Source-free Converted-wave RTM using Acoustic...
Transcript of Source-free Converted-wave RTM using Acoustic...
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Source-free Converted-wave RTM
using Acoustic Propagators
Yue Du
Co-Authors: Yunyue Elita Li, Jizhong Yang, Arthur Cheng, Xinding Fang
May 2018
Singapore Geophysics Project
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Introduction: What is source-free?
Source Receivers
R(t)p
S(t)p
Reverse Time Migration (RTM)
Backward propagate
Receiver wavefieldI=0đ
*Forward propagate
source wavefield
Conventional PP image condition
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R(t)s
Backward propagate
S Receiver wavefieldI=0đ
*Backward propagate
P Receiver wavefield
SFCW image condition
(Shabelansky et al., 2017)
\PS
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Motivation: Velocity imprints by elastic propagator !
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Elastic Propagator Acoustic Propagator
? ? ?
Use a wrong
velocity model to
back propagate
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SFCW Image
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Outline
âTheoretical basis⢠New set of elastic wave equations
⢠Imaging as an inverse problem
âNumerical examples⢠Acoustic propagator v.s. Elastic propagator
⢠SFCW applications in surface seismic and VSP
âSummary
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Outline
âTheoretical basis⢠New set of elastic wave equations
⢠Imaging as an inverse problem
âNumerical examples⢠Acoustic propagator v.s. Elastic propagator
⢠SFCW applications in surface seismic and VSP
âSummary
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New set of elastic wave equations
P- and S-
potential
Propagation
Equation:
PP at ÎVp PP at ÎVs SP at ÎVs
SS at ÎVs PS at ÎVs
Converted-wave
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â New set of equations: coupled but separated for P- and S-
propagations in heterogeneous (LamĂŠ) media (constant density).
â âIn-situâ mode conversion happens at S-wave discontinuities.
Source term
u: particle displacement
(Li et al., 2018)
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SFCW imaging condition
â The gradients/images for converted-wave:
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⢠Match the modeled S-wave data ds with the recorded S-wave data ds0
Backward propagate
Receiver wavefieldI=0
đ*
Forward propagate
source wavefield
Conventional PS image condition
Backward propagate
S Receiver wavefieldI=0đ
*Backward propagate
P Receiver wavefield
SFCW image condition
and are propagation operators.
Singapore Geophysics Project
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Outline
âTheoretical basis⢠New set of elastic wave equations
⢠Imaging as an inverse problem
âNumerical examples⢠Acoustic propagator v.s. Elastic propagator
⢠SFCW applications in surface seismic and VSP
âSummary
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4-layer example
P S
Simulated Elastic Data: i.e. source x = 0m
(Removed direct arrival)
Vp_scatter = 5000 m/s;
Vs_scatter = 2500 m/s
PP1
PP2
PP3 PS2
PS3
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4-layer example: RTM images
Receiver spacing: 5m
Source spacing: 50m
Acoustic Propagator
Elastic Propagator
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PS Image SFCW Image
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Degradation of SFCW images
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Snapshot at early T
PP1PP2
PP3
PS2
PS3
PP1
PP2
PP3
PS2
PS3
Snapshot at late T
SFCW Image for S0
1. Degraded resolution because of the narrow angle range between PP and PS-waves.
2. Strong artifacts due to the cross-talk of PP and PS-waves from different reflectors.
θ
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? ? ?
Use a wrong velocity model to back propagate
Singapore Geophysics Project
Elastic Propagator Acoustic Propagator
SFCW Image
Motivation: Velocity imprints by elastic propagator !
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Velocity imprints by Vs scatter
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Acoustic
Propagator
PS ImagePP Image
Elastic
Propagator
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SFCW Image
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Velocity imprints by Vs scatter
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SS from vertical-scatter
PS from vertical-
scatter
PP from vertical-
scatter
Back propagated P wavefield
Acoustic
Propagator
Back propagated P wavefield
Back propagated S wavefield
Back propagated S wavefield
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SFCW Image
Elastic
Propagator
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Outline
âTheoretical basis⢠New set of elastic wave equations
⢠Imaging as an inverse problem
âNumerical examples⢠Acoustic propagator v.s. Elastic propagator
⢠SFCW applications in surface seismic and VSP
âSummary
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Mamoursi: Smooth velocity model
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Acoustic
Propagator
SFCW Image Conventional PS Image
Elastic
Propagator
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? ? ?
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Acoustic
Propagator
SFCW Image Conventional PS Image
Elastic
Propagator
Mamoursi: Rough velocity model
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Application for VSP
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PP Image
? ? ? ? ? ?
Avoid uncertain overburden structure
S(t)p
PS Image SFCW Image
R(t)s
R(t)p
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Application for VSP
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PP Image
A part of SEAM model
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PS Image SFCW Image
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Avoid
uncertain
overburden
structure
Wrong shallow layer velocity
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Application for VSP
PP Image
A part of SEAM model
PS Image SFCW Image
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Summary
â˘This work provides a rigorous theoretical basis for the SFCW image conditions from the new set of elastic wave equations.
â˘Degradation of SFCW images:
⢠Low resolution & Strong artifacts
⢠Elastic propagator issue:
⢠Imprints of S-wave velocity model â âin-situâ mode conversions.
⢠The SFCW image may not be beneficial to use in surface seismic. However, we can apply it for VSP to avoid uncertain overburden structure and image the target around wellbore.
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Thank you!
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