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:
Apr. 12, 2011

Filed:

Aug. 19, 2005
Applicants:

John C. Van Wagoner, Houston, TX (US);

Paul A. Dunn, Houston, TX (US);

Max Deffenbaugh, Califon, NJ (US);

David N. Awwiller, Houston, TX (US);

Tao Sun, Missouri City, TX (US);

Dachang LI, Katy, TX (US);

David C. Hoyal, Houston, TX (US);

Chris J. Donofrio, The Woodlands, TX (US);

Inventors:

John C. Van Wagoner, Houston, TX (US);

Paul A. Dunn, Houston, TX (US);

Max Deffenbaugh, Califon, NJ (US);

David N. Awwiller, Houston, TX (US);

Tao Sun, Missouri City, TX (US);

Dachang Li, Katy, TX (US);

David C. Hoyal, Houston, TX (US);

Chris J. Donofrio, The Woodlands, TX (US);

Assignee:

Other;

Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G06G 7/48 (2006.01);
U.S. Cl.
CPC ...
Abstract

A method is disclosed for using a three-dimensional seismic image of a subsurface earth volume to construct a geologic model specifying the spatially-varying grain size distribution, porosity, and permeability throughout the volume. The method applies to earth volumes composed of water-lain clastic sedimentary deposits and involves, in one embodiment, (a) identifying the outline forms of geologic bodies in geologic data; (b) using the outline forms of the geologic bodies to determine the spatially-varying grain size distribution within the bodies, guided by assumptions about the nature and behavior of the paleoflow that deposited the bodies; (c) determining rock properties such as, porosity and permeability within the geologic bodies based on grain-size distribution, mineralogy and burial history information.


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