Depth Conversion and Velocity Modelling Course
At a glance
- Duration
- 1 Week
- Format
- Classroom
- Cities
- Bali, Langkawi, Singapore, Muscat, Istanbul, Barcelona and more
- Next session
- 8 – 12 November 2026, Bali
- Average fee
- 7,500 €
Overview
Advanced Depth Conversion and Velocity Modelling Training Course is a one-week advanced course for seismic interpreters, exploration geophysicists, depth-imaging reviewers, subsurface team leads, and geoscientists who must turn time-domain interpretations into defensible depth products. Participants connect velocity data qualification, well-to-seismic calibration, Dix interval velocity, layered velocity model building, gridded velocity model construction, anisotropic depth imaging review, time-to-depth conversion, structural depth uncertainty, and technical assurance. The course is software-neutral and converts evidence into a Velocity Model and Depth Conversion Assurance File. Agile Leaders Training Center presents advanced depth conversion and velocity modelling.
Who Should Attend
- Seismic interpretation functions responsible for horizons, faults, structural closures, and depth maps
- Exploration and development geophysicists responsible for velocity evidence and depth prognosis
- Depth-imaging reviewers responsible for tomography, migration gathers, and model-update acceptance
- Well-seismic integration functions responsible for checkshots, vertical seismic profiles, sonic logs, and synthetic ties
- Subsurface team leads responsible for structural uncertainty, assurance gates, and technical handover
- Geoscience quality functions responsible for traceability, residual analysis, and model governance
The course assumes working knowledge of seismic interpretation and basic travel-time concepts. It leaves out introductory seismic acquisition, detailed signal processing, vendor-specific button sequences, software programming, and full mathematical derivations of migration algorithms.
Departments and Industries
The course supports functions that use seismic travel time, well evidence, and velocity models to make depth-based subsurface decisions.
- Oil and gas exploration and appraisal
- Field development and well planning
- Seismic interpretation and depth imaging
- Subsurface assurance and technical governance
- Carbon storage site characterization
- Geothermal and regional geoscience studies
Learning Objectives
By the end of this course, participants will be able to:
- Distinguish stacking, RMS, average, interval, migration, and anisotropic velocities
- Qualify checkshot, vertical seismic profile, sonic-log, well-top, and processing velocity evidence
- Build layered and gridded velocity models with geological constraints
- Convert interpreted horizons and faults from time to depth with traceable assumptions
- Diagnose calibration residuals, misties, structural artifacts, and model limitations
- Test scenarios and communicate depth uncertainty for assurance decisions
Course Agenda
Day 1: Qualify Velocity Evidence
- Velocity Type, Domain, Datum, and Unit Classification Matrix
- Checkshot, Vertical Seismic Profile, and Sonic-Log Evidence Register
- Well-Tie, Polarity, Phase, and Horizon Correspondence Checklist
- RMS-to-Interval Velocity Conversion using Dix Relationships
- Velocity Data Provenance and Fitness-for-Purpose Scorecard
Day 2: Build Geological Velocity Models
- Layer Framework, Fault Boundary, and Formation Constraint Panel
- Constant, Gradient, Compaction, and Trend Function Comparison
- Layered Velocity Model Building and Well Calibration Workflow
- Gridded Velocity Model Construction and Spatial Interpolation Controls
- Velocity Outlier, Lateral Variation, and Scenario Register
Day 3: Review Depth Imaging Updates
- Time Migration versus Depth Migration Decision Matrix
- Kirchhoff, Reverse-Time Migration, and Imaging Assumption Map
- Tomographic Residual-Moveout Interpretation and Update Review
- Full-Waveform Inversion Interface and Low-Wavenumber Model Check
- VTI and TTI Anisotropy Parameter Evidence and Sensitivity Sheet
Day 4: Convert and Assure Structural Interpretation
- Vertical-Ray, Image-Ray, and Volume-Based Time-to-Depth Conversion
- Horizon, Fault, Point, and Grid Domain-Conversion Control Sheet
- Well-Top Residual Map and Calibration Closure Test
- Depth-Surface Structure, Thickness, and Closure Integrity Review
- Structural Depth Uncertainty Scenario and Envelope Map
Day 5: Defend the Depth Solution
- Suggested Exercise: Reconcile Velocity Sources and Select Model Inputs
- Suggested Exercise: Build Layered and Gridded Velocity Scenarios
- Suggested Exercise: Diagnose Residuals and Depth-Imaging Artifacts
- Suggested Exercise: Convert Horizons and Test Closure Sensitivity
- Capstone Exercise: Complete the Velocity Model and Depth Conversion Assurance File
Practical Exercises
The course uses suggested activities to connect interpreter decisions, velocity evidence, model behavior, and depth risk.
