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Reverse-Time Migration For 3D SEG/EAGE Salt Model

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Presentation on theme: "Reverse-Time Migration For 3D SEG/EAGE Salt Model"— Presentation transcript:

1 Reverse-Time Migration For 3D SEG/EAGE Salt Model
Yue Wang University of Utah

2 Outline Method & Previous 2D results Result for 3D SEG/EAGE Salt Model
Conclusions & Discussions

3 2-D Salt Model Source * Geophone Line Depth (km) 2.7 4.5 Distance (km)

4 Shot Gather Reversed Phase Horizontal Vertical Pressure PS PP
Reversed Phase PS PP Receiver-Side Surface Ghost Time (s) 2 0.9 Distance (km) 3.6 0.9 Distance (km) 3.6 0.9 Distance (km) 3.6

5 How to use P & V? Key Idea: Migrate pressure and particle
velocity simultaneously by using wave-equation; Water bottom Down-going Wave Up-going Up-going Wave Down-going

6 Kirchhoff Migration Depth (km) 2.5 0.45 4.05 Distance (km)

7 Kirchhoff Migration Depth (km) 2.5 0.45 4.05 Distance (km)

8 Particle-Velocity RT Scheme
Depth (km) 2.5 0.45 4.05 Distance (km)

9 P & V RT Scheme Depth (km) 2.5 0.45 4.05 Distance (km)

10 Outline Method & Previous 2D results Result for 3D SEG/EAGE Salt Model
Conclusions & Discussions

11 3-D SEG/EAGE Salt Model Crossline Ocean-Bottom Geophone Line
Ocean-Bottom Geophone Line Depth (km) Exploding Reflector Source 2 4.5 Distance (km)

12 3-D SEG/EAGE Salt Model Direct Arrival From Ghost Reflectins
Ghost Reflectins Direct Arrival From Reflection Layer Ocean-Bottom Geophone Line Depth (km) Exploding Source 2 4.5 Distance (km)

13 3-D SEG/EAGE Salt Model Depth (km) Ocean-Bottom Geophone Line 2
Ocean-Bottom Geophone Line Depth (km) Exploding Source 2 4.5 Distance (km)

14 3-D SEG/EAGE Salt Model Ghost Reflectins Depth (km) Ocean-Bottom
Ghost Reflectins Ocean-Bottom Geophone Line Depth (km) Exploding Source 2 4.5 Distance (km)

15 Particle-Velocity RT Scheme
Depth (km) 2 4.5 Distance (km)

16 Particle-Velocity RT Scheme
Depth (km) 2 4.5 Distance (km)

17 P & V RT Scheme Depth (km) 2 4.5 Distance (km)

18 Particle-Velocity RT Scheme
Depth (km) 2 4.5 Distance (km)

19 Conclusions & Discussions
Image using both primary and ghost reflections. FD + kirchhoff hybrid scheme?

20 Acknowledgement We are grateful to the 2000 sponsors of the UTAM consortium for the financial support

21 P & V Scheme Depth (km) 2 4.5 Distance (km)

22 P & V RT Scheme Depth (km) 2 4.5 Distance (km)

23 How to use P & V? 2. Reverse-time migration using P & V:
Migrate pressure and particle velocity simultaneously by using wave-equation; Ghost is used for imaging; Non-flat water bottom; Worked on 2D Model.


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