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. 14, 2022

Filed:

Mar. 01, 2019
Applicant:

Acoustic Zoom, Inc., Paradise, CA;

Inventors:

Jacques Y. Guigné, Paradise, CA;

Adam Gogacz, St. John's, CA;

Assignee:

Acoustic Zoom, Inc., Paradise, CA;

Attorney:
Primary Examiner:
Int. Cl.
CPC ...
G01V 1/30 (2006.01); G01V 1/28 (2006.01); E21B 49/00 (2006.01); G01V 1/34 (2006.01); E21B 7/04 (2006.01); G01V 1/42 (2006.01);
U.S. Cl.
CPC ...
G01V 1/301 (2013.01); E21B 49/00 (2013.01); G01V 1/282 (2013.01); G01V 1/306 (2013.01); G01V 1/34 (2013.01); E21B 7/04 (2013.01); G01V 1/42 (2013.01); G01V 2210/121 (2013.01); G01V 2210/1293 (2013.01); G01V 2210/1295 (2013.01); G01V 2210/1297 (2013.01); G01V 2210/1299 (2013.01); G01V 2210/1423 (2013.01); G01V 2210/1425 (2013.01); G01V 2210/1427 (2013.01); G01V 2210/1429 (2013.01); G01V 2210/161 (2013.01); G01V 2210/165 (2013.01); G01V 2210/21 (2013.01); G01V 2210/51 (2013.01); G01V 2210/55 (2013.01); G01V 2210/6169 (2013.01); G01V 2210/624 (2013.01); G01V 2210/64 (2013.01); G01V 2210/643 (2013.01); G01V 2210/74 (2013.01);
Abstract

A method for imaging non-specular seismic events as well as correlating non-specular events with physically measurable quantites in a volume of Earth's subsurface. Includes entering as input to a computer signals detected by a plurality of seismic sensors disposed above and/or within the volume in response to actuation of at least one seismic energy source above and/or within the volume. Parameter analysis is performed to populate the initial model with point-wise, best-fit wavefront travel-time approximations. Imaging is performed to obtain undifferentiated specular and non-specular representations of the volume. Specular boundaries are mapped using the imaged volume and using the boundaries to form a model of specular components of the volume. Beamforming is used to characterize seismic attributes associated with specular and non-specular reflections as separate and differentiated data sets.


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