All Stories

  1. The Unappreciated Importance of Refraction Echoes or Guided Waves in Causing Bad Land Seismic Data
  2. Refraction multiple attenuation by pattern-based machine learning with a case study
  3. Episode 224: The Physics Behind Land Seismic Noise (Christof Stork)
  4. Understanding Land Seismic Scattering Noise through Careful Simulation
  5. Analysing Acquisition and Processing Methods to Address Land Seismic Scattering Noise through Fine Scale Elastic Modelling
  6. The Unappreciated Importance of Refraction Multiples as Land Seismic Noise
  7. Recent advances, road ahead: Acquisition, processing, and interpretation improvements in using land seismic data for QI
  8. Using ‘Noise-Corrected OVT Fold’ to optimise land seismic acquisition risk, costs, and quality
  9. Land and OBN near surface seismic distortion is often more complicated than the standard SC-Decon model
  10. Using “Noise-Corrected OVT Fold” to Optimize Land Seismic Acquisition Risk, Costs, and Quality
  11. Basic Land Seismic Surface Correction Processing Steps have Artifacts that Corrupt Seismic Reservoir Characterization
  12. Evidence that land seismic surface scattering noise can be treated as correctable signal distortion
  13. Optimizing seismic land acquisition and processing for surface scattering noise
  14. A Model for Land Seismic Surface Scattering Noise has Implications for Acquisition and Processing
  15. Reducing land seismic scattering noise through surface effects deconvolution
  16. Key seismic processing steps to resolve amplitude characteristics of reservoir geobodies in the SEAM-Barrett model
  17. How does the thin near surface of the earth produce 10–100 times more noise on land seismic data than on marine data?
  18. Global land seismic acquisition optimization by accounting for varying noise, obstacles, non-uniform placement costs, and signal
  19. Introduction to special section: Foothills exploration
  20. We can and should be using more prestack attributes to characterize unconventional reservoirs: An example from the Permian Basin
  21. Steps for Improving the Utility of Land Seismic Data for Unconventional Reservoirs
  22. Game changing seismic noise attenuation is possible with irregular acquisition
  23. Results from a large field test using 2D ring arrays to address backscattered surface noise in land seismic acquisition
  24. Using 2D Ring Arrays to Remove Back-scattered Surface Noise from Land Seismic Data
  25. Using 2D ring arrays to remove back-scattered surface noise from land seismic data
  26. The decline of conventional seismic acquisition and the rise of specialized acquisition: This is compressive sensing
  27. A practitioner's approach to full waveform inversion
  28. Wave equation illumination using RTM
  29. Illuminating imperfections of imaging inversion
  30. Eliminating Nearly All Dispersion Error from FD Modeling and RTM with Minimal Cost Increase
  31. 3D nonlinear stack enhancement: Correlation based stacking
  32. Interpretive Full Waveform Inversion using region constraints
  33. Testing Different 3D Acquisition Geometries for Reducing Back-scattered Surface Noise
  34. Seismic acquisition is moving from a “CMP Fold” perspective to a “Wavefield Recording” perspective which has significant implications on acquisition design
  35. RTM images from SEAM data show interesting features
  36. Signals
  37. CRS Workflow for Enhanced 3D Seismic Salt Imaging and Model Building
  38. Predicting subsalt dip‐dependent illumination variations using density bubbles with RTM migration
  39. Addressing key land data quality challenges with passive seismic interferometry
  40. Fixing the Non-Uniform Directionality Problem of Seismic Interferometry May Be Crucial to its Success
  41. Fixing the nonuniform directionality of seismic daylight interferometry may be crucial to its success
  42. Response to the reply
  43. Reply to the discussion
  44. On “Delayed-shot 3D depth migration” ()
  45. Benefits of Low Frequencies for Subsalt Imaging
  46. Solving Static Problems with Ultra-Low Frequency Data and Waveform Inversion
  47. Predicting and removing complex 3D surface multiples with WEM modeling—an alternative to 3D SRME for wide azimuth surveys?
  48. Signals
  49. Benefits of low frequencies for subsalt imaging
  50. How many P values do you want to migrate for delayed shot wave equation migration?
  51. Integrating complementary tools for improved depth imaging
  52. Comparison between angle and offset gathers from wave equation migration and Kirchhoff migration
  53. Near‐salt‐flank imaging with Kirchhoff and wavefield‐extrapolation migration
  54. Hardware and Software Issues for Making Large Clusters Effective in a Production Seismic Processing Environment
  55. Making prestack depth migration work despite the inherent‐errors in the velocity model building process
  56. Hybrid Born and Rytov inversion
  57. Demonstration of MVA tomography with controls and constraints for determining an accurate velocity model for prestack depth migration
  58. Staged hybrid genetic search for seismic data imaging
  59. Hybrid Born and Rytov inversion for seismic applications
  60. A Hybrid genetic algorithm/steepest ascent approach has success with difficult statics
  61. The Rytov approximation aids the resolution of the broad velocity components in non-linear waveform inversion
  62. Modification of conjugate gradient iteration for stable and reproducible inversions
  63. Singular value decomposition of the velocity‐reflector depth tradeoff, Part 1: Introduction using a two‐parameter model
  64. Singular value decomposition of the velocity‐reflector depth tradeoff, Part 2: High‐resolution analysis of a generic model
  65. Combining reflection tomography with migration velocity analysis
  66. The interactive setup, calculation & display of finite difference modelling on a workstation
  67. The non-uniqueness of migration velocities
  68. Reflection tomography in the postmigrated domain
  69. Using constraints to address the instabilities of automated prestack velocity analysis
  70. Hybrid genetic autostatics: New approach for large‐amplitude statics with noisy data
  71. Making depth migration work in complex structures
  72. Stable Determination of Internal Velocities in Complex Structure Using Tomographic Migration Velocity Analyses
  73. Linear aspects of tomographic velocity analysis
  74. High‐resolution SVD analysis of the coupled velocity determination and reflector imaging problem
  75. Need for constraints in generalized prestack velocity analysis
  76. Analysis of issues in transmission tomography using ray trace tomography
  77. Application of tomography to two data sets containing lateral velocity variations
  78. Case study of traveltime tomography applied to data sets containing lateral velocity variations
  79. Analysis of the resolution between ambiguous velocity and reflector position for traveltime tomography
  80. Iterative tomographic and migration reconstruction of seismic images