Reverse Time Migration Reverse Time Migration. Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse.

Slides:



Advertisements
Similar presentations
Time-reversal acoustics, virtual source imaging, and seismic interferometry Haijiang Zhang University of Science and Technology of China.
Advertisements

Multi-source Least Squares Migration and Waveform Inversion
Adaptive Grid Reverse-Time Migration Yue Wang. Outline Motivation and ObjectiveMotivation and Objective Reverse Time MethodologyReverse Time Methodology.
Locating Trapped Miners Using Time Reversal Mirrors Sherif M. Hanafy Weiping CaoKim McCarter Gerard T. Schuster November 12, 2008.
Prestack Migration Deconvolution Jianxing Hu and Gerard T. Schuster University of Utah.
Imaging Multiple Reflections with Reverse- Time Migration Yue Wang University of Utah.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
IntroductionUofU TestTime ShiftSuper-stackTucson TestSuper-resolution Locating Trapped Miners Using Time Reversal Mirrors Sherif M. Hanafy Weiping CaoKim.
Wavepath Migration versus Kirchhoff Migration: 3-D Prestack Examples H. Sun and G. T. Schuster University of Utah.
Primary-Only Imaging Condition Yue Wang. Outline Objective Objective POIC Methodology POIC Methodology Synthetic Data Tests Synthetic Data Tests 5-layer.
Reverse-Time Migration By A Variable Grid-Size And Time-Step Method Yue Wang University of Utah.
Solving Illumination Problems Solving Illumination Problems in Imaging:Efficient RTM & in Imaging:Efficient RTM & Migration Deconvolution Migration Deconvolution.
TARGET-ORIENTED LEAST SQUARES MIGRATION Zhiyong Jiang Geology and Geophysics Department University of Utah.
Overview of Utah Tomography and Modeling/Migration (UTAM) Chaiwoot B., T. Crosby, G. Jiang, R. He, G. Schuster, Chaiwoot B., T. Crosby, G. Jiang, R. He,
Migration MigrationIntuitive Least Squares Green’s Theorem.
Kirchhoff vs Crosscorrelation
Stabilization of Migration Deconvolution Jianxing Hu University of Utah.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
Local Migration with Extrapolated VSP Green’s Functions Xiang Xiao and Gerard Schuster Univ. of Utah.
1 Fast 3D Target-Oriented Reverse Time Datuming Shuqian Dong University of Utah 2 Oct
D(r) = m(x) G(s|x) G(x|r) G(x|r) [] * * ,r,s Trial image pt x Direct wave Backpropagated traces T=0 Reverse Time Migration Generalized Kirch. Migration.
1 Local Reverse Time Migration: P-to-S Converted Wave Case Xiang Xiao and Scott Leaney UTAM, Univ. of Utah Feb. 7, 2008.
Demonstration of Super-Resolution and Super-Stacking Properties of Time Reversal Mirrors in Locating Seismic Sources Weiping Cao, Gerard T. Schuster, Ge.
Multisource Least-squares Reverse Time Migration Wei Dai.
V.2 Wavepath Migration Overview Overview Kirchhoff migration smears a reflection along a fat ellipsoid, so that most of the reflection energy is placed.
Making the Most from the Least (Squares Migration) G. Dutta, Y. Huang, W. Dai, X. Wang, and Gerard Schuster G. Dutta, Y. Huang, W. Dai, X. Wang, and Gerard.
