Geoscientist Artificial Intelligence
Geoscientist Artificial Intelligence
  • Home
  • WorkFlow
    • Pre Processing
    • Time Processing
    • Time Imaging
  • Processing & Imaging
    • Anisotropy Analysis
    • Deconvolution
    • Inverse Q Filtering
    • Migration
    • Multiple Attenuation
    • Noise Attenuation
    • Ray Tracing
    • Stacking
    • Static Correction
    • Velocity & NMO Analysis
    • Waveform Modeling
    • Wave Equation Datuming
    • VSP
  • Interpretation
    • AVO Analysis
    • Data Conditioning
    • Facies Analysis
    • INVERSION
    • Rock Physics Modeling
    • Seismic Attributes
    • Spectral Blending
    • Well-Tie Analysis
  • Petrophysics
    • Geology
    • Natural Radiation Tools
    • Resistivity Tools
    • Sonic Tools
    • Neutron Tools
    • Formation Micro Imager
    • Cement Bounded Log
    • Caliper
  • More
    • Home
    • WorkFlow
      • Pre Processing
      • Time Processing
      • Time Imaging
    • Processing & Imaging
      • Anisotropy Analysis
      • Deconvolution
      • Inverse Q Filtering
      • Migration
      • Multiple Attenuation
      • Noise Attenuation
      • Ray Tracing
      • Stacking
      • Static Correction
      • Velocity & NMO Analysis
      • Waveform Modeling
      • Wave Equation Datuming
      • VSP
    • Interpretation
      • AVO Analysis
      • Data Conditioning
      • Facies Analysis
      • INVERSION
      • Rock Physics Modeling
      • Seismic Attributes
      • Spectral Blending
      • Well-Tie Analysis
    • Petrophysics
      • Geology
      • Natural Radiation Tools
      • Resistivity Tools
      • Sonic Tools
      • Neutron Tools
      • Formation Micro Imager
      • Cement Bounded Log
      • Caliper
  • Home
  • WorkFlow
    • Pre Processing
    • Time Processing
    • Time Imaging
  • Processing & Imaging
    • Anisotropy Analysis
    • Deconvolution
    • Inverse Q Filtering
    • Migration
    • Multiple Attenuation
    • Noise Attenuation
    • Ray Tracing
    • Stacking
    • Static Correction
    • Velocity & NMO Analysis
    • Waveform Modeling
    • Wave Equation Datuming
    • VSP
  • Interpretation
    • AVO Analysis
    • Data Conditioning
    • Facies Analysis
    • INVERSION
    • Rock Physics Modeling
    • Seismic Attributes
    • Spectral Blending
    • Well-Tie Analysis
  • Petrophysics
    • Geology
    • Natural Radiation Tools
    • Resistivity Tools
    • Sonic Tools
    • Neutron Tools
    • Formation Micro Imager
    • Cement Bounded Log
    • Caliper

Time Imaging (PSTM)

1. Velocity Model Building (Time): Refined RMS velocity picking on an optimized grid.
2. Initial PSTM: Preliminary Pre-Stack Time Migration for QC.
3. Iterative Velocity/Anisotropy Updating: Migration velocity analysis (MVA) and residual moveout correction.
4. Final Full 3D Anisotropic PSTM: Producing the final time-migrated gathers.
5. Post-Stack Processing: Residual noise suppression, spectral whitening, and time-variant filtering.

Time Imaging Workflow (PSTM Focus)

1. PSTM Velocity Model Building

- Objective: 

To create an initial RMS velocity field suitable for moving seismic events to their true spatial positions in time.
- Detailed Parameters:
1. Grid Density: Velocity picking grid (e.g., 400m x 400m or 200m x 200m).
2. Smoothing Kernels: Spatial smoothing (e.g., 500m radius) to ensure stability during migration.
- Controlling Parameters (QC):
1. Semblance Resolution: Ensure sharp energy peaks in the semblance plots.
2. Horizon Consistency: Velocity picks must follow key geological markers (horizons).
- Issues to Check:
1. Velocity Inversion: Be cautious of unrealistic velocity drops unless geologically justified (e.g., overpressure zones).
2. Lateral Variations: Strong lateral velocity changes can cause PSTM to fail; this is the signal to move to PSDM 

2. Pre-Stack Time Migration (PSTM) Execution

- Objective: 

To focus diffractions, collapse Fresnel zones, and image dipping events.
- Detailed Parameters:
1. Migration Aperture: The radius (in meters) the algorithm searches for energy (e.g., 5000m).
2. Maximum Dip: Limit of the angle to be imaged (typically 70°–80°).
3. Anti-Aliasing Filter: Frequency cut-offs to prevent spatial aliasing on steep dips.
- Controlling Parameters (QC):
1. Impulse Response: Check for "Migration Smiles" which indicate aperture or velocity issues.
2. Fault Definition: Sharpness of fault planes is the ultimate test for migration accuracy.
- Issues to Check:
1. Aperture Edge Effects: Insufficient aperture leads to "chopped" dipping reflectors or missing fault segments.
2. Computational Cost: Excessive aperture significantly increases run-time without always improving quality.

 

3. Residual Velocity Analysis (RVA / RMO)

- Objective: 

To flatten the events in Common Image Gathers (CIGs) after the initial migration.
- Detailed Parameters:
1. High-Density Picking: Finer grid (e.g., 100m x 100m) for residual corrections.
2. RMO Scans: Percentage-based velocity updates (e.g., 90% to 110% of V-initial).
- Controlling Parameters (QC):
1. Gather Flatness: Visually inspect PSTM Gathers to ensure reflectors are perfectly horizontal across all offsets.
2. Stack Power Maximization: Compare the stack before and after RVA.
- Issues to Check:
1. Non-Hyperbolic Moveout: In far offsets, standard RMO may fail, requiring anisotropy correction.

 

4. Anisotropy Correction (ETA Estimation)

- Objective: 

To correct the "Hockey-stick" effect at far offsets caused by Vertical Transverse Isotropy (VTI).
- Detailed Parameters:
1. ETA (h) Parameter: Used to adjust the non-hyperbolic moveout equation.
2. Long Offset Range: Typically requires offsets > 1.5x the target depth.
- Controlling Parameters (QC):
1. Far-Offset Alignment: Ensure events at 4000m+ offsets are aligned with near-offset events.
- Issues to Check:
1. V-ETA Ambiguity: Velocity and Eta parameters are coupled; picking one incorrectly affects the other. 

5. Final Conditioning & Stack

- Objective: 

To produce the final 3D volume with maximum Signal-to-Noise ratio (SNR).
- Detailed Parameters:
1. Muting Strategy: Surgical mutes to remove NMO stretch and refracted energy.
2. Stacking Method: Mean stack, Median stack, or Diversity stack to suppress noise.
3. TVF (Time-Variant Filtering): Bandpass filters that evolve with depth to maintain resolution.
- Controlling Parameters (QC):
1. Frequency Spectrum: Analyze the bandwidth to ensure no over-filtering.
2. Amplitude Preservation: Ensure the relative amplitudes are geologically meaningful (for AVO).

- Issues to Check:
1. Over-Muting: Can lead to loss of deep signal or poor SNR.
2. Artifacts: Look for acquisition footprints or processing-induced noise (smearing).

Copyright © 2026 Geoscientist Artificial Intelligent - All Rights Reserved.

Powered by

This website uses cookies.

We use cookies to analyze website traffic and optimize your website experience. By accepting our use of cookies, your data will be aggregated with all other user data.

Accept