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![Page 1: Deep$learning$seismic$tomography - sesaai.stanford.edu · Velocity$model$building$(tomography) • Estimate(subsurface(wave(speed(from(seismic(data • Arguably(the(most(important(and(difficult(task(in(exploration(geophysics](https://reader030.fdocuments.in/reader030/viewer/2022040622/5d25ccb288c993e5378c321e/html5/thumbnails/1.jpg)
Deep learning seismic tomographyMauricio Araya-‐Polo (Shell), Joseph Jennings* (Shell, Stanford) and Stuart Farris (Stanford)
March 30, 2018
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Velocity model building (tomography)
• Estimate subsurface wave speed from seismic data
• Arguably the most important and difficult task in exploration geophysics
• Common approaches:1. Refraction/reflection tomography
2. Full waveform inversion
2
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J(m) =1
2||f(m)� d
obs
||22
Formulation of tomography problem
-‐ velocity model
-‐ Recorded data
-‐ Predicted data
mdobs
• models synthetic data via the wave/Eikonal equation
• Solved using gradient-‐based optimization techniques
• Computationally demanding
3
f(m)
f(m)
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Oberved data ( )dobs
4
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Velocity model ( ) from tomography
(Almomin, 2016)
m
5
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Another perspective on tomography
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is known deterministicallyf(m)
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Statistical learning
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f : X ! Y X
Y
-‐ Random input vector (observed data)
-‐ Random output variable (velocity models),
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Statistical learning
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f : X ! Y X
Y
-‐ Random input vector (observed data)
-‐ Random output variable (velocity models)
argminf
L(Y, f(X)) L(Y, f(X)) -‐ Loss function,
,
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Statistical learning
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f : X ! Y X
Y
-‐ Random input vector (observed data)
-‐ Random output variable (velocity models)
argminf
L(Y, f(X)) L(Y, f(X)) -‐ Loss function,
,
L(Y, f(X)) = (Y � f(X))2 (squared error loss)
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Statistical learning
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f : X ! Y X
Y
-‐ Random input vector (observed data)
-‐ Random output variable (velocity models)
argminf
L(Y, f(X)) L(Y, f(X)) -‐ Loss function,
,
L(Y, f(X)) = (Y � f(X))2
) f(x) = E(Y |X = x)
(squared error loss)
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A different perspective on tomography
Estimated via statistical learningmethods
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Deep learning as a seismic imaging tool
• 2D fault prediction from shot gathers – (Zhang, C. et al., 2014)
• 3D fault prediction from shot gathers – (Araya-‐Polo, M. et al., 2017)
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Why deep learning for velocity estimation?
• Potential for less computational burden
• Automated (no human-‐curated analysis of gathers)
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Deep learning training workflow
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(Y )
(X)
argminf
L(Y, f(X))
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Deep learning training workflow
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(Y )
(X)
argminf
L(Y, f(X))
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Features for deep-‐learning tomography
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Choosing the feature
• Suspected poor performance on raw data and dimensionality issues
• Many seismic attributes from which to choose
• Cheap to compute
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Semblance (velocity spectrum)
• A basic velocity analysis tool (Taner and Koehler, 1969)
• Contains “apparent velocity” information
• Cheap to compute
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Earth Model
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Seismic Experiment
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Seismic Experiment
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Seismic Experiment
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Common midpoint gather (CMP)
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Synthetic CMP (muted direct arrival)
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• Data redundancy
Synthetic CMP (muted direct arrival)
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Synthetic CMP (NMO hyperbola)
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NMO-‐corrected CMP ( )
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NMO-‐corrected CMP ( )
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NMO-‐corrected CMP ( )
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for
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q
q[j, k]
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for
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Stack over offset
q
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for
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Stack over offset
q
Smooth along time
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Semblance
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• -‐ NMO-‐corrected image
for a particular velocity
• -‐ time index
• -‐ offset index
• -‐ output index
• -‐ length of smoothing window
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Semblance
