1. Pre-Stack Depth Migration of Dual-Azimuth Surveys Incorporating Azimuthal P-Wave Anisotropy Phil WhitfieldWesternGeco Fiona Dewey Wintershall Noordzee B.V. Malcolm KingMonarch Geophysical

2. Overview Project outline and illumination comparisons Illustration of azimuthal velocity variations Butterfly gathers 5 possible solutions Chosen workflow – dual anisotropy Results Conclusions

3. Plan view of the surveys and the salt structures Objective is to combine both azimuth datasets to improve signal to noise and to maximise the subsalt illumination

4. Standard workflow for dual-azimuth surveys INITIAL VELOCITY MODEL MIGRATE DATASET 1 RESIDUAL PICKS 1 MIGRATE DATASET 2 RESIDUAL PICKS 2 TOMOGRAPHY RAY TRACE WITH ACQUISITION AZIMUTHS NEW VELOCITY MODEL Ideal is to build a single velocity model combining information from both datasets

5. E-W datasetN-S dataset “Butterfly gathers” – dual azimuth super gathers East-West dataset fast North-South dataset fast

6. Dual-anisotropy workflow for dual-azimuth surveys INITIAL VELOCITY MODEL INCLUDING BACKGROUND ANISOTROPY MIGRATE DATASET 1 RESIDUAL PICKS 1 MIGRATE DATASET 2 RESIDUAL PICKS 2 NEW VELOCITY MODEL TOMOGRAPHY WITH WELL CONSTRAINTS BUTTERFLY GATHER ANALYSIS Analysis OK? UPDATE RESIDUAL ANISOTROPY 1 UPDATE RESIDUAL ANISOTROPY 2 Yes No

7. Butterfly gather moveout analysis Further velocity update is required No further update required – ideal moveout as shown keeps residual anisotropy positive Zero offsets don’t tie – incorrect model

8. Residual anisotropy analysis

9. Overview Project outline and illumination comparisons Illustration of azimuthal velocity variations Butterfly gathers 5 possible solutions Chosen workflow – dual anisotropy Results Conclusions

10. -2 0 2 4 6 8 10 12 14 16 18 20 Dual Anisotropy – spatially varying epsilon East-West modelNorth-South model

11. Butterfly gather results – fast East-West dataset Initial modelDual anisotropy model

12. Conclusions Dual-azimuth surveys provide enhanced illumination under complex salt Build a single velocity model if you can, BUT – Always check for azimuthal velocity variations Butterfly gathers help to show any azimuthal variations If there are azimuthal variations – Shouldn’t ignore them – Cannot combine datasets if build two independent velocity models – HTI solution is only feasible if VTI is weak Dual anisotropic models are a good pragmatic solution

13. Acknowledgements Wintershall Noordzee B.V. Energie Beheer Nederland B.V. Petro-Canada Colleagues at WesternGeco: Emmanuel Saragoussi, Peter Szabo, Richard Whitebread Chris Soufleris, Steve Horne, Phil Kitchenside, Tamara Khlussovich Sergei Tcherkashnev for Walkaway VSP analysis