Overview of Multisource Phase Encoded Seismic Inversion Wei Dai, Ge Zhan, and Gerard Schuster KAUST.
Superresolution Imaging with Resonance Scatterring Gerard Schuster, Yunsong Huang, and Abdullah AlTheyab King Abdullah University of Science and Technology.
Least Squares Migration of Stacked Supergathers Wei Dai and Gerard Schuster KAUST vs.
Time vs Depth Migration Insensitive to v(z) model Sensitive to v(z) model Time migration uses best fit hyperbola Depth migration uses best guess moveout.
Migration Deconvolution of 3-D Seismic Data Jianxing Hu (University of Utah) Paul Valasek (Phillips Petroleum Company)
Migration In a Nutshell Migration In a Nutshell Migration In a Nutshell D.S. Macpherson.
Prestack Migration Intuitive Least Squares Migration Green’s Theorem.
1 Local Reverse Time Migration: Salt Flank Imaging by PS Waves Xiang Xiao and Scott Leaney 1 1 Schlumberger UTAM, Univ. of Utah Feb. 8, 2008.
Moveout Correction and Migration of Surface-related Resonant Multiples Bowen Guo*,1, Yunsong Huang 2 and Gerard Schuster 1 1 King Abdullah University of.
Multisource Least-squares Migration of Marine Data Xin Wang & Gerard Schuster Nov 7, 2012.
Reverse Time Migration of Prism Waves for Salt Flank Delineation
Benefits & Limitations of Least Squares Migration W.Dai,D.Zhang,X.Wang,GTSKAUST RTM Least Squares RTM GOM RTM GOM LSRTM.
Tutorial on Green’s Functions, Forward Modeling, Reciprocity Theorems, and Interferometry..
Hydro-frac Source Estimation by Time Reversal Mirrors Weiping Cao and Chaiwoot Boonyasiriwat Feb 7, 2008.
3-D Prestack Migration Deconvolution Bob Estill ( Unocal) Jianhua Yu (University of Utah)
 = 0.5  j  r j (  kk’ (  m kk’ /  z) 2  m ii’ =  j  r j  r j /  m ii’ + (  kk’  m kk’ /  m ii’  m kk’ /  z) (1) m 11 m 12.
Reverse Time Migration Reverse Time Migration ? ?.
Fast Least Squares Migration with a Deblurring Filter 30 October 2008 Naoshi Aoki 1.
Reverse Time Migration
Interpolating and Extrapolating Marine Data with Interferometry
LSM Theory: Overdetermined vs Underdetermined
Making Marchenko imaging work with field data and the bumpy road to 3D
Zero-Offset Data d = L o ò r ) ( g = d dr r ) ( g = d
Velocity Analysis Using Surface-Seismic Primaries-Only Data Obtained Without Removing Multiples
Rigorous Derivation of LSM (& FWI)
Reverse Time Migration
Primary-Only Imaging Condition And Interferometric Migration
Making the Most from the Least (Squares Migration)
Overview of Multisource Phase Encoded Seismic Inversion
Migration Intuitive Least Squares Migration Green’s Theorem.
Non-local Means (NLM) Filter for Trim Statics
Multiple attenuation in the image space
Initial asymptotic acoustic RTM imaging results for a salt model
Summary: Lateral Resolution
I.1 Diffraction Stack Modeling
I.1 Diffraction Stack Modeling
Non-local Means (NLM) Filter for Trim Statics
Migration Resolution.
Seismic Interferometry and 3x3 Classification Matrix
Migration Resolution.
Inverse Crimes d=Lm m=L-1 d Red Sea Synthetics
Least Squares Migration
Presentation transcript:

