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Spring 2007
Series

Elements of seismic data processing
Wendy Ohlhauser
March 13 or 15 more info

Curvature and coherence attributes – a definite aid in seismic interpretation
Satinder Chopra
March 20 or 29 more info

Structural processing needs tender loving care (TLC)
Dan Negut
April 10 or 12 more info

Spectral decomposition applications beyond the seismic bandwidth
Satinder Chopra
April 17 or 19 more info

Reliable deterministic inversion of Athabasca oil sand reservoir heterogeneity
Yong Xu
April 24
more info

Wave Equation Summation (WESUM) for prestack time and depth migration Jianhua Pan & Dan Negut
May 1 or 3

AVO data preparation and conditioning
Yong Xu
May 8 or 10 more info

To RSVP for any of the above seminars,
click here.

For more information contact Florence
at 781-1437.

www.arcis.com

Lunch and Learn Seminars
Spring 2007

Wave Equation Summation (WESUM) for Prestack time and depth migration

Presented by Jianhua Pan & Dan Negut
May 1st or 3rd
11:45 to 1 pm (lunch provided)
Suite 2600, 111 - 5th Ave SW, East Petro-Canada Tower
Limited seating, click here to RSVP

This is the sixth in a series of lunch & learn seminars, see the sidebar for information on the other topics.

Wave Equation Prestack Depth Migration (WEM) has been used in the seismic industry for several years. Its ability to handle multiple arrivals from a surface position to subsurface point provides us with higher quality images than Kirchhoff migration. However, apart from computational efficiency, WEM lacks some other advantages of Kirchhoff migration such as the flexibility and the option to output surface-offset-indexed common image gathers (CIGs) which can be used for offset-domain migration velocity analysis and AVO analysis.

We have developed a wave-field extrapolation approach which is able to handle multiple arrivals and has both the flexibility and the ability to output surface-offset-indexed CIGs. We call this approach Wave Equation Summation (WESUM). In most cases, WESUM generates better images than shot profile migration.

Moreover, WESUM can be used for running prestack time migration with rms velocity as opposed to running wave equation migration using interval velocity. Just as in Kirchhoff prestack time migration, the image at one point is only related to the rms velocity at that point, it is possible to use WESUM to perform prestack time migration velocity analysis. The image quality with WESUM, of course, is better than the one from Kirchhoff migration.

To learn more, attend the lunch & learn session on May 1 or May 3. Click here to RSVP.

This course is available as a free in-house seminar. For more information contact Florence Janzen, 781-1437 or email fjanzen@arcis.com.