Tomographic inversion Velocity determination with CRS attributes: - - PowerPoint PPT Presentation

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Tomographic inversion Velocity determination with CRS attributes: - - PowerPoint PPT Presentation

CO 2 CRS: Tomography T. Klver & J. Mann Introduction Tomographic inversion Velocity determination with CRS attributes: NIP waves & velocities CRS tomography Inversion procedure data extraction and preconditioning First example


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SLIDE 1

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Tomographic inversion with CRS attributes: data extraction and preconditioning

Tilman Klüver and Jürgen Mann

Geophysical Institute, University of Karlsruhe (TH) 09/22/2006

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SLIDE 2

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Overview

Introduction Velocity determination with 3D CRS attributes Attribute preconditioning and extraction Synthetic data example Conclusions Acknowledgments

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SLIDE 3

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Introduction

Construction of a background/migration velocity model is one of the key aims of seismic imaging schemes.

◮ Problems with conventional reflection tomography:

identifying and picking events in the prestack data

◮ 3D velocity models for depth imaging ◮ Tomographic approach based on CRS stack results ◮ Advantages:

◮ picking in simulated ZO volume of high S/N ratio ◮ pick locations independent of each other ◮ very few picks required

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SLIDE 4

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

NIP waves and velocities

ξ ξ ξ

p ξ ξ ξ NIP , , T , ) ( Mh

CRS attributes Mh and pξ at (t0,ξ ξ ξ) describe second-order traveltime approximation of emerging NIP wave.

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SLIDE 5

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

NIP waves and velocities

ξ ξ ξ

p ξ ξ ξ NIP , , T , ) ( Mh

In consistent velocity models, NIP waves focus at zero traveltime.

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SLIDE 6

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Tomography with CRS attributes

Find a velocity model in which all considered NIP waves, described by kinematic wavefield attributes, are correctly modeled. For tomographic inversion in 3D, one azimuth φ of Mh is required: Mφ. For multi-azimuth data the full Matrix Mh is to be preferred.

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SLIDE 7

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

3D tomography with CRS attributes

Data and model components

ξ ξ ξ ξ

(p ,p )

x y y x

(e ,e ) (ξ ,ξ )

τ

v(x,y,z)

x y

NIP (x,y,z) M

Data: (τ, M11, M12, M22, pξx, pξy, ξx, ξy)i τ = t0/2 Model: (x, y, z, ex, ey)i, vjkl vjkl: B-spline coefficients

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SLIDE 8

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion procedure

◮ nonlinear least-squares problem:

◮ iterative solution, local linearization ◮ τ, pξx , pξy , ξx, ξy

from kinematic ray tracing

◮ Mh = DB−1 from dynamic ray-tracing:

T =

  • A

B C D

  • propagator matrix in Cartesian coordinates

◮ model update ∆m: least-squares solution of

F∆m = ∆d

◮ calculation of Fréchet derivatives (matrix F):

ray perturbation theory

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SLIDE 9

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Regularization/additional constraints

Regularization:

◮ minimization of second derivatives of velocity

(spatially dependent) Additional constraints:

◮ v(x,y,z) values at arbitrary locations (x,y,z) ◮ force velocity structure to follow local reflector

structure

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SLIDE 10

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Synthetic example: forward modeled attributes

Model description:

◮ 9×9×9 = 729 B-spline knots ◮ horizontal spacing: 500 m ◮ vertical spacing: 400 m ◮ 1008 NIP-locations used to model the input data ◮ initial ray direction follows local velocity gradient

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SLIDE 11

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

True model

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=0m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=2000m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=4000m

Inversion result

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=0m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=2000m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=4000m

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SLIDE 12

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Difference

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m]

  • 300
  • 200
  • 100

100 200 300 velocity [m/s]

x=0m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m]

  • 300
  • 200
  • 100

100 200 300 velocity [m/s]

x=2000m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m]

  • 300
  • 200
  • 100

100 200 300 velocity [m/s]

x=4000m

Inversion result

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=0m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=2000m

1000 2000 3000 z [m] 1000 2000 3000 4000 5000 y [m] 1500 2000 2500 3000 3500 4000 4500 velocity [m/s]

x=4000m

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SLIDE 13

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Motivation

CRS attributes have characteristic features:

◮ they should be constant along the wavelet ◮ they should vary smoothly along the event

However, in practice

◮ unphysical fluctuations ◮ outliers ◮ possibly not locally coherent

Thus

◮ event-consistent smoothing ◮ identification of valid pick locations

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SLIDE 14

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

The event-aligned volume

✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✁ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✂ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄ ✄

midpoint x midpoint y x0 t 0 y p 2 time smoothing box seismic event

slide-15
SLIDE 15

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Event-consistent smoothing

For each zero-offset sample and CRS-parameter

◮ align smoothing volume with reflection event using

first traveltime derivatives

◮ reject samples below user-defined coherence

threshold

◮ reject samples with dip difference beyond

user-defined threshold

➥ avoid mixing of events

◮ apply combined filter:

