Joint Migration of Primary and Multiple Reflections in RVSP Data Jianhua Yu, Gerard T. Schuster University of Utah.

Slides:



Advertisements
Similar presentations
Time-Lapse Monitoring of CO2 Injection with Vertical Seismic Profiles (VSP) at the Frio Project T.M. Daley, L.R. Myer*, G.M. Hoversten and E.L. Majer.
Advertisements

Warping for Trim Statics
Geological Model Depth(km) X(km) 2001 Year.
Adaptive Grid Reverse-Time Migration Yue Wang. Outline Motivation and ObjectiveMotivation and Objective Reverse Time MethodologyReverse Time Methodology.
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.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
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.
Solving Illumination Problems Solving Illumination Problems in Imaging:Efficient RTM & in Imaging:Efficient RTM & Migration Deconvolution Migration Deconvolution.
CROSSWELL IMAGING BY 2-D PRESTACK WAVEPATH MIGRATION
3-D Migration Deconvolution Jianxing Hu, GXT Bob Estill, Unocal Jianhua Yu, University of Utah Gerard T. Schuster, University of Utah.
Improve Migration Image Quality by 3-D Migration Deconvolution Jianhua Yu, Gerard T. Schuster University of Utah.
Depth (m) Time (s) Raw Seismograms Four-Layer Sand Channel Model Midpoint (m)
Bedrock Delineation by a Seismic Reflection/Refraction Survey at TEAD Utah David Sheley and Jianhua Yu.
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.
Kirchhoff vs Crosscorrelation
Autocorrelogram Migration of Drill-Bit Data Jianhua Yu, Lew Katz, Fred Followill, and Gerard T. Schuster.
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)
Local Migration with Extrapolated VSP Green’s Functions Xiang Xiao and Gerard Schuster Univ. of Utah.
Midyear Overview of Year 2001 UTAM Results T. Crosby, Y. Liu, G. Schuster, D. Sheley, J. Sheng, H. Sun, J. Yu and M. Zhou J. Yu and M. Zhou.
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.
MD + AVO Inversion Jianhua Yu, University of Utah Jianxing Hu GXT.
3-D Migration Deconvolution: Real Examples Jianhua Yu University of Utah Bob Estill Unocal.
Interferometric Multiple Migration of UPRC Data
Autocorrelogram Migration for Field Data Generated by A Horizontal Drill-bit Source Jianhua Yu, Lew Katz Fred Followill and Gerard T. Schuster.
Crosscorrelation Migration of Free-Surface Multiples in RVSP Data Jianming Sheng University of Utah February, 2001.
4C Mahogony Data Processing and Imaging by LSMF Method Jianhua Yu and Yue Wang.
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.
3D Wave-equation Interferometric Migration of VSP Free-surface Multiples Ruiqing He University of Utah Feb., 2006.
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,
The main instrument used is called the sonde. A basic sonde consists of a source and two receivers one-foot apart. The sonde is lowered down the borehole.
Impact of MD on AVO Inversion
EXPLORATION GEOPHYSICS. EARTH MODEL NORMAL-INCIDENCE REFLECTION AND TRANSMISSION COEFFICIENTS WHERE:  1 = DENSITY OF LAYER 1 V 1 = VELOCITY OF LAYER.
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
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.
Wave-Equation Waveform Inversion for Crosswell Data M. Zhou and Yue Wang Geology and Geophysics Department University of Utah.
Migration Velocity Analysis of Multi-source Data Xin Wang January 7,
3-D Prestack Migration Deconvolution Bob Estill ( Unocal) Jianhua Yu (University of Utah)
Seismic Methods Geoph 465/565 Vertical Seismic Profiling– Nov 2, 2015
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.
MD+AVO Inversion: Real Examples University of Utah Jianhua Yu.
Primary-Only Imaging Condition And Interferometric Migration
SEISMIC DATA GATHERING.
Modeling of free-surface multiples - 2
4C Mahogony Data Processing and Imaging by LSMF Method
Interferometric Least Squares Migration
Acoustic Reflection 2 (distance) = (velocity) (time) *
Han Yu, Bowen Guo*, Sherif Hanafy, Fan-Chi Lin**, Gerard T. Schuster
Review of Coherent Noise Suppression Methods
—Based on 2018 Field School Seismic Data
EXPLORATION GEOPHYSICS
LSMF for Suppressing Multiples
Presentation transcript:

Joint Migration of Primary and Multiple Reflections in RVSP Data Jianhua Yu, Gerard T. Schuster University of Utah

Time (s) SP Drill-bit Primary Autocorrelogram Migration Drill Hole Real ? Ghost ?

