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Monitoring the Groningen gas field by seismic noise interferometry
W. Zhou
,
H. Paulssen
Seismology
Seismology
IVAU: Instituut voor Aardwetenschappen Utrecht
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Dive into the research topics of 'Monitoring the Groningen gas field by seismic noise interferometry'. Together they form a unique fingerprint.
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Keyphrases
Geophone
100%
Groningen Gas Field
100%
Seismic Noise Interferometry
100%
Travel Time
37%
P-wave
37%
Velocity Structure
37%
P-wave Velocity
25%
S-velocity
25%
Shear Wave
25%
Netherlands
12%
Borehole
12%
Wave Velocity
12%
Borehole Data
12%
Maximum Likelihood
12%
Ambient Noise
12%
Seismic Interferometry
12%
Bandpass Filter
12%
Social Noise
12%
P-velocity
12%
Probability Density Function
12%
Seismic Velocity Structure
12%
Reservoir Level
12%
Gas Field
12%
Deep Borehole
12%
Well Log Data
12%
Kernel Density Estimation
12%
Vertical Component
12%
Wave Travel Time
12%
Reflected Wave
12%
Induced Seismicity
12%
Noise Interferometry
12%
Spectral Whitening
12%
Weekly Variation
12%
1-bit
12%
Normalized Cross Correlation
12%
Natural Frequency
12%
Earth and Planetary Sciences
Gas Field
100%
Interferometry
100%
Geophone
100%
Seismic Noise
100%
Cross Correlation
87%
Travel Time
50%
Velocity Structure
50%
Borehole
25%
Wave Velocity
25%
P Wave
25%
Netherlands
12%
Ambient Noise
12%
Probability Density Function
12%
Induced Seismicity
12%
Reflected Wave
12%
Bandpass Filter
12%
Well Logging
12%
Engineering
Gas Field
100%
Geophone
100%
Interferometry
100%
Crosscorrelation
87%
Borehole
25%
Wave Velocity
25%
Good Agreement
12%
Maximum Likelihood
12%
Gaussians
12%
Well Logging
12%
Bandpass Filter
12%
Seismicity
12%
Resonant Frequency
12%
Probability Density Function
12%
Reflected Wave
12%
Physics
Cross Correlation
100%
Interferometry
100%
P Wave
71%
S Wave
42%
Wave Velocity
28%
Bandpass Filter
14%
Induced Seismicity
14%
Gaussian Distribution
14%
Ambient Noise
14%
Seismic Velocity
14%
Resonant Frequency
14%
Reflected Wave
14%