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GEOL882.3
Reflection
Seismic Processing
Objective
Processing Systems
General concept of CMP
processing
Processing Tools
SEGY and similar file formats
General features of ProMAX
Reading:
ProMAX manual (Introduction)
GEOL882.3
Reflection
Seismic Processing
Objective - transform
redundant reflection seismic
records in the time domain
into an interpretable depth
image.
Data reduction and editing;
Transformation into conveniently
computer-manageable form;
Removal of bad records;
Gathering;
CMP sorting;
Filtering in time and space;
Attenuation of noise;
Imaging
Final velocity and reflectivity
image.
GEOL882.3
Seismic Processing
Systems
Usually geared to a particular
type of application
Mostly CMP reflection processing;
Land or marine, 2D or 3D.
Commercial:
ProMAX (Landmark);
Omega (Western Geophysical, marine);
Focus (Paradigm);
Amoco and almost every other company have
their own…
Vista (Seismic Image Soft.).
Open-source/Universities:
Stanford Exploration Project;
Seismic UNIX (Colorado School of Mines);
FreeUSP (Amoco);
SIOSEIS (Scrippts, marine, not free!);
SIA: http://seisweb.usask.ca/SIA
GEOL882.3
Seismic data formats
SEG-Y
Most seismic data formats are similar, and
include:
Text file header (comments for the user, line
description);
Binary file header (number of traces, other vital
formatting information);
‘Traces’, each including:
➢
Binary trace header (channel number, coordinate,
offset, statics, mute times, filter parameters,
etc.). Some formats allow user-defined trace
headers.
➢
Trace sample values (integer or floating-point).
SEG-Y (adopted by SEG as the standard data
exchange format):
Text file header of 3200 bytes (40 80-character
lines);
Binary file header of 400 bytes;
Traces include:
➢
240-byte headers, fixed predefined format.
➢
Samples in any of the 2- or 4-byte formats
(usually stored as 4-byte IBM REAL).
A moderate 2-D seismic line with 800 shots
recorded by 96 channels at 1500 samples per
trace takes about 500 Mb of storage in SEG-Y
format (verify this!)
GEOL882.3
General CMP Processing
Sequence
1) Demultiplex, Vibroseis
correlation, Gain recovery
Conversion from file formats produced
by field data loggers into processing-
oriented formats
➢
SEG-Y, SEG-2.
➢
ProMax, Focus, Omega, SU, Vista, etc.,
internal formats.
These days, may not be required (done
in the field).
2) Field Geometry
Assignment of source-receiver
coordinates, offsets, etc. in the
trace headers.
3) Edit
Removal of bad traces (noisy
channels, poorly planted
geophones, channels contaminated
by power line noise, etc.).
GEOL882.3
General CMP Processing
Sequence (continued)
4) First arrival picking
May be semi-automatic or manual;
Required for generation of refraction statics;
models and for designing the mutes.
5) Elevation statics
Based on geometry information, compensates
the travel-time variations caused by variations
in source/receiver elevations.
Transforms the records as if recorded at a
common horizontal datum surface.
6) Refraction statics
Builds a model for the shallow, low-velocity
subsurface;
Compensates the travel-time variations caused
by the shallow velocities.
7) ‘Top’, ‘bottom’, and ‘surgical’ mute
Eliminates (sets amplitude=0) the time
intervals where strong non-reflection energy is
present:
First arrivals, ground roll, airwave.
GEOL882.3
General CMP Processing
Sequence (continued)
8) Gain recovery
Compensates geometrical spreading;
Based on a simple heuristic relation.
10) Trace balance
Equalizes the variations in amplitudes
caused by differences in coupling;
In true-amplitude processing, replaced with
‘surface-consistent deconvolution’.
9) Deconvolution
Compresses the wavelet in time, attenuates
reverberations.
10) Gather, CMP sort
In modern processing systems (ProMax,
Omega, Vista) done by using trace lookup
spreadsheets rather than by creating
additional copies of the dataset.
GEOL882.3
General CMP Processing
Sequence (continued)
12) Velocity analysis
For each of the CMP gathers,
determines the optimal stacking
velocity.
13) Dip Moveout (DMO) correction
Transforms the records so that the
subsequent NMO+stack work well even
in the presence of dipping reflectors.
14) Normal Moveout (NMO)
correction
Removes the effects of source-receiver
separation from reflection records;
Transforms the records as if recorded
at normal incidence.
15) Residual statics
Removes the remaining small travel-
time variations caused by inaccurate
statics or velocity model
GEOL882.3
General CMP Processing
Sequence (continued)
16) Steps 12-15 above are usually
iterated 3-5 times to produce
accurate velocity and residual
statics models.
