Title: The Marmousi2 Elastic Model and Synthetic Data
1The Marmousi2 Elastic Model and Synthetic Data
- SEG Annual Meeting
- October 2003
Gary Martin, GX Technology Robert Wiley and Kurt
Marfurt, AGL/University of Houston
2Outline
- Introduction
- The Marmousi2 model
- Marmousi2 acquisition
- Marmousi2 synthetic data
- Processing and migration examples
- Conclusion
3Introduction
- This work has been performed as part of the Next
Generation Numerical Modeling and Imaging
project. - New suite of shared seismic models
- Update the popular and very useful Marmousi model
using modern computing power.
4The Marmousi2 Model
5Original Marmousi
- Geologic Model
- Created in 1988 by IFP
- Based on real geology from West Africa (Angola)
- Complex model (160 layers)
- 9.2 km x 3 km
- Simulation
- Acoustic simulation using a second order (in time
and space) finite difference algorithm - 4m grid size, frequencies up to 55Hz
- Maximum offset 2.5 km
6Marmousi2
- Model
- Larger model (2X length)
- Deep water (450m)
- Longer offsets (up to 17km)
- Hydrocarbons with AVO effects
- Stratigraphic features
7Marmousi models
8Lithology and Features
9Layer Properties
- Determined by lithology, fluid content, and
original Marmousi P-wave velocity.
- Lithologies
- Sand
- Shale
- Marl
- Salt
- Fluids
- Water
- Gas
- Oil (varying GOR)
10P-wave Velocity
- Extracted from original Marmousi model
- Modifications for
- Hydrocarbon saturated layers
- Salt velocity, reduced to 4500m/s
- Velocity parameterization
- Constants
- Vertical velocity gradients
- P-wave velocity is the source for both density
and S-wave transforms
11P-wave Velocity
km/s
1
2
3
4
5
12S-wave Velocity
- Determined directly from P-wave velocity using
Greenburg and Castagna (1992) - Sand Vs 0.804Vp 856
- Shale Vs 0.770Vp 867
- Limestone Vs 1.017Vp 0.055Vp2 1030
- Marl
- 30 limestone, 70 shale
- Using mixing laws and effective medium theory
m/s
13S-wave Velocity
km/s
0
1
2
3
14Density
- Determined directly from P-wave velocity using
Castagnas (1993) transforms - Sand r 0.2736Vp.261
- Shale r 0.2806Vp.265
- Limestone r 0.3170Vp.225
- Marl
- 30 limestone, 70 shale
- Using mixing laws and effective medium theory
g/cm3 and m/s
15Density
g/cm3
1.0
1.5
2.0
2.0
2.5
3.0
16Hydrocarbons
- Gas and oil emplaced into some sand layers.
- 5 gas sands
- 3 oil sands
- 1 oil and gas cap
- Fluid substitution used to provide realistic
properties that will be useful for AVO
calibration. - Seismic responses verified using simplified
models and ray-tracing.
17Data Acquisition
18Marmousi2 Acquisition
- Acquisition objectives
- Elastic simulation.
- Simultaneous streamer, OBC, and VSP acquisition.
- Multi-component recording for OBC and VSPs.
- Record Wave-front snapshots.
- Reflecting boundary at free surface.
19Acquisition Geometry
20Source
- An Ormsby wavelet with frequencies up to 80 Hz,
(5-10, 60-80).
Near field
Far field
21Computation Considerations
- Grid size
- To ensure adequate sampling (to prevent numerical
problems) a grid size of 1.25m was required.
Marmousi grid 4m x 4m
Marmousi2 grid 1.25m x 1.25m
22Computation
- Algorithm
- E3D National Labs. elastic modeling code
- 2nd order time, 4th order space finite difference
elastic modeling - Computation Time
- Sun 6800 Starfire system at UH
- 20 CPUs for 5 months
- 4 ½ CPU days per shot
- Total hours 70,000 8 CPU years
23Marmousi2 Synthetic Data
24Synthetic Data
- Wavefront snapshots
- Synthetic Shot Records
- Streamer
- OBC
- VSP
25Wave Propagation Example
2
Shot 2 Complex Geology, x9000
26Shot 2 Complex Geology
time
0
27Shot 2 Complex Geology
time
0.25
28Shot 2 Complex Geology
time
0.50
29Shot 2 Complex Geology
time
0.75
30Shot 2 Complex Geology
time
1.00
31Shot 2 Complex Geology
time
1.25
32Shot 2 Complex Geology
time
1.50
33Shot 2 Complex Geology
time
1.75
34Shot 2 Complex Geology
time
2.00
35Shot 2 Complex Geology
time
2.25
36Shot 2 Complex Geology
time
2.50
37Shot 2 Complex Geology
time
2.75
38Shot 2 Complex Geology
time
3.00
39Shot 2 Complex Geology
time
3.25
40Shot 2 Complex Geology
time
3.50
41Shot 2 Complex Geology
time
3.75
42Shot 2 Complex Geology
time
4.00
43Shot Record Examples
1
2
44Shot 1 Streamer and OBC Pressure
-4 Offset (km)
8 -4 Offset (km)
8
0
Streamer pressure
OBC pressure
t (s)
4
45Shot 1 OBC Velocity components
-4 Offset (km)
8 -4 Offset (km)
8
0
Vx
Vz
t (s)
4
46Shot 1 VSP records at offset500m
3.5 Z (km) 0 3.5
Z (km) 0 3.5 Z (km)
0
0
t (s)
4
pressure
Vx
Vz
47Shot 2 Streamer and OBC Pressure
-4 Offset (km)
8 -4 Offset (km)
8
0
Streamer pressure
OBC pressure
t (s)
4
48Shot 2 OBC Velocity components
-4 Offset (km)
8 -4 Offset (km)
8
0
Vx
Vz
t (s)
4
49Shot 2 VSP records at offset500m
3.5 Z (km) 0 3.5
Z (km) 0 3.5 Z (km)
0
0
t (s)
4
pressure
Vx
Vz
50Data Sets
- Four datasets are available from UH
- Full dataset (all offsets, all components)
- Acoustic dataset (all offsets)
- A 6km acoustic towed streamer subset
- Wavefront snapshots
- A Marmousi2 website is being created
- www.uh.edu/Geosciences/Marmousi2 ??
51Processing and Migration Examples
52Processing and Migration Examples
- Using the 6km acoustic streamer subset
- Minimum processing
- Correct for source/receiver depths
- Shift data by 72ms (correct for wavelet)
- NMO/Stack
- Poststack time migration
- Poststack depth migration
- Prestack time migration
- Prestack depth migration
53Simple NMO/Stack
54ProMAX Stolt PoSTM
55ProMAX Kirchhoff PoSDM
56PrimeTime Kirchhoff PreSTM
57Primus Kirchhoff PreSDM
Shortest path
58Primus Kirchhoff PreSDM
Max energy
59Optimus Wave Equation PreSDM
60Conclusion
61Conclusion
- A complex structure 2D elastic model with
realistic hydrocarbons and stratigraphic features
has been created. - A high quality elastic finite difference
synthetic data set has been created. - Model and data are freely available.
62Conclusion
- Uses
- AVO calibration
- Velocity estimation
- Migration algorithm evaluation
- Multi-component and VSP evaluation
- Multiple suppression, etc.
- Limitations
- Model and data are 2D.
63Acknowledgements
- GX Technology Corporation
- Don Larson, GX Technology
- Aline Bougeois, IFP
- Fred Hilterman, GDC