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Simple Seismic processing
workflow
By: Ali Ismael AlBaklishy
Senior Student, Geophysics Department,
School of sciences, Cairo University
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 Processing Workflow:
 References.
 Q&A.
Content
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 Processing Workflow:
 References.
 Q&A.
Introduction
Seismic Prospecting
Seismic
Interpretation
Seismic
acquisition
Seismic
Processing
Seismic
Interpretation
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 Processing Workflow:
 References.
 Q&A.
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
 DataReformat(Transcription)
Field data format
SEG Y
SEG D
Internal format of
the co.
Ex.: DIO (Omega)
Data Initialization
 Geometry update
Objective :
• Insert the X,Y,Z coordinates for each
shot and geophone group by merge the
Navigation/SPS file with the data file .
Data Initialization
 Trace Editing
Objective :
1- Remove bad traces.
2- Remove bad shots.
3-Remove Duplicated traces.
4- Polarity Revers.
Data Initialization
Trace Editing
before
after
Data Initialization
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
 AmplitudeRecovery AndGain
• Energy is attenuated due to the spherical divergence
effect.
Amplitude Processing
Before after
• Before And After Amplitude Recovery
Amplitude Processing
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
1- Ground Roll Attenuation.
Before
Noise Attenuation
• Ground Roll Attenuation
After
Noise Attenuation
2- Swell Noise Attenuation.
Before After
Noise Attenuation
3- Liner Noise Attenuation
By using FK filter & Radon (tau p)
Noise Attenuation
• Tau p Radon transform
Noise Attenuation
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
Deconvolution
Objective:
To get rid of the energy wavelet so that get the earth’s
Reflectivity.
• Deterministic Deconv. (de-signature Deconv.)
(known Wavelet)
Deconvolution
• Statistical Deconv. (Gap Deconv).
(Unknown Wavelet)
Before
Deconvolution
After
Deconvolution
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
MultipleAttenuation
• Water Bottom Multiples Attenuation
BeforeAfter
• Surface Multiples Attenuation
MultipleAttenuation
BeforeAfter
• Interbed Multiples Attenuation
• Short period and residual Multiples
Attenuation
By using Deconvolution
MultipleAttenuation
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
VelocityAnalysisAndNMO
Objective :
1- Determine NMO Velocity.
2- Determine stack velocity.
3- Determine Migration velocity.
VelocityAnalysisAndNMO
MVFS
• In case of wrong Velocity
VelocityAnalysisAndNMO
• Stretch Muting
VelocityAnalysisAndNMO
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
Migration
Objective:
Is to reposition the data from its apparent reflection
point (due to Non Horizontal Reflectors) to its true
reflection point.
• Migration classification According to its position in the
workflow
Post stack
Migration
Pre-Stack
Migration
• Take long time.
• High cost.
• No data losses.
• Less time.
• Low cost.
• Loss in data.
Migration
• Pre-stack and post stack
Migration
Migration
• Migration classification According to its types:
Time
Migration
Depth
Migration
• Time and space
Domain.
• Don’t takes ray
bending & lateral
velocity change into
account.
• Take shorter time.
• Depth Domain.
• takes ray bending
& lateral velocity
change into
account.
• require greater
computer time.
Migration
1- Time Migration
• Time migration is the repositioning of reflected seismic data to their
true reflection points in space and time.
Ex: Kirchhoff Migration
Migration
2- Depth Migration.
• In depth migration, data are migrated in depth domain
and the input data for the process is unmigrated seismic
data in time domain. The output is migrated data in the
depth domain.
• take into account the bending of ray paths by
refraction within a complex geology.
Migration
• Time Migration and depth Migration
Migration
• Migration Examples
Migration
• Migration Examples
Migration
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
Stacking
Stacking
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 References.
 Q&A.
 Data Makeup
• Data Filtering
• Amplitude Scaling
Stacking
Stacking
Content
 Introduction.
• Data Initialization.
• Amplitude Processing.
• Noise Attenuation.
• Deconvolution.
• Multiple Attenuation.
• Velocity Analysis and NMO.
• Migration.
• Stack.
• Data Makeup.
 Processing Workflow:
 Q&A.
References:
• Exploration Geophysics, Mamdouh R. Gadallah · Ray
Fisher,2009.
• Seismic data Processing, OZ Yilmaz.
• Seismic Data Analysis And Techniques in Hydrocarbon
Exploration, ENWENODE ONAJITE, 2014
• Seismic Reflections: Marine Processing - Part 5 | Direct
Arrivals, Refractions, and Linear Noise
• Seismic Reflections: Marine Processing - Part 4 | Swell Noise
Removal
Q&A
Simple seismic processing workflow

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