Success of velocity analysis depends
on the quality of DMO/NMO and
residual statics, and vice versa.
17) Stack
Produces a zero-offset section;
Utilizes CMP redundancy to increase
the Signal/Noise ratio.
18) Migration
Transforms the zero-offset time
section into a depth image;
Establishes correct extents and dips of
the reflectors.
GEOL882.3
Processing tools
Preprocessing
Demultiplex;
Editing;
Gain recovery;
Field geometry;
Elevation (‘field’) statics.
Travel-time corrections
Statics, i.e., time shifts
(elevation, refraction
(weathering), residual);
Velocity analysis (testing for
hyperbolic moveout);
Normal-moveout correction
(NMO);
Dip moveout correction (DMO);
Migration.
GEOL882.3
Processing tools
Continued
Wavelet adjustments
Vibroseis correlation,
Deconvolution;
Frequency filtering.
Amplitude corrections
Compensation of Geometrical
spreading;
Gain
➢
Automatic Gain Correction
(AGC,), trace normalization, etc.
Noise reduction
Velocity filtering (f-k and τ-p
filters);
‘Vertical' stack, CMP stack;
Muting.
GEOL882.3
General Processing Flow
Seismic processing flow is a
computer program
Implemented as a 'script' (DISCO, SIA,
SU), 'instruction list' (ProMAX), or visual
'graph' (Vista, Omega)
User builds the processing sequence using
a collection of tools for data manipulation
Results in generation of a code customized
to perform the specified task
GEOL882.3
A More General
Processing Flow (SIA)
SIA Seismic processing logic is based on
independent operation of the modules
Each module transforms an input gather of
multicomponent traces into output one
SIA also maintains a system of database tables
and inter-modular messaging mechanism
GEOL882.3
ProMAX
Data hierarchy
Area (project)
Line
Processing Flows (perform specific
processing tasks with the traces or
databases)
Datasets (traces, headers, lookup
tables)
Databases (most of them called
OPF – Ordered Parameter Files)
Tables (travel times, velocity
models, etc.)
A special area used for archiving
and restoring other projects
('areas')
GEOL882.3
ProMAX
Key components
Front-end GUI
Navigates within areas, lines, flows,
datasets, databases, tables, etc.
Flow builder
Allows building processing flows
from a library of modules
Send flows to execution
Monitor
Monitors running jobs, allows
suspending and killing them
Displays job logs
Database editors
Display/edit various databases

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Seismic_Processing.pdf

  • 1. GEOL882.3 Reflection Seismic Processing Objective Processing Systems General concept of CMP processing Processing Tools SEGY and similar file formats General features of ProMAX Reading: ProMAX manual (Introduction)
  • 2. GEOL882.3 Reflection Seismic Processing Objective - transform redundant reflection seismic records in the time domain into an interpretable depth image. Data reduction and editing; Transformation into conveniently computer-manageable form; Removal of bad records; Gathering; CMP sorting; Filtering in time and space; Attenuation of noise; Imaging Final velocity and reflectivity image.
  • 3. GEOL882.3 Seismic Processing Systems Usually geared to a particular type of application Mostly CMP reflection processing; Land or marine, 2D or 3D. Commercial: ProMAX (Landmark); Omega (Western Geophysical, marine); Focus (Paradigm); Amoco and almost every other company have their own… Vista (Seismic Image Soft.). Open-source/Universities: Stanford Exploration Project; Seismic UNIX (Colorado School of Mines); FreeUSP (Amoco); SIOSEIS (Scrippts, marine, not free!); SIA: http://seisweb.usask.ca/SIA
  • 4. GEOL882.3 Seismic data formats SEG-Y Most seismic data formats are similar, and include: Text file header (comments for the user, line description); Binary file header (number of traces, other vital formatting information); ‘Traces’, each including: ➢ Binary trace header (channel number, coordinate, offset, statics, mute times, filter parameters, etc.). Some formats allow user-defined trace headers. ➢ Trace sample values (integer or floating-point). SEG-Y (adopted by SEG as the standard data exchange format): Text file header of 3200 bytes (40 80-character lines); Binary file header of 400 bytes; Traces include: ➢ 240-byte headers, fixed predefined format. ➢ Samples in any of the 2- or 4-byte formats (usually stored as 4-byte IBM REAL). A moderate 2-D seismic line with 800 shots recorded by 96 channels at 1500 samples per trace takes about 500 Mb of storage in SEG-Y format (verify this!)
