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4D Interferometric Traveltime Tomography
Yuqing Chen King Abdullah University of Science and Technology 11/12/2015
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Outlines 1.Theory part Numerical Test Problem (also opportunities)
Further plan
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Theory
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Theory Pre Fluid Post Fluid
With time elapse , The velocity of the layer changes…
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Theory Pre Fluid Post Fluid
With time elapse , The velocity of the layer changes…
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Advantage Multiples are more sensitivity to velocity change.
Eliminate source and receiver statics
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Method Instead of Raytracing, using approximate WET (wave path eikonal traveltime inversion) method to implement this method. Source side traveltime table: Receiver side traveltime table:
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Method Add them together: Subtract observe time:
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Method Cigar Rabbit ear Snake
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Method Raytracing AWET
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Numerical Test
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Numerical Result
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Static Test Update first layer Add static in traveltime Residual curve
Similarity
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First Layer Change Test
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Second Layer Change Test
Absolute time= Global velocity anomalies Differential time= Local velocity anomalies
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Second Layer Change Test
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Both Layer Change
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(Left) Trace 20 & Residual curve (up)
Both Layer Change Layer 1 (Left) Trace 20 & Residual curve (up)
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(Left) Trace 20 & Residual curve (up)
Both Layer Change Layer 2 (Left) Trace 20 & Residual curve (up)
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Problem (or opportunities)
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Problem 1: Convergence Property
Approximate of Hessian of Multiples Approximate of Hessian of Reflection The difference of between the above two Hessian
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Problem 2 : Traveltime Prediction
The way we predict reflection and multiples
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Problem 2 : Traveltime Prediction
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Problem 2 : Traveltime Prediction
Refraction Refraction-Reflection
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Problem 2 : Traveltime Prediction
Refraction multiples Refraction multiples
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Problem 2 : Traveltime Prediction
Gradient of Multiples Refraction of Reflection
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Problem 2 : Traveltime Prediction
Initial model True model
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Problem 2 : Traveltime Prediction
Initial model Inversion result
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Problem 2 : Traveltime Prediction
(Left) Trace 20 & Residual curve (up)
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Future Plan
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Further plan Real Data Test: Resonant Multiples Refraction Multiples
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