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Brackin A Smith

from Katy, TX
Age ~60

Brackin Smith Phones & Addresses

  • 19 Wyndehaven Lakes Dr, Katy, TX 77494 (281) 693-1473
  • 2911 Zachary Bend Ln, Katy, TX 77494 (281) 693-1473
  • College Station, TX
  • Gulf Shores, AL
  • Bartlesville, OK
  • Briggs, TX

Work

Company: Conocophillips Sep 2013 Position: Geophysics coordinator

Education

Degree: Doctorates, Doctor of Philosophy School / High School: The University of Texas at Austin 1986 to 1991 Specialities: Physics

Skills

Seismology • Geophysics • Reservoir Management • Petrophysics • Petroleum Geology • Field Development • Seismic Imaging • Petroleum • Structural Geology • Geology • Earth Science • Drilling • Mineral Exploration • Upstream • Modeling • Unconventional

Interests

Education

Industries

Oil & Energy

Resumes

Resumes

Brackin Smith Photo 1

Geophysics Coordinator

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Location:
Katy, TX
Industry:
Oil & Energy
Work:
Conocophillips
Geophysics Coordinator

Conocophillips Nov 2002 - Sep 2009
Team Lead, Time-Lapse Seismic

Conocophillips Nov 2002 - Sep 2009
Staff Geophysicist - Gulf of Mexico Development

Conocophillips Jul 1998 - Nov 2002
Geophysicist

Conocophillips Mar 1991 - Jul 1998
Research Geophysicist
Education:
The University of Texas at Austin 1986 - 1991
Doctorates, Doctor of Philosophy, Physics
Auburn University 1983 - 1986
Bachelors, Bachelor of Science, Physics
Skills:
Seismology
Geophysics
Reservoir Management
Petrophysics
Petroleum Geology
Field Development
Seismic Imaging
Petroleum
Structural Geology
Geology
Earth Science
Drilling
Mineral Exploration
Upstream
Modeling
Unconventional
Interests:
Education

Publications

Us Patents

Method And Apparatus For Migration By Finite Differences

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US Patent:
59994886, Dec 7, 1999
Filed:
Apr 27, 1998
Appl. No.:
9/067650
Inventors:
Brackin A. Smith - Bartlesville OK
Assignee:
Phillips Petroleum Company - Bartlesville OK
International Classification:
G01V 128
US Classification:
367 50
Abstract:
An improved method for eliminating reflections from artificial model boundaries encountered in finite-difference acoustic wave propagation computations is based on applying two different boundary conditions at the artificial boundary. In this method one boundary condition generates reflections having the same polarity as the incident acoustic wave, and the other boundary condition generates reflections with opposite polarity. To apply the improved method simply compute both boundary conditions on a small narrow region adjacent the artificial boundary on a separate set of grids and average the two solutions.
Brackin A Smith from Katy, TX, age ~60 Get Report