Reverse Time Migration Reverse Time Migration

Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration Code ZO Reverse Time Migration Code Examples Examples

Liberty Park Lake Liberty Park Lake Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Find Location of Rock Find Location of Rock Rolls of Toilet Paper Time

Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration Code ZO Reverse Time Migration Code Examples Examples

ZO Modeling 1-way time Reverse Order Traces in Time 0 5

1-way time Reverse Time Migration (Go Backwards in Time) T=0 Focuses at Hand Grenades -5 0

Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration Code ZO Reverse Time Migration Code Examples Examples

1-way time Reverse Time Migration (Reverse Traces Go Forward in Time) T=0 Focuses at Hand Grenades -5 0

Poststack RTM 1. Reverse Time Order of Traces 5 1-way time Reversed Traces are Wavelets of loudspeakers

Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration Code ZO Reverse Time Migration Code Examples Examples

Forward Modeling Forward Modeling for it=1:1:nt p2 = 2*p1 - p0 + cns.*del2(p1); p2(xs,zs) = p2(xs,zs) + RICKER(it); % Add bodypoint src term p0=p1;p1=p2; end for it=nt:-1:1 p2 = 2*p1 - p0 + cns.*del2(p1); p2(1:nx,2) = p2(1:nx,2) + data(1:nx,it); % Add bodypoint src term p0=p1;p1=p2; end Reverse Time Modeling Reverse Time Modeling

Recall Forward Modeling d=Lm d(x) = G(x|x’)m(x’)dx’  ~~~~~~ Fourier d(x,t) = G(x,t-t s |x’,0)m(x’,t s )dx’dt s   = G(x,t|x’,t s )m(x’,t s )dx’dt s  Stationarity x ztsrc Forward reconstruction of half circles

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity x zt Note: t < t s t=0 t=0

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity x zt Note: t < t s t=0 t=0

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity x zt Note: t < t s t=0 t=0

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity x zt Note: t < t s t=0 t=0

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity x zt Note: t < t s Backward reconstruction of half circles t=0 t=0

Migration = Adjoint of Data d=Lm d(x) = G(x|x’)m(x’)dx’  m=L d m(x’) = G(x|x’)*d(x)dx T Fourier m(x) = G(x,-t+t s |x’,0)d(x’,t s )dx’dt s   = G(x, t s |x’,t)d(x’,t s )dx’dt s  Stationarity Note: t < t s x zt Backward reconstruction of half circles Let t s = -t s -- Note: t > t s x zt Backward reconstruction of half circles zx z t Forward prop. Of reverse time data t=0 t=0

Advantages of m(x’+dx) = d(x) G(x|x’+dx)* time time Multiples Primary Primary Kirchhoff Mig. vs Full Trace Migration 1. Low-Fold Stack vs Superstack 2. Poor Resolution vs Superresolution Multiples x

Outline Outline Finding a Rock Splash at Liberty Park Finding a Rock Splash at Liberty Park ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (backwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration (forwd in time) ZO Reverse Time Migration Code ZO Reverse Time Migration Code Examples Examples

Numerical Examples

3D Synthetic Data 3D SEG/EAGE Salt Model Z 2.0 Km X 3.5 Km Y 3.5 Km 4

Cross line 160 Depth (Km) 0 W E 3D Synthetic Data 3.5 Offset (km) Offset (km) 0 Kirchhoff Migration Redatum + KM 5

Cross line 180 Depth (Km) 0 W E 3.5 Offset (km) Offset (km) 0 Kirchhoff Migration Redatum + KM 3D Synthetic Data 6

Cross line 200 Depth (Km) 0 W E 3.5 Offset (km) Offset (km) 0 Kirchhoff Migration Redatum + KM 7

Numerical Examples GOM DataGOM Data Prism Synthetic ExamplePrism Synthetic Example

? GOM Kirchhoff

? GOM RTM

?

Numerical Examples GOM DataGOM Data Prism Synthetic ExamplePrism Synthetic Example

Prism Wave Migration One Way Migration of Prestack Data RTM of Prestack Data Courtesy TLE: Farmer et al. (2006)

Summary 1. RTM much more expensive than Kirchhoff Mig. 2. If V(x,y,z) accurate then all multiples Included so better S/N ration and better Resolution. 3. If V(x,y,z) not accurate then smooth velocity Model seems to work better. Free surface multiples included. 4. RTM worth it for salt models, not layered V(x,y,z). 5. RTM is State of art for GOM and Salt Structures.

Solution Claim: Image both Primaries and MultiplesClaim: Image both Primaries and Multiples? ?AD Methods: RTMMethods: RTM

Piecemeal Methods Assume Knowledge of Important MirrorAssume Knowledge of Important Mirror? ?AD Reverse Time MigrationReverse Time Migration 2-Way Mirror Wave Migration: