wavelet extraction using seismic interferometry c. boonyasiriwat and s. dong november 15, 2007
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Wavelet Extraction Wavelet Extraction usingusing
Seismic Seismic InterferometryInterferometry
C. Boonyasiriwat and S. DongC. Boonyasiriwat and S. DongNovember 15, 2007November 15, 2007
OutlineOutline TheoryTheory Numerical ResultsNumerical Results
Synthetic Data TestSynthetic Data Test 10-Layer Model10-Layer Model Model with Mapleton TopographyModel with Mapleton Topography
Field Data TestField Data Test Mapleton DataMapleton Data
ConclusionConclusion Future WorkFuture Work
Field Data Test on North Sea DataField Data Test on North Sea Data VSP -> VSP CaseVSP -> VSP Case Statics Estimation for SSP -> SSP CaseStatics Estimation for SSP -> SSP Case
TheoryTheory
Virtual CSGVirtual CSG )(|)(|)( 2 GSPvirt
Real CSGReal CSG )()()( GSPreal
Extracted WaveletExtracted Wavelet
*
*
*
)()(
)()()(
realreal
realvirt
PP
PPS
Numerical ResultsNumerical Results
Synthetic Data TestSynthetic Data Test 10-Layer Model10-Layer Model Model with Mapleton TopographyModel with Mapleton Topography
Field Data TestField Data Test Mapleton DataMapleton Data
Original CSG vs. Virtual Original CSG vs. Virtual CSGCSG
Offset (meter)
Tim
e (
seco
nd
s)Original Shot Gather
0 1000 2000
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
Offset (meter)
Tim
e (
seco
nd
s)
Virtual Shot Gather
0 1000 2000
0
0.2
0.4
0.6
0.8
1
1.2
1.4
1.6
1.8
2
True Source vs. True Source vs. Extracted SourceExtracted Source
0 0.1 0.2 0.3 0.4 0.5-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
Time (seconds)
Am
plit
ud
eTrue Source Signature versus Extracted Source Signature
Extracted SourceTrue Source
Original CSG vs. Virtual Original CSG vs. Virtual CSGCSG
Offset (meter)
Tim
e (
seco
nd
s)Original Shot Gather
0 10 20
0
0.05
0.1
0.15
0.2
0.25
Offset (meter)
Tim
e (
seco
nd
s)
Virtual Shot Gather
0 10 20
0
0.05
0.1
0.15
0.2
0.25
True Source vs. True Source vs. Extracted SourceExtracted Source
0 0.01 0.02 0.03 0.04 0.05 0.06 0.07-1
-0.8
-0.6
-0.4
-0.2
0
0.2
0.4
0.6
0.8
1
Time (seconds)
Am
plit
ud
eTrue Source Signature versus Extracted Source Signature
Extracted SourceTrue Source
Mapleton DataMapleton Data Surface wave has relatively lower Surface wave has relatively lower
frequency than the P-wave signal.frequency than the P-wave signal. The extracted wavelet has low peak The extracted wavelet has low peak
frequency and narrower bandwidth frequency and narrower bandwidth compared to those of the data.compared to those of the data. The strong surface wave affected the The strong surface wave affected the
extracted wavelet.extracted wavelet.
ConclusionConclusion Seismic interferometry (SSP -> SSP Seismic interferometry (SSP -> SSP
case) can be utilized to extract a case) can be utilized to extract a source signature from a data set source signature from a data set itself without velocity information.itself without velocity information.
Further test will be done on the Further test will be done on the North Sea data.North Sea data.