  • 5. GEOL882.3 General CMP Processing Sequence 1) Demultiplex, Vibroseis correlation, Gain recovery Conversion from file formats produced by field data loggers into processing- oriented formats ➢ SEG-Y, SEG-2. ➢ ProMax, Focus, Omega, SU, Vista, etc., internal formats. These days, may not be required (done in the field). 2) Field Geometry Assignment of source-receiver coordinates, offsets, etc. in the trace headers. 3) Edit Removal of bad traces (noisy channels, poorly planted geophones, channels contaminated by power line noise, etc.).
  • 6. GEOL882.3 General CMP Processing Sequence (continued) 4) First arrival picking May be semi-automatic or manual; Required for generation of refraction statics; models and for designing the mutes. 5) Elevation statics Based on geometry information, compensates the travel-time variations caused by variations in source/receiver elevations. Transforms the records as if recorded at a common horizontal datum surface. 6) Refraction statics Builds a model for the shallow, low-velocity subsurface; Compensates the travel-time variations caused by the shallow velocities. 7) ‘Top’, ‘bottom’, and ‘surgical’ mute Eliminates (sets amplitude=0) the time intervals where strong non-reflection energy is present: First arrivals, ground roll, airwave.
  • 7. GEOL882.3 General CMP Processing Sequence (continued) 8) Gain recovery Compensates geometrical spreading; Based on a simple heuristic relation. 10) Trace balance Equalizes the variations in amplitudes caused by differences in coupling; In true-amplitude processing, replaced with ‘surface-consistent deconvolution’. 9) Deconvolution Compresses the wavelet in time, attenuates reverberations. 10) Gather, CMP sort In modern processing systems (ProMax, Omega, Vista) done by using trace lookup spreadsheets rather than by creating additional copies of the dataset.
  • 8. GEOL882.3 General CMP Processing Sequence (continued) 12) Velocity analysis For each of the CMP gathers, determines the optimal stacking velocity. 13) Dip Moveout (DMO) correction Transforms the records so that the subsequent NMO+stack work well even in the presence of dipping reflectors. 14) Normal Moveout (NMO) correction Removes the effects of source-receiver separation from reflection records; Transforms the records as if recorded at normal incidence. 15) Residual statics Removes the remaining small travel- time variations caused by inaccurate statics or velocity model
  • 9. GEOL882.3 General CMP Processing Sequence (continued) 16) Steps 12-15 above are usually iterated 3-5 times to produce accurate velocity and residual statics models. Success of velocity analysis depends on the quality of DMO/NMO and residual statics, and vice versa. 17) Stack Produces a zero-offset section; Utilizes CMP redundancy to increase the Signal/Noise ratio. 18) Migration Transforms the zero-offset time section into a depth image; Establishes correct extents and dips of the reflectors.
  • 10. GEOL882.3 Processing tools Preprocessing Demultiplex; Editing; Gain recovery; Field geometry; Elevation (‘field’) statics. Travel-time corrections Statics, i.e., time shifts (elevation, refraction (weathering), residual); Velocity analysis (testing for hyperbolic moveout); Normal-moveout correction (NMO); Dip moveout correction (DMO); Migration.
  • 11. GEOL882.3 Processing tools Continued Wavelet adjustments Vibroseis correlation, Deconvolution; Frequency filtering. Amplitude corrections Compensation of Geometrical spreading; Gain ➢ Automatic Gain Correction (AGC,), trace normalization, etc. Noise reduction Velocity filtering (f-k and τ-p filters); ‘Vertical' stack, CMP stack; Muting.
  • 12. GEOL882.3 General Processing Flow Seismic processing flow is a computer program Implemented as a 'script' (DISCO, SIA, SU), 'instruction list' (ProMAX), or visual 'graph' (Vista, Omega) User builds the processing sequence using a collection of tools for data manipulation Results in generation of a code customized to perform the specified task
  • 13. GEOL882.3 A More General Processing Flow (SIA) SIA Seismic processing logic is based on independent operation of the modules Each module transforms an input gather of multicomponent traces into output one SIA also maintains a system of database tables and inter-modular messaging mechanism
  • 14. GEOL882.3 ProMAX Data hierarchy Area (project) Line Processing Flows (perform specific processing tasks with the traces or databases) Datasets (traces, headers, lookup tables) Databases (most of them called OPF – Ordered Parameter Files) Tables (travel times, velocity models, etc.) A special area used for archiving and restoring other projects ('areas')
  • 15. GEOL882.3 ProMAX Key components Front-end GUI Navigates within areas, lines, flows, datasets, databases, tables, etc. Flow builder Allows building processing flows from a library of modules Send flows to execution Monitor Monitors running jobs, allows suspending and killing them Displays job logs Database editors Display/edit various databases