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• -‐ NMO-‐corrected image
for a particular velocity
• -‐ time index
• -‐ offset index
• -‐ output index
• -‐ length of smoothing window
Stack over offsetSmooth in time
Normalization
![Page 35: Deep$learning$seismic$tomography - sesaai.stanford.edu · Velocity$model$building$(tomography) • Estimate(subsurface(wave(speed(from(seismic(data • Arguably(the(most(important(and(difficult(task(in(exploration(geophysics](https://reader030.fdocuments.in/reader030/viewer/2022040622/5d25ccb288c993e5378c321e/html5/thumbnails/35.jpg)
Semblance (velocity spectrum)
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Training data
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X
Y
(feature)
(label)
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Deep learning training workflow
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(Y )
(X)
argminf
L(Y, f(X))
![Page 38: Deep$learning$seismic$tomography - sesaai.stanford.edu · Velocity$model$building$(tomography) • Estimate(subsurface(wave(speed(from(seismic(data • Arguably(the(most(important(and(difficult(task(in(exploration(geophysics](https://reader030.fdocuments.in/reader030/viewer/2022040622/5d25ccb288c993e5378c321e/html5/thumbnails/38.jpg)
Deep neural network training
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Training the network• 10,000 synthetic pseudorandom velocity models- 80% training, 20% testing
• Squared error loss:
• Metrics: Structual similarity index (SSIM) and score
39
L(Y, f(X)) = (Y � f(X))2
R2
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SSIM
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SSIM
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x
y1
• Compares mean and standard deviation within window
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SSIM
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x
y1
• Compares mean and standard deviation within window
• Mean SSIM ( ) average of SSIM for all windowsMSSIM
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• Compares mean and standard deviation within window
• Mean SSIM ( ) average of SSIM for all windows
• , MSSIM 1
SSIM
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x
y1
MSSIM = 0.14
MSSIM
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SSIM
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x
y2
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SSIM
45
x
MSSIM = 0.84
y2
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Training results
46
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Deep learning testing workflow
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Test set (20% of the total data)
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Deep learning testing results
48
MSSIM = 0.66170
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Deep learning testing resultsMSSIM = 0.72079
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Deep learning testing resultsMSSIM = 0.78219
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Deep learning testing resultsMSSIM = 0.76253
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FWI results
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MSSIM = 0.49666
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Deep learning testing results
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MSSIM = 0.66170
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Multiscale FWI results
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MSSIM = 0.84702
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DNN vs multiscale FWI results
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MSSIM = 0.66170 MSSIM = 0.84702
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Conclusions/future work
• We estimated a tomography operator via deep learning
• Semblance was the input feature
• Extend the method to 3D data
• Test on real data
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Questions?
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SStot
=mX
i=1
(yi � µy)2
Coefficient of determination
R2 = 1� SSres
SStot
58
(R2)
where,
Variance in the labels
Error in prediction
,
,
,SSres =mX
i=1
(yi � f(xi))2
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SStot
=mX
i=1
(yi � µy)2
Coefficient of determination
R2 = 1� SSres
SStot
59
(R2)
where,
Variance in the labels
Error in prediction
,
,
,SSres =mX
i=1
(yi � f(xi))2
![Page 60: Deep$learning$seismic$tomography - sesaai.stanford.edu · Velocity$model$building$(tomography) • Estimate(subsurface(wave(speed(from(seismic(data • Arguably(the(most(important(and(difficult(task(in(exploration(geophysics](https://reader030.fdocuments.in/reader030/viewer/2022040622/5d25ccb288c993e5378c321e/html5/thumbnails/60.jpg)
SStot
=mX
i=1
(yi � µy)2
Coefficient of determination
R2 = 1� SSres
SStot
60
(R2)
where,
Variance in the labels
Error in prediction
,
,
,SSres =mX
i=1
(yi � f(xi))2
![Page 61: Deep$learning$seismic$tomography - sesaai.stanford.edu · Velocity$model$building$(tomography) • Estimate(subsurface(wave(speed(from(seismic(data • Arguably(the(most(important(and(difficult(task(in(exploration(geophysics](https://reader030.fdocuments.in/reader030/viewer/2022040622/5d25ccb288c993e5378c321e/html5/thumbnails/61.jpg)
Coefficient of determination
• zero error (we fit the data perfectly)
• no learning occurred. We predict
• we perform worse than just predict
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(R2)
R2 = 1� SSres
SStot
R2 = 1 )
R2 = 0 ) µy
µyR2 < 0 )
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Deep learning testing results
4
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