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Fall 2006
Series

Curvature and coherence attributes – a definite aid in seismic interpretation Satinder Chopra
Sept 26 or 28 more info

Spectral decomposition applications beyond the seismic bandwidth
Satinder Chopra
Oct 10 or 11
more info

Wave Equation Summation (WESUM) for prestack time and depth migration Jianhua Pan
Oct 17 or 19

Reliable deterministic inversion of Athabasca oil sand reservoir heterogeneity
Yong Xu
Oct 24 or 25
more info

Elements of seismic
Wendy Ohlhauser
Oct 31 or Nov 2
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
Fall 2006

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

Presented by Jianhua Pan
October 17th or 19
th, 2006

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 third 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 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 October 17 or October 19. 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.