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Seismic Interpretation Pitfalls Caused by Fresnel Effects, Anisotropic Effects, and/or Velocity Effects, and How They Influence Seismic Imaging in Time and Depth
AAPG Geophysical Integration Group
Date: Saturday, 5 April
Time: 8:00 a.m.–4:30 p.m.
Location: George R. Brown Convention Center
Instructors: Leon Thomsen (Delta Geophysics, Houston, Texas) and J. Bee Bednar (Panorama Technologies, Houston, Texas)
Fee: Professionals $380, Students $190 (limited)
Includes: Course notes (CD) and refreshments
Limit: 40 people
In increasing numbers, geologists are interpreting reflection seismic data, especially in 3-D format. But, unlike industry-trained geophysicists, they often lack basic knowledge of how Anisotrophy (the difference between velocities measured perpendicular and parallel to a bedding unit), Velocity Anomalies (near surface and mid-section) and even Fresnel zones (vertical and lateral inspection distances along a CDP trace) have upon seismic imaging in time and depth.
The course is designed for geoscientists and engineers who are, or will soon be, involved in petroleum exploration and development.
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