Synopsis Flashcards
Causes of seismic noise
Random Noise: • Wind - notably in desert & near trees • Industry • Roads, trains (also electrical pick-up) • Surf zone - coastal areas • High tension power lines & plants • Nightlife
Organised Noise:
• Groundroll • Near surface scattering • Shallowrefractions • Shallow reverberations
2 D over 3 D Survey
2D • Cheap • Simpleoperation • Straight processing • Seriousimaging/ subsurface positioning problems
3D • Not so cheap • Possiblycomplex operation • Straight processing possible, yet often complicated processing is needed • Considerably less imaging problems
Fundamental criteria & requirements of the survey
- Desired spatial resolution
- Subsurface geometry & depth of objective(s)
- Envisaged processing sequence, AVO, inversion etc
- Choice of acquisition geometry
- Environmental & logistical issues
!!!!Depth and nature of objective(s) determines acquisition geometry !!!!!!
5 major Phases - classical séquences
- Pre-processing1. Merge of field tapes with obs. logs, topo, bad trace editing
- Pre-stack processing2. Statics, deconvolution, velocity derivation and application
- Post-stack processing3. NMO correction, stacking and deconvolution
- Imaging (Migration)4. Imaging and bandpass filtering
- Archiving
- Tape & report generation
How to –> eliminate unwanted signal
Filtering-k/f
Bandpass
How to suppress random noise
stacking
How to focus and position better the seismic image
Imaging and migration
CMP vs CDP
CMP = smear
loss of resolution
improper position
CDP = better to image before stacking !
Time domaine VS Depth domain
T-domaine =
- Straightforward from recorded traces
- Relative simple operators
- One-pass operations
Depth-domaine =
• Depth model needed
• No straightforward operators
• Layer-by layer approach
Post stack vs Prestack
Post =
Fast and Cheap
One-pass operation
Error prone
Prestack =
Expensive & time consuming
Iterative opé (répétitif)
Best available

Minimum and Zero Phase wavelet
Minimum Phase Wavelet:
a) Physically realizable
b) Highly asymmetric
c) Very difficult to pick when dealing with low frequencies and low amplitudes
d) All the energy is “front-loaded”, and the time-lag between “zero-time” and the peak of the main
pulse is not constant
Zero Phase Wavelet: The only meaningful signal
a) Unphysical
b) It peaks at time=0
c) Its peak representative for reflection coefficient
d) It is easier to interpret as the reflection time is exactly at the peak of the main amplitude.
e) The wider the frequency band, the sharper the signal