

Inventors:

Shaoping Lu, Houston, TX (US);

Faqi Liu, Katy, TX (US);

Alejandro A. Valenciano Mavilio, Bellaire, TX (US);

Nizar Chemingui, Houston, TX (US);

Assignee:

PGS Geophysical AS, Oslo, NO;

Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G01V 1/34 (2006.01); G01V 1/38 (2006.01); G01V 1/36 (2006.01); G01V 1/30 (2006.01); G01V 1/28 (2006.01);
U.S. Cl.
CPC ...
G01V 1/345 (2013.01); G01V 1/28 (2013.01); G01V 1/303 (2013.01); G01V 1/362 (2013.01); G01V 1/38 (2013.01); G01V 2210/32 (2013.01); G01V 2210/44 (2013.01); G01V 2210/51 (2013.01);
Abstract

This disclosure describes processes and systems for generating a seismic image of a subterranean formation from recorded seismic data gathers obtained in a marine seismic survey of the subterranean formation. The seismic data comprises recorded pressure and vertical velocity wavefields that are used to separate the recorded pressure wavefield into upgoing and downgoing pressure wavefields. A seismic image is computed from the subterranean formation based on a product of the downgoing pressure wavefield and a migration operator applied to the upgoing pressure wavefield. The downgoing pressure wavefield is a boundary source wavefield and the upgoing pressure wavefield is boundary receiver wavefield of the migration operator. The seismic image is iteratively updated by computing a residual seismic image based on the upgoing pressure wavefield and adding the residual seismic image to the seismic image. The final seismic image displays increased illumination and reduced crosstalk artifacts compared to conventional seismic imaging techniques.


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