Marine Seismic Acquisition
Marine Seismic Acquisition
Introduction
Discussion
« Conventionnal » seismic
Target depth ≅ X 1000 m
Target size ≅ X 100 m
Deep scientific / industrial exploration
High Resolution
Target depth ≅ X 100 m
Target size ≅ X 10 m
Fluid escape, gaz hydrates,
reservoir modelling
Log10 (FHertz)
-2 -1 0 1 2 3 4
7 Natural seismicity
5 « Conventionnal » seismic
Log10 (Métres)
4
HR seismic
3
VHR seismic
-1
Log10 (FHertz)
-2 -1 0 1 2 3 4
Natural seismicity
Explosives
Air guns
Water guns
« Conventionnal » seismic
Sparkers
HR seismic
Electro-acoustic transducers
Boomers
VHR seismic
Air delivery
¾ 4 * 300 m3/h
¾ 1 * 660 m3/h
Seismic source
Acquisition system
¾ Acquisition management
- Sampling rate : 4ms, 2 ms, 1 ms, 0.5 ms
- Data format SEGD 2
- Storage media : DLT
¾ Streamer control
ECOS workstation
¾ SUN Ultra 60
¾ Storage media :
- DLT
- 70 Gb hard disks
N/O NADIR
Deep structure of the Angolan Margin : “Source and acquisition design for deep imaging”
¾ The “monobulle” source : ”bubble” tuning versus “peak” tuning
¾ Acquisition configuration : combined seismic reflection and refraction (OBS) studies
Gas hydrates studies in the Nankai Trough : “What long offsets can bring us”
¾ Amplitude variations with offsets and AVA analysis
¾ Acquisition configuration
¾ Subsalt imaging
¾ Processing
Amplitude
Amplitude
Time Time
Amplitude
Amplitude
The « monobulle » source consists in
tuning the different guns on the main
Time Time
bubble instead of on the first peak, thus
allowing to increase low frequency
acoustic level. 50 50
dB
dB
30 30
10 10
0 50 100 Hz 0 50 100 Hz
Frequency Frequency
4500 metres
Seismic reflection
• Source : 4802 inch3
• Shot spacing : 100 m
• Air delivery : 992m3/h
75 inch3 9L 9L 9L 9L
5 s Twt
Corresponding composite oil exploration section
Bassin du Bas Congo
Bassin du Kwanza
5 s Twt
from Maryline Moulin,
Thèse Univ. Brest, 2003
Refraction data
Reflection data
Gravimetry data
EGU - Nice, France, 25-30 April 2004
Marine Seismic Acquisition
« Conventionnal » seismic data examples
0 10 20 30 km
500
1000
Gas hydrates studies in the Nankai Trough : Amplitude Versus Offset anomalies
Twt (ms)
Depth (m)
1600
1000
Gas hydrates studies in the Nankai Trough : Amplitude Versus Angle anomalies
0.9
0.8
Reflection coefficient
0.7
0.6
0.5
0.4
0.3
0.2
0.1
0.
0 10 20 30 40 50 60
Breakthroughs
¾ 2D High Resolution seismic exploration / 3D detailed survey
¾ kinematics processing / amplitude processing and inversion
¾ multidisciplinary studies
¾ multi-frequency and multi-scale studies
¾ Operational system
¾ Amplitude control
¾End-user requirement
⇒ Integrated approach
EGU - Nice, France, 25-30 April 2004
Marine Seismic Acquisition
2D HR seismic layout
¾ Source: Sparker
¾ Operating vessel: N/O L’Europe
Equipment
¾ SEAL seismic acquisition system (SERCEL)
¾ Numerical streamers on two winches
¾ Shot control unit (bubble cancelled air guns, flip/flop shooting mode)
¾ Oiling system of guns for high shooting rate (< 5 s)
Integration
¾ 10" acquisition container remotely controlled
¾ Interface with on-board navigation system
Depth controller
Navigation • Pre-processing
control unit • Automatic signal analysis
Archive
Seismic
recording / QC
Bathymetry (3D)
3D stack
(X,Y) position + Z coordinate Navigation and
⇒ Navigation quality control seismic Quality
control
SEGD file
Navigation Seismic
2D survey:
¾ one streamer of 120 traces
¾ one array of two mini-GI air guns
¾ shooting rate: 6 s
¾ source immersion: 1.5 m / streamer immersion: 3 m
3D survey:
¾ two streamers of 48 traces
¾ two arrays of one mini-GI air gun
¾ shooting rate: 3 s
¾ source immersion: 1.5 m / streamer immersion: 3 m
2D survey:
¾ one streamer of 72 traces
¾ shooting rate: 3 s
¾ source immersion: surface / streamer immersion: 2 m
EGU - Nice, France, 25-30 April 2004
Marine Seismic Acquisition
Hydratech cruise - 2D HR seismic
3D
1000 m
1500 m
Data set
¾ profile length: 8 km
¾ 173 recorded profiles, 12 days
¾ 7700 x 3400 m (25 km²), 150 Gb
sailed lines fold map
3D seismic interpretation
800 m
fluid escape
1 km structure
seismic
horizon
1000 m
Depth
1200 m
BSR
1400 m fault
undisturbed
sediments
disturbed
sediments
2 km
Detailed mapping of the most recent evidence of slope instability – Sismage software courtesy of Total
7.5 km
Seismic layout:
¾ Coastal vessel (N/O L’Europe)
¾ One streamer of 72 traces
¾ One Sparker source Bathymetry
(m)
Performance:
¾ Vertical resolution 1 m
¾ Horizontal resolution 3 m
North
Geological settings
Extension of the Golo sedimentary system,
system, from
3D view of the bathymetry (EM300) A. Gervais and T. Mulder (University of Bordeaux)
Bordeaux)
340
Head of Golo canyon
2D Migrated section
(2001, N/O L’Europe)
415
depth (m)
490
565
3 km
W E
10 km
790
depth (m)
(2003, N/O L’Europe)
940
1015
Further evolution
¾Increase streamer length to 6000 meters
¾Tail buoy
- Increase offset (800 metres)
- Positioning accuracy
¾ Additional active sections
- 2D (120 traces)
- 3D (2 * 72 traces)
¾Source monitoring (air pressure, calibrated hydrophones) for
amplitude processing
Source monitoring
¾ Source modelling through near field measurements
¾ Gun control
Quality control
¾ Definition of a standard Quality Control sequence (SMT, HR, SISRAP)
¾ Development of Quality Control tools
- Navigation data
- Seismic data