Crosscorrelation Migration of Free-Surface Multiples in RVSP Data Jianming Sheng University of Utah February, 2001.

Slides:



Advertisements
Similar presentations
Geological Model Depth(km) X(km) 2001 Year.
Advertisements

First Arrival Traveltime and Waveform Inversion of Refraction Data Jianming Sheng and Gerard T. Schuster University of Utah October, 2002.
Closure Phase Statics Correction Closure Phase Statics Correction University of Utah Jianhua Yu.
Interferometric Interpolation of 3D OBS Data Weiping Cao, University of Utah Oct
Prestack Migration Deconvolution Jianxing Hu and Gerard T. Schuster University of Utah.
Imaging Multiple Reflections with Reverse- Time Migration Yue Wang University of Utah.
Finite-Frequency Resolution Limits of Traveltime Tomography for Smoothly Varying Velocity Models Jianming Sheng and Gerard T. Schuster University of Utah.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
Specular-Ray Parameter Extraction and Stationary Phase Migration Jing Chen University of Utah.
Wavepath Migration versus Kirchhoff Migration: 3-D Prestack Examples H. Sun and G. T. Schuster University of Utah.
Reduced-Time Migration of Converted Waves David Sheley and Gerard T. Schuster University of Utah.
Wave-Equation Interferometric Migration of VSP Data Ruiqing He Dept. of Geology & Geophysics University of Utah.
Wave-Equation Interferometric Migration of VSP Data Ruiqing He Dept. of Geology & Geophysics 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.
TARGET-ORIENTED LEAST SQUARES MIGRATION Zhiyong Jiang Geology and Geophysics Department University of Utah.
CROSSWELL IMAGING BY 2-D PRESTACK WAVEPATH MIGRATION
MULTIPLE PREDICTION & ATTENUATION Ruiqing He University of Utah Feb Feb
Joint Migration of Primary and Multiple Reflections in RVSP Data Jianhua Yu, Gerard T. Schuster University of Utah.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
Finite-Frequency Resolution Limits of Traveltime Tomography for Smoothly Varying Velocity Models Jianming Sheng and Gerard T. Schuster University of Utah.
Arbitrary Parameter Extraction, Stationary Phase Migration, and Tomographic Velocity Analysis Jing Chen 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 and Attenuation of Surface-Related and Interbed Multiple Reflections Zhiyong Jiang University of Utah April 21, 2006.
1 Interferometric Interpolation and Extrapolation of Sparse OBS and SSP Data Shuqian Dong and G.T.Schuster.
Kirchhoff vs Crosscorrelation
Acquisiton of Passive Seismic Data at Tooele Army Depot, Utah David Sheley, Travis Crosby, Jianming Sheng.
Autocorrelogram Migration of Drill-Bit Data Jianhua Yu, Lew Katz, Fred Followill, and Gerard T. Schuster.
Wavefield Prediction of Water-layer Multiples Ruiqing He University of Utah Oct Oct
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
LEAST-SQUARES MIGRATION OF BOTH PRIMARIES AND MULTIPLES Ruiqing He, Gerard Schuster University of Utah Oct
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
3-D PRESTACK WAVEPATH MIGRATION H. Sun Geology and Geophysics Department University of Utah.
Fresnel-zone Traveltime Tomo. for INCO and Mapleton Data Fresnel-zone Traveltime Tomo. for INCO and Mapleton Data Jianming Sheng University of Utah Feb.
Applications of Time-Domain Multiscale Waveform Tomography to Marine and Land Data C. Boonyasiriwat 1, J. Sheng 3, P. Valasek 2, P. Routh 2, B. Macy 2,
Migration Deconvolution vs Least Squares Migration Jianhua Yu, Gerard T. Schuster University of Utah.
Crosscorrelation Migration of Free-Surface Multiples in CDP Data Jianming Sheng University of Utah February, 2001.
MD + AVO Inversion Jianhua Yu, University of Utah Jianxing Hu GXT.
Virtual Source Imaging vs Interferometric Imaging Gerard T. Schuster, Andrey Bakulin and Rodney Calvert.
Interferometric Multiple Migration of UPRC Data
Reverse-Time Migration For 3D SEG/EAGE Salt Model
Autocorrelogram Migration for Field Data Generated by A Horizontal Drill-bit Source Jianhua Yu, Lew Katz Fred Followill and Gerard T. Schuster.
Demonstration of Super-Resolution and Super-Stacking Properties of Time Reversal Mirrors in Locating Seismic Sources Weiping Cao, Gerard T. Schuster, Ge.
Prestack Migration Deconvolution in Common Offset Domain Jianxing Hu University of Utah.
Multisource Least-squares Reverse Time Migration Wei Dai.
3D Wave-equation Interferometric Migration of VSP Free-surface Multiples Ruiqing He University of Utah Feb., 2006.
Topographic Phase Shift with Applications to Migration and Multiple Prediction Ruiqing He University of Utah Feb
Seeing the Invisible with Seismic Interferometry: Datuming and Migration Gerard T. Schuster, Jianhua Yu, Xiao Xiang and Jianming Sheng University of Utah.
Coherence-weighted Wavepath Migration for Teleseismic Data Coherence-weighted Wavepath Migration for Teleseismic Data J. Sheng, G. T. Schuster, K. L. Pankow,
Impact of MD on AVO Inversion
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.
Velocity Estimation of Friendswood’s Weathering Zone using Fermat’s Interferometric Principle By Chaiwoot Boonyasiriwat University of Utah.
LEAST SQUARES DATUMING AND SURFACE WAVES PREDICTION WITH INTERFEROMETRY Yanwei Xue Department of Geology & Geophysics University of Utah 1.
Super-virtual Interferometric Diffractions as Guide Stars Wei Dai 1, Tong Fei 2, Yi Luo 2 and Gerard T. Schuster 1 1 KAUST 2 Saudi Aramco Feb 9, 2012.
Interferometric Traveltime Tomography M. Zhou & G.T. Schuster Geology and Geophysics Department University of Utah.
Migration Velocity Analysis of Multi-source Data Xin Wang January 7,
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)
The Earth’s Near Surface as a Vibroseis Signal Generator Zhiyong Jiang University of Utah.
Jianhua Yu University of Utah Robust Imaging for RVSP Data with Static Errors.
Shuqian Dong and Sherif M. Hanafy February 2009 Interpolation and Extrapolation of 2D OBS Data Using Interferometry.
MD+AVO Inversion: Real Examples University of Utah Jianhua Yu.
Interpolating and Extrapolating Marine Data with Interferometry
WAVEFIELD PREDICTION OF WATER-LAYER-MULTIPLES
Skeletonized Wave-equation Inversion for Q
Interferometric Least Squares Migration
Han Yu, Bowen Guo*, Sherif Hanafy, Fan-Chi Lin**, Gerard T. Schuster
Review of Coherent Noise Suppression Methods
Presentation transcript:

Crosscorrelation Migration of Free-Surface Multiples in RVSP Data Jianming Sheng University of Utah February, 2001

Outline ObjectiveObjective Crosscorrelation migrationCrosscorrelation migration Numerical examplesNumerical examples SummarySummary

Objective Validate the feasibility of crosscorrelation migration for RVSP data; Image the reflectivity distribution without knowing the source position. (Schuster and Rickett, 2000)

Outline ObjectiveObjective Crosscorrelation migrationCrosscorrelation migration Numerical examplesNumerical examples SummarySummary

Crosscorrelation Migration Principle Asymptotic analysis Key steps

Principle of CCM S G’ G X Crosscorrelogram

Principle of CCM S G’ G X Virtualsource Imaging condition

Asymptotic Analysis Migration image Trial image point Crosscorrelograms

Asymptotic Analysis Under stationary phase condition D irect G host Negligible contribution from: D irect Contribution from: Contribution from: G host Contribution from: Contribution from: G host D irect Reflection coefficient

Asymptotic Analysis CCM image gives the reflectivity distribution except contaminated by artifacts up to order

Key Steps of CCM Step 1: Bandpass filter and other preprocess; Step 2: Dip filter; Step 5: Migrate the crosscorrelograms. Step 3: Generate crosscorrelograms; Step 4: Filter aliasing in crosscorrelograms;

Outline ObjectiveObjective Crosscorrelation migrationCrosscorrelation migration Numerical examplesNumerical examples SummarySummary

Numerical Examples Three-layered modelThree-layered model Exxon’s Friendswood RVSP dataExxon’s Friendswood RVSP data

RECEIVERS 91.4 m m V1 = 762 m/s V3 = 1372 m/s V2 = 1067 m/s SOURCES Three-Layered Model 98 shots 24 traces per shot

1st-CRG Depth (m) Depth (m) Time (sec.) Dip-filtered Before dip-filtered Direct Primary Ghost

1st-CSG Time (sec.) Offset (m) Shot Gather Crosscorrelogram Pseudo-Shot Gather D G High-order Ghost

Crosscorrelation migration image Offset (m) Depth (m) True Reflectors

RECEIVERS SOURCES Exxon’s Friendswood RVSP Data 98 shots 23 traces per shot 9.1 m m 7.6 m m

Exxon’s Friendswood RVSP Data Depth (m) 100 ReflectivityWell-log CCM

Exxon’s Friendswood RVSP Data Offset (m) Depth (m) CCM image

Outline ObjectiveObjective Crosscorrelation migrationCrosscorrelation migration Numerical examplesNumerical examples SummarySummary

Summary Asymptotic analysis shows that CCM is capable of imaging the reflectivity distribution;Asymptotic analysis shows that CCM is capable of imaging the reflectivity distribution; The results of synthetic and Exxon’s Friendswood RVSP data validate the feasibility of CCM.The results of synthetic and Exxon’s Friendswood RVSP data validate the feasibility of CCM.

Further Work To attenuate the artifacts generated by CCM;To attenuate the artifacts generated by CCM; To deal with the amplitude preservation problem.To deal with the amplitude preservation problem.

Acknowledgment I thank the sponsors of the 2000 University of Utah Tomography and Modeling /Migration (UTAM) Consortium for their financial support.