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

Transcript of Source-free Converted-wave RTM using Acoustic...

  • 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

  • Introduction: What is source-free?

    Source Receivers

    R(t)p

    S(t)p

    Reverse Time Migration (RTM)

    Backward propagate

    Receiver wavefieldI=0𝑇

    *Forward propagate

    source wavefield

    Conventional PP image condition

    2

    R(t)s

    Backward propagate

    S Receiver wavefieldI=0𝑇

    *Backward propagate

    P Receiver wavefield

    SFCW image condition

    (Shabelansky et al., 2017)

    \PS

    Singapore Geophysics Project

  • Motivation: Velocity imprints by elastic propagator !

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    Elastic Propagator Acoustic Propagator

    ? ? ?

    Use a wrong

    velocity model to

    back propagate

    Singapore Geophysics Project

    SFCW Image

  • Outline

    ❖Theoretical basis• New set of elastic wave equations

    • Imaging as an inverse problem

    ❖Numerical examples• Acoustic propagator v.s. Elastic propagator

    • SFCW applications in surface seismic and VSP

    ❖Summary

    4Singapore Geophysics Project

  • Outline

    ❖Theoretical basis• New set of elastic wave equations

    • Imaging as an inverse problem

    ❖Numerical examples• Acoustic propagator v.s. Elastic propagator

    • SFCW applications in surface seismic and VSP

    ❖Summary

    5Singapore Geophysics Project

  • New set of elastic wave equations

    P- and S-

    potential

    Propagation

    Equation:

    PP at ΔVp PP at ΔVs SP at ΔVs

    SS at ΔVs PS at ΔVs

    Converted-wave

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    ✓ New set of equations: coupled but separated for P- and S-

    propagations in heterogeneous (LamĂŠ) media (constant density).

    ✓ “In-situ” mode conversion happens at S-wave discontinuities.

    Source term

    u: particle displacement

    (Li et al., 2018)

    Singapore Geophysics Project

  • SFCW imaging condition

    ✓ 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

    𝑇*

    Forward propagate

    source wavefield

    Conventional PS image condition

    Backward propagate

    S Receiver wavefieldI=0𝑇

    *Backward propagate

    P Receiver wavefield

    SFCW image condition

    and are propagation operators.

    Singapore Geophysics Project

    ≈

  • Outline

    ❖Theoretical basis• New set of elastic wave equations

    • Imaging as an inverse problem

    ❖Numerical examples• Acoustic propagator v.s. Elastic propagator

    • SFCW applications in surface seismic and VSP

    ❖Summary

    8Singapore Geophysics Project

  • 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

    8Singapore Geophysics Project

  • 4-layer example: RTM images

    Receiver spacing: 5m

    Source spacing: 50m

    Acoustic Propagator

    Elastic Propagator

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    PS Image SFCW Image

    Singapore Geophysics Project

  • 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

    Singapore Geophysics Project

  • 12

    ? ? ?

    Use a wrong velocity model to back propagate

    Singapore Geophysics Project

    Elastic Propagator Acoustic Propagator

    SFCW Image

    Motivation: Velocity imprints by elastic propagator !

  • Velocity imprints by Vs scatter

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    Acoustic

    Propagator

    PS ImagePP Image

    Elastic

    Propagator

    Singapore Geophysics Project

    SFCW Image

  • 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

    Singapore Geophysics Project

    SFCW Image

    Elastic

    Propagator

  • Outline

    ❖Theoretical basis• New set of elastic wave equations

    • Imaging as an inverse problem

    ❖Numerical examples• Acoustic propagator v.s. Elastic propagator

    • SFCW applications in surface seismic and VSP

    ❖Summary

    15Singapore Geophysics Project

  • Mamoursi: Smooth velocity model

    16Singapore Geophysics Project

    Acoustic

    Propagator

    SFCW Image Conventional PS Image

    Elastic

    Propagator

  • 17

    ? ? ?

    Singapore Geophysics Project

    Acoustic

    Propagator

    SFCW Image Conventional PS Image

    Elastic

    Propagator

    Mamoursi: Rough velocity model

  • 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

    Singapore Geophysics Project

  • Application for VSP

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    PP Image

    A part of SEAM model

    Singapore Geophysics Project

    PS Image SFCW Image

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    Avoid

    uncertain

    overburden

    structure

    Wrong shallow layer velocity

    Singapore Geophysics Project

    Application for VSP

    PP Image

    A part of SEAM model

    PS Image SFCW Image

  • Summary

    ➢This work provides a rigorous theoretical basis for the SFCW image conditions from the new set of elastic wave equations.

    ➢Degradation of SFCW images:

    • Low resolution & Strong artifacts

    ➢ Elastic propagator issue:

    • Imprints of S-wave velocity model – “in-situ” 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.

    21Singapore Geophysics Project

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    Thank you!

    Singapore Geophysics Project