- Suggested activity: inventory velocity sources, reconcile domains and datums, and record evidence limitations.
- Suggested activity: calculate interval velocities, calibrate a layered model to wells, and inspect residual patterns.
- Suggested activity: compare velocity scenarios and diagnose their effects on faults, closures, thickness, and well prognosis.
- Suggested activity: assemble a review file with acceptance criteria, uncertainty envelopes, decision logs, and handover actions.
FAQs
Who suits advanced depth conversion and velocity modelling training?
Advanced depth conversion and velocity modelling training suits experienced seismic interpreters, exploration geophysicists, imaging reviewers, well-seismic integration specialists, and subsurface assurance leads. Participants should already understand seismic sections, horizons, faults, and basic travel-time concepts.
How does time-to-depth conversion differ from depth migration?
Time-to-depth conversion transforms interpreted time-domain objects through a velocity model. Depth migration repositions seismic energy during imaging with a depth-domain velocity model. Both depend on velocity quality, but they use different workflows and must be reviewed with different controls.
Which velocity data are used in a depth conversion model?
A depth conversion model can use checkshots, vertical seismic profiles, calibrated sonic logs, well tops, stacking or migration velocities, geological trends, and interpreted layer boundaries. Their value depends on domain, datum, sampling, uncertainty, and fitness for the intended conversion.
How is a velocity model calibrated and quality controlled?
Calibration compares predicted and observed travel times or depths at wells, maps residuals, investigates systematic and local misties, tests alternative functions and spatial trends, and confirms that structural results remain geologically plausible.
How is structural depth uncertainty communicated?
Structural depth uncertainty is communicated through traceable model scenarios, parameter sensitivities, well residuals, depth envelopes, closure and thickness changes, assumption registers, and clear conditions for accepting or revisiting the model.
Conclusion
Participants take back a Velocity Model and Depth Conversion Assurance File that links data provenance, velocity classification, well calibration, model construction, imaging review, converted structural products, residuals, uncertainty scenarios, and acceptance decisions. It supports clearer technical challenge, more defensible depth maps, and better communication between interpreters, imagers, geologists, and well planners.
credits: 5 credit per day
Course Mode: full-time
Provider: Agile Leaders Training Center
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Events for this Course
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Bali 8 – 12 November 2026
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Langkawi 15 – 19 November 2026
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Singapore 16 – 20 November 2026
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Muscat 22 – 26 November 2026
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Istanbul 30 November – 4 December 2026
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Barcelona 7 – 11 December 2026
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Trabzon 13 – 17 December 2026
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Jakarta 21 – 25 December 2026
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Madrid 28 December 2026 – 1 January 2027
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Dubai 4 – 8 January 2027
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Tokyo 4 – 8 January 2027
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Doha 10 – 14 January 2027
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Nice 11 – 15 January 2027
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Johannesburg 17 – 21 January 2027
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Casablanca 18 – 22 January 2027
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Paris 1 – 5 February 2027
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San Diego 1 – 5 February 2027
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London 8 – 12 February 2027
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Manama 14 – 18 February 2027
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Bangkok 14 – 18 February 2027
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Kuwait 21 – 25 February 2027
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Rome 1 – 5 March 2027
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Zoom 8 – 12 March 2027
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Tashkent 21 – 25 March 2027
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Baku 22 – 26 March 2027
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Geneva 28 March – 1 April 2027
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New York 5 – 9 April 2027