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Source Geophone ? RVSP While Drilling Provide Look-ahead Image Below the Drill Bit Reduce Uncertainty in Drilling

Source Geophone Bit Position? Problems in RVSPWD Pilot signal? Wavelet ?

Problems with Drill-bit and RVSP Data No source wavelet No source initiation time Not easy to get pilot signal in deviated well Not easy to get pilot signal in deviated well and horizontal well

Static shift errors may exist Difficulty for separating primary and ghost waves from deviated or horizontal well Problems with Drill-bit and RVSP Data

Solution Autocorrelogram Migration Why do we use autocorrelation of seismic data rather than the seismogram ???

Strengths of Autocorrelogram Migration No need to know initial time No limits to deviated well Be able to reduce static errors No need to know source wavelet

Well Drill bit Receiver Primary Direct Wave Ghost What is Joint Migration

Final migration image Ghost migration Primary migration Seismic Data

Joint Migration using Primary and Ghost Reflections Do not need to separate primary and ghost waves Attenuate the interferences in migration image What is Benefit from Joint Migration

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Primary Autocorrelogram Imaging Condition: x g s Autocorrelating Trace

Primary Autocorrelogram Imaging Condition: x g s

x g s

x g s Ghost Autocorrelogram Imaging Condition Ghost Autocorrelogram Imaging Condition: Autocorrelating Trace

x g s Ghost Autocorrelogram Imaging Condition Ghost Autocorrelogram Imaging Condition:

x g s

Principle of Joint Migration Seismic data: Primary + Ghost Ghost migrationPrimary migration Final migration image Product

Procedure of Joint Migration Pre-processing raw data Autocorrelating seismic traces: Migrating traces using both primary Mp and ghost imaging conditions Migrating traces using both primary Mp and ghost imaging conditions Mg Weighting primary image Calculating weight by w= Mp*Mg

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Horizontal Well Model 0 Depth (m) 3 40 X (m) V1 V2 V4 V3 V5 V6

Shot Gather Time (s) CSG Time (s) Traces Autocorrelogram

Depth (km) X (km) X (km) Standard migration Joint migration Standard Migration with Joint Migration (3 CSGs) Source

Time (s) X (km) X (km) With only primaryJoint auto. migration Time Migration Results (39 CSGs) Source X (km)

Depth (km) X (km) X (km) Kirchhoff migAuto. mig Depth Migration With Static Errors Source 3 CSGs

Depth (km) X (km) X (km) Joint Kirchhoff mig Joint auto. mig Depth Migration With Static Errors Source 39 CSGs

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

Acquisition Survey East (kft) North (kft) Well Rig 3C Receivers Drill bit 10 Depth (kft) 0

Recording Length: 20 s Sample Interval: 2 ms East (kft) North (kft) Well Rig 10 Depth (kft) ft Offset= ft Main Acquisition Parameters

Main Processing Steps Trace editing and static shift Trace editing and static shift Frequency panel analysis and noise elimination Frequency panel analysis and noise elimination Velocity analysis Velocity analysis Amplitude balance and energy normalization Autocorrelograms, vertical stacking utocorelograms Joint migrating autocorelograms

Autocorrelograms of CSG Time (s) s 12 s16 s

Time (s) 50 Joint Migration Images Traces

Acquisition Survey Map Well Rig 3C Receivers Drill bit East (ft) North (ft) C Line AC4

Time (s) SP Drill hole Joint Migration ( insert) and CDP Section

Time (s) SP Primary Migration ( insert) and CDP Section Drill hole

Time (s) SP Drilling hole Joint Migration ( insert) and CDP Section Joint

Time (s) SP Primary Migration ( insert) and CDP Section Drilling hole Primary

Outline Motivation Joint Migration Method Examples Synthetic data UPRC data Summary

SUMMARY Need separating primary and multiple? NO Work for deviated or horizontal well ? YES Reduce the influence of static errors ? YES Need pilot signal ? NO Need source wavelet and initial time ? NO Suppress coherent noise ? YES Amplitude fidelity ? NO Virtual Multiple ? YES

Acknowledgments I greatly appreciate Union Pacific Resources Corporation for providing this dataI greatly appreciate Union Pacific Resources Corporation for providing this data I thank the sponsors of the UTAM consortium for financial supportI thank the sponsors of the UTAM consortium for financial support