◮ median filter ➥ remove outliers ◮ averaging ➥ remove fluctuations

◮ assign result to zero-offset sample

slide-16
SLIDE 16

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Automated attribute extraction

For each selected trace

◮ search (next) coherence maximum ◮ get nearest maximum of stack envelope ◮ align volume with reflection event using first

traveltime derivatives

◮ reject pick if user-defined percentage of all samples

inside the volume

◮ is below a given coherence threshold or ◮ has a dip difference exceeding a given threshold

◮ or if amplitude is below a user-defined threshold

➥ prefer high-energy events

◮ continue on selected trace

slide-17
SLIDE 17

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Synthetic data example

1 2 3 4 z [km] 2 4 6 8 10 12 x [km] 2200 2300 2400 2500 2600 2700 2800 2900 3000 3100

interval velocity [m/s] model at y = 5000 m

slide-18
SLIDE 18

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Synthetic data example

1 2 3 4 z [km] 2 3 4 5 6 y [km] 2200 2300 2400 2500 2600 2700 2800 2900 3000 3100

interval velocity [m/s] model at x = 5000 m

slide-19
SLIDE 19

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

CRS-stacked volume

1 2 3 t [s] 2 4 6 8 10 12 x [km]

inline section at y = 5000 m

slide-20
SLIDE 20

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

CRS-stacked volume

1 2 3 t [s] 2 4 6 8 y [km]

crossline section at x = 5000 m

slide-21
SLIDE 21

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Automatically picked ZO locations

2000 4000 6000 8000 10000 12000 14000 1000 3000 5000 7000 2 1.8 1.6 1.4 1.2 1 0.8 0.6 0.4 0.2 t [s] picked ZO locations x [m] y [m]

p and M available for all picks

slide-22
SLIDE 22

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion result (1)

1 2 3 z [km] 2 4 6 8 10 12 x [km] 2200 2300 2400 2500 2600 2700 2800 2900 3000

reconstructed velocity [m/s] model at y = 5000 m

slide-23
SLIDE 23

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion result (1)

1 2 3 z [km] 2 3 4 5 6 y [km] 2200 2300 2400 2500 2600 2700 2800 2900 3000

reconstructed velocity [m/s] model at x = 5000 m

slide-24
SLIDE 24

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion result (2)

Reconstructed NIPs Nearest true NIPs 2000 4000 6000 8000 10000 12000 x [m] 3000 4000 5000 6000 7000 y [m]

  • 4500
  • 4000
  • 3500
  • 3000
  • 2500
  • 2000
  • 1500
  • 1000
  • 500

z [m]

full 3D view

slide-25
SLIDE 25

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion result (2)

  • 4000
  • 3500
  • 3000
  • 2500
  • 2000
  • 1500
  • 1000

2000 4000 6000 8000 10000 12000 z [m] x [m] Reconstructed NIPs Nearest true NIPs

inline view at 4000 < y < 4300 m

slide-26
SLIDE 26

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Inversion result (2)

  • 4000
  • 3500
  • 3000
  • 2500
  • 2000
  • 1500
  • 1000

3000 4000 5000 6000 7000 z [m] y [m] Reconstructed NIPs Nearest true NIPs

crossline view at 8000 < x < 8300 m

slide-27
SLIDE 27

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Conclusions

◮ 3D tomographic inversion based on CRS attributes ◮ Advantages:

◮ very few picks are required ◮ automated smoothing of attributes ◮ automated picking in ZO volume ◮ no assumptions about reflector continuity ◮ smooth velocity model (ideal for ray tracing)

◮ Limitations:

◮ smooth velocity description must be valid ◮ limited lateral variation within CRS apertures

(approximately hyperbolic traveltimes)

slide-28
SLIDE 28

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

Acknowledgments

This work was kindly supported by the Federal Ministry

  • f Education and Research (BMBF), Germany, and the

sponsors of the Wave Inversion Technology (WIT) consortium. Contributors: Miriam Spinner: model building, acquisition design, and forward-modelling with NORSAR Nils-Alexander Müller: 3D CRS stack processing

slide-29
SLIDE 29

CO2CRS: Tomography

  • T. Klüver & J. Mann

Introduction Velocity determination NIP waves & velocities CRS tomography Inversion procedure First example

  • Preconditioning. . .

Basics Smoothing Extraction Data example Conclusions Acknowledgments

.