Synopsis Flashcards

1
Q

Causes of seismic noise

A
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
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2
Q

2 D over 3 D Survey

A
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
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3
Q

Fundamental criteria & requirements of the survey

A
  • 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 !!!!!!

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4
Q

5 major Phases - classical séquences

A
  1. Pre-processing1. Merge of field tapes with obs. logs, topo, bad trace editing
  2. Pre-stack processing2. Statics, deconvolution, velocity derivation and application
  3. Post-stack processing3. NMO correction, stacking and deconvolution
  4. Imaging (Migration)4. Imaging and bandpass filtering
  5. Archiving
  6. Tape & report generation
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5
Q

How to –> eliminate unwanted signal

A

Filtering-k/f

Bandpass

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6
Q

How to suppress random noise

A

stacking

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7
Q

How to focus and position better the seismic image

A

Imaging and migration

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8
Q

CMP vs CDP

A

CMP = smear
loss of resolution
improper position

CDP = better to image before stacking !

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9
Q

Time domaine VS Depth domain

A

T-domaine =

  • Straightforward from recorded traces
  • Relative simple operators
  • One-pass operations

Depth-domaine =
• Depth model needed
• No straightforward operators
• Layer-by layer approach

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10
Q

Post stack vs Prestack

A

Post =
Fast and Cheap
One-pass operation
Error prone

Prestack =
Expensive & time consuming
Iterative opé (répétitif)
Best available



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11
Q

Minimum and Zero Phase wavelet

A

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

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