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SEISMIC ACQUISITION, PROCESSING and IMAGING
Synthesis
INTRODUCTION
- Seismic in the Exploration-Production Workflow
- The main steps of the seismic workflow: Acquisition, Time Processing, Depth Imaging, Interpretation
- Objectives of seismic interpretation: 3D geological model building , volumes, risks and uncertainties, well placement
PRINCIPLES OF THE SEISMIC REFLECTION METHOD
- Reminder of the fundamentals of the seismic signal: Dirac, Fourier transform, f-K filtering, convolution deconvolution, amplitude, frequency, phase,…
- Wavefront and seismic rays in a homogeneous medium
- P and S waves, different types of seismic waves in a stratified medium.
- Geometry of seismic rays propagation, Snell-Descartes law
- “Time of arrival vs. Offset” equation for direct and reflected waves
- Acoustic impedance, reflection coefficients, seismic amplitudes and polarity
- Frequency, wavelength, vertical and lateral seismic resolutions
SEISMIC DATA ACQUISITION TECHNIQUES
- Land acquisition: vibroseis and explosive sources, receivers (geophones), transmitters; Onshore acquisition specifics (static correction, noise,…)
- Marine acquisition: Air guns, hydrophones and streamers, Narrow and Wide Azimuth, Ocean Bottom Cables / Nodes, Broadband,…
- Other types of seismic acquisitions: borehole (VSP, check-shot), 4D
- From Shot Point (SP) to Common Mid Point (CMP); Multiple coverage, Bin
PRE-PROCESSING
- 5D regularization, bin centering
- Amplitude compensation,
- Attenuation of organized and random noise
- Seismic source designature, deconvolution
TIME PROCESSING – SEISMIC VELOCITIES
- Dynamic Corrections, Normal Move-Out: principles and applications
- Velocity analysis, stack, multiple removal.
- Different types of seismic velocities. Dix formula
PRINCIPLES OF MIGRATION
- Why migrate? The blind geophysicist’s experiment
- Different types of seismic rays (normal, zero offset,…)
- Construction of the time image from a simple geological model in depth
- Effects of migration: repositioning and focusing of the image
TIME & DEPTH IMAGING
- Different types of migration: 2D vs 3D, post vs. pre-stack, Time vs. depth
- Differences between pre-stack Time migration (PSTM) vs. depth migration (PSDM)
- Velocity model building for PSDM. Tomography
- Migration algorithms: seismic rays, wave equation
- Anisotropy, full waveform inversion (FWI)
- Overview of seismic acquisition and processing costs
BEYOND THE SEISMIC IMAGE: ATTRIBUTES AND INTERPRETATION
- The 3D seismic cube ready for interpretation: geometric and attributes information
- Structural interpretation and depth mapping
- Stratigraphic interpretation for reservoir characterization (seismic stratigraphy)
- Fluid interpretation for hydrocarbon identification (DHI)
Language
english, french, spanish
Audience type
Geosciences / Georesources students (Licence, Master) of Schools and Universities
Planned duration
5 days, 21 hours, can be adjusted 15 to 24 hours if needed
Support material
Power point presentations, interactive quiz (Wooclap), videos
Prerequisite
Fundamentals of Seismic signal, structural and stratigraphy geology
Objectives
This course, delivered as an integrated week (3 to 5 days), is the first part of the more general geophysical course delivered by TPA entitled: Geophysical Techniques and Methods applied to Hydrocarbons Exploration-Production but also and increasingly, to other geo-resources or geo-energies (geological storage of CO2, geothermal, offshore wind, …) After a review of the seismic reflection method principles, this course covers the different stages from the acquisition of seismic data to the depth imaging : Onshore/offshore acquisition techniques (2D/3D, NATS/ WAZ, OBC/OBN, broadband), the Time Processing (NMO, stack, seismic velocities), the Migration principles and effects, the main differences between a pre-stack time migrated and depth migrated seismic image in particular regarding the Velocity Model building. The course ends, as an introduction to the part 2, with an overview of the use made of this 3D seismic cube through structural, stratigraphic and fluid interpretations, leading to the 3D geological model of the subsurface to be explored.
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