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:
Dec. 31, 2019

Filed:

Oct. 20, 2015
Applicants:

Tetyana Vdovina, Spring, TX (US);

Valeriy Brytik, Houston, TX (US);

John E. Anderson, Houston, TX (US);

Thomas A. Dickens, Houston, TX (US);

William Curry, Houston, TX (US);

Carey M. Marcinkovich, The Woodlands, TX (US);

Inventors:

Tetyana Vdovina, Spring, TX (US);

Valeriy Brytik, Houston, TX (US);

John E. Anderson, Houston, TX (US);

Thomas A. Dickens, Houston, TX (US);

William Curry, Houston, TX (US);

Carey M. Marcinkovich, The Woodlands, TX (US);

Assignee:
Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G01V 1/28 (2006.01); G01V 1/30 (2006.01); G06F 17/50 (2006.01);
U.S. Cl.
CPC ...
G01V 1/282 (2013.01); G01V 1/30 (2013.01); G01V 2210/30 (2013.01); G01V 2210/50 (2013.01); G01V 2210/614 (2013.01); G01V 2210/626 (2013.01); G01V 2210/67 (2013.01); G06F 17/5009 (2013.01); G06F 2217/16 (2013.01);
Abstract

A method for exploring for hydrocarbons, including: simulating a seismic waveform, using a computer, wherein computations are performed on a computational grid representing a subsurface region, said computational grid using perfectly matched layer (PML) boundary conditions that use an energy dissipation operator to minimize non-physical wave reflections at grid boundaries; wherein, in the simulation, the PML boundary conditions are defined to reduce computational instabilities at a boundary by steps including, representing direction of energy propagation by a Poynting vector, and dissipating energy, with the dissipation operator, in a direction of energy propagation instead of in a phase velocity direction; and using the simulated waveform in performing full waveform inversion or reverse time migration of seismic data, and using a physical property model from the inversion or a subsurface image from the migration to explore for hydrocarbons.


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