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Addis Ababa 19 – 23 April 2027
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Nairobi 25 – 29 April 2027
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Amman 2 – 6 May 2027
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Abu Dhabi 3 – 7 May 2027
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Vienna 10 – 14 May 2027
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Phuket 16 – 20 May 2027
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Toronto 13 – 17 June 2027
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Tbilisi 14 – 18 June 2027
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Chicago 4 – 8 July 2027
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Lagos 18 – 22 July 2027
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Prague 19 – 23 July 2027
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Lisbon 26 – 30 July 2027
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Abu Dhabi 2 – 6 August 2027
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Berlin 9 – 13 August 2027
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Athens 16 – 20 August 2027
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Montreux 23 – 27 August 2027
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Frankfurt 30 August – 3 September 2027
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Cape town 5 – 9 September 2027
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Dubai 13 – 17 September 2027
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Munich 13 – 17 September 2027
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Cairo 20 – 24 September 2027
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Kuala Lumpur 27 September – 1 October 2027
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Seoul 27 September – 1 October 2027
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Zanzibar 3 – 7 October 2027
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Accra 17 – 21 October 2027
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Sharm El-Sheikh 18 – 22 October 2027
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Marbella 24 – 28 October 2027
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London 25 – 29 October 2027
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Amsterdam 1 – 5 November 2027
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Milan 8 – 12 November 2027
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Porto 8 – 12 November 2027
| Image | Location | Dates | Duration | Mode | Price | Actions |
|---|---|---|---|---|---|---|
|
|
Bali |
Week 45, 2026 8 – 12 November 2026 |
1 Week | Onsite | €6,500 | |
|
|
Langkawi |
Week 46, 2026 15 – 19 November 2026 |
1 Week | Onsite | €8,000 | |
|
|
Singapore |
Week 47, 2026 16 – 20 November 2026 |
1 Week | Onsite | €6,500 | |
|
|
Muscat |
Week 47, 2026 22 – 26 November 2026 |
1 Week | Onsite | €6,500 | |
|
|
Istanbul |
Week 49, 2026 30 November – 4 December 2026 |
1 Week | Onsite | €6,000 | |
|
|
Barcelona |
Week 50, 2026 7 – 11 December 2026 |
1 Week | Onsite | €6,500 | |
|
|
Trabzon |
Week 50, 2026 13 – 17 December 2026 |
1 Week | Onsite | €8,000 | |
|
|
Jakarta |
Week 52, 2026 21 – 25 December 2026 |
1 Week | Onsite | €8,000 | |
|
|
Madrid |
Week 53, 2026 28 December 2026 – 1 January 2027 |
1 Week | Onsite | €6,500 | |
|
|
Dubai |
Week 01, 2027 4 – 8 January 2027 |
1 Week | Onsite | €6,500 | |
|
|
Tokyo |
Week 01, 2027 4 – 8 January 2027 |
1 Week | Onsite | €12,000 | |
|
|
Doha |
Week 01, 2027 10 – 14 January 2027 |
1 Week | Onsite | €7,000 | |
|
|
Nice |
Week 02, 2027 11 – 15 January 2027 |
1 Week | Onsite | €8,000 | |
|
|
Johannesburg |
Week 02, 2027 17 – 21 January 2027 |
1 Week | Onsite | €6,000 | |
|
|
Casablanca |
Week 03, 2027 18 – 22 January 2027 |
1 Week | Onsite | €6,000 | |
|
|
Paris |
Week 05, 2027 1 – 5 February 2027 |
1 Week | Onsite | €6,500 | |
|
|
San Diego |
Week 05, 2027 1 – 5 February 2027 |
1 Week | Onsite | €16,000 | |
|
|
London |
Week 06, 2027 8 – 12 February 2027 |
1 Week | Onsite | €6,500 | |
|
|
Manama |
Week 06, 2027 14 – 18 February 2027 |
1 Week | Onsite | €6,500 | |
|
|
Bangkok |
Week 06, 2027 14 – 18 February 2027 |
1 Week | Onsite | €8,000 |
Frequently asked questions
What does this course cover?
OverviewAdvanced Depth Conversion and Velocity Modelling Training Course is a one-week advanced course for seismic interpreters, exploration geophysicists, depth-imaging reviewers, subsurface team leads, and geoscientists who must turn time-domain interpretations into defensible depth products. Participants connect velocity data qualification, well-to-sei…
Are training dates available?
Yes. Available dates and destinations are listed in the course dates section on this page.
How can I register?
Choose an available date on this page and complete the registration form, or send a programme enquiry.
Can I download the course brochure?
Yes. Use the brochure download link provided on this page.
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