Seismogram
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•
•
•
Relation between seismic trace and geology
Wavelets
Multiples
Resolution
– Vertical resolution
– Horizontal resolution
Seismogram of an earthquake
mid atlantic ridge measured in Brasil magnitude 5 (sept 2002) 3000km
Amplitude
Unfiltered:
Time (s)
Filtered:
P
PP
PcP
S
SS
Rayleigh
From geology to seismogram
Amplitude
Waves
t or x
1
Period τ ==--f
Wavelength λ
Period τ
Phase
2π
Wavenumber k = --λ
Velocity v
=
f⋅λ
2π
-----ω
Important wave forms
Zero-Phase
0 time
Minimum Phase
0 time
Minimum phase and zero-phase wavelet
Minimum phase wavelet:
Zero phase wavelet:
Energy is maximally front-loaded
(Energy does not arrive before zero time)
Symmetric with respect to zero time
and peaks at zero time
(Energy arrives also before zero time)
Important waveforms
Minimum Phase
Zero Phase
Display of Seismogram
Example of a shot
Reynolds, 1997
Multiples
Air gun record
Keary and Brooks
Surface
Riverbed
Sediment
Bedrock
Reynolds
Resolution
Resolution refers to the minimum separation
between two features such that we can tell that
there are two features rather than only one.
• Vertical resolution
• Horizontal resolution
Comparison of resolution of different data sets
30 Hz wave
at 2000 m/s
Big Ben (ca. 123 m)
gamma log
through oil field
(Emery and Myers)
Vertical resolution
Rayleigh’s-criterion:
λ
4
Vertical resolution depends on:
- Frequency
- Velocity
v
λ=
f
Resolution of two boundaries depends on wavelength
λ/4=12 ms
V1
V1
or
>
<
V2
>
<
V2
V3
V3
R12
R23
R12/R23= pos.
V1
or
>
<
V2
V1
V2
<
>
V3
V3
R12/R23= neg.
R12
R23
Horizontal resolution
z
w = 2zλ
w
for z>>λ
Sampling theorem
At least two samples per (horizontal) apparent
wavelength must be obtained in order to recognize
Features (remember the time sampling theorem!!).
For example, to recognize a stream channel on a
horizontal slice generally requires bin sizes no larger
than 1/3 or ¼ the channel width.