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The Fallacy of Simple Geology: a Case for Depth Imaging All Previous Hit3-DNext Hit Data

Young, John A.1
1 Data Processing, WesternGeco, Denver, CO.

Previous HitPrestackNext Hit Previous HittimeNext Hit Previous HitmigrationNext Hit been accepted by the industry as standard Previous Hit3-DNext Hit seismic processing practice. This has lead to improved imaging in many areas and the ability to use Previous Hit3-DNext Hit seismic data for AVO, Previous HitprestackNext Hit inversion, and other advanced prospecting methods. Refinements such as ray tracing, and the incorporation of anisotropic parameters have provided further improvements in Previous HittimeNext Hit imaging. Despite these in-novations, Previous HittimeNext Hit Previous HitmigrationNext Hit is inherently unable to properly handle lateral velocity variations, limiting its effectiveness for accurate imaging. Previous HitPrestackNext Hit depth Previous HitmigrationNext Hit addresses these shortcomings.

Previous HitPrestackNext Hit depth Previous HitmigrationNext Hit has been used extensively to resolve imaging problems in areas where strong lateral velocity contrasts are caused by salt bodies or complex structural geology. However, the method has been under-utilized in areas of lower structural relief, and “simple” velocity regimes where the limita-tions of Previous HittimeNext Hit imaging can be less obvious. The combination of high-resolution gridded tomography and Previous HitprestackNext Hit depth Previous HitmigrationTop can resolve the local velocity contrasts that distort the subtle structural re-sponse and compromise seismic attributes. Various examples illustrate the uplift provided by depth im-aging. Case studies include data from the Rocky Mountains, the Eastern U.S., South Texas, and a do-mestic resource play where fracture detection and fault avoidance are critical.


AAPG Search and Discovery Article #90090©2009 AAPG Annual Convention and Exhibition, Denver, Colorado, June 7-10, 2009