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:
Jun. 27, 2006

Filed:

Dec. 14, 2001
Applicants:

Douglas Francis Goff, Danville, CA (US);

Luc Vincent, Palo Alto, CA (US);

Kevin L. Deal, Houston, TX (US);

William S. Kowalik, La Habra Heights, CA (US);

Sebastien Bombarde, Oakland, CA (US);

Sandra Lee, Danville, CA (US);

William R. Volz, Katy, TX (US);

Richard C. Jones, Fullerton, CA (US);

Inventors:

Douglas Francis Goff, Danville, CA (US);

Luc Vincent, Palo Alto, CA (US);

Kevin L. Deal, Houston, TX (US);

William S. Kowalik, La Habra Heights, CA (US);

Sebastien Bombarde, Oakland, CA (US);

Sandra Lee, Danville, CA (US);

William R. Volz, Katy, TX (US);

Richard C. Jones, Fullerton, CA (US);

Assignee:

Chevron U.S.A. Inc., San Ramon, CA (US);

Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G01V 1/28 (2006.01);
U.S. Cl.
CPC ...
Abstract

A computer implemented method for interpreting faults from a fault-enhanced 3-D seismic attribute cube. The method includes the steps of extracting faults from a 3-D seismic attribute cube, and of calculating a minimum path value for each voxel of the 3-D seismic attribute cube. A fault network skeleton is extracted from the 3-D seismic attribute cube by utilizing the minimum path values which correspond to voxels within the 3-D seismic attribute cube. The individual fault networks are then labeled, and a vector description of the fault network skeleton is created. The fault network skeleton is subdivided into individual fault patches wherein the individual fault patches are the smallest, non-intersecting, non-bifurcating patches that lie on only one geologic fault. The individual fault patches are then correlated into a representation of geologic faults.


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