Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals

In seismic tomography, the finite frequency content of broad-band data leads to interference effects in the process of medium reconstruction, which are ignored in traditional ray theoretical implementations. Various ways of looking at these effects in the framework of transmission tomography can...

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Main Authors: van der Hilst, Robert D., de Hoop, Maarten V., Shen, Peng
Other Authors: Massachusetts Institute of Technology. Earth Resources Laboratory
Format: Technical Report
Published: Massachusetts Institute of Technology. Earth Resources Laboratory 2012
Subjects:
Online Access:http://hdl.handle.net/1721.1/68030
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author van der Hilst, Robert D.
de Hoop, Maarten V.
Shen, Peng
author2 Massachusetts Institute of Technology. Earth Resources Laboratory
author_facet Massachusetts Institute of Technology. Earth Resources Laboratory
van der Hilst, Robert D.
de Hoop, Maarten V.
Shen, Peng
author_sort van der Hilst, Robert D.
collection MIT
description In seismic tomography, the finite frequency content of broad-band data leads to interference effects in the process of medium reconstruction, which are ignored in traditional ray theoretical implementations. Various ways of looking at these effects in the framework of transmission tomography can be found in the literature. Here,we consider inverse scattering of bodywaves to develop a method of wave-equation reflection tomography with broad-band waveform data— which in exploration seismics is identified as a method of wave-equation migration velocity analysis. In the transition from transmission to reflection tomography the usual cross correlation between modelled and observed waveforms of a particular phase arrival is replaced by the action of operators (annihilators) to the observed broad-bandwave fields. Using the generalized screen expansion for one-way wave propagation, we develop the Fréchet (or sensitivity) kernel, and show how it can be evaluated with an adjoint state method. We cast the reflection tomography into an optimization procedure; the kernel appears in the gradient of this procedure.We include a numerical example of evaluating the kernel in a modified Marmousi model, which illustrates the complex dependency of the kernel on frequency band and, hence, scale. In heterogeneous media the kernels reflect proper wave dynamics and do not reveal a self-similar dependence on frequency: low-frequency wave components sample preferentially the smoother parts of the model, whereas the high-frequency data are—as expected—more sensitive to the stronger heterogeneity.We develop the concept for acoustic waves but there are no inherent limitations for the extension to the fully elastic case.
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spelling mit-1721.1/680302019-04-10T13:16:04Z Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals van der Hilst, Robert D. de Hoop, Maarten V. Shen, Peng Massachusetts Institute of Technology. Earth Resources Laboratory van der Hilst, Robert D. Tomography In seismic tomography, the finite frequency content of broad-band data leads to interference effects in the process of medium reconstruction, which are ignored in traditional ray theoretical implementations. Various ways of looking at these effects in the framework of transmission tomography can be found in the literature. Here,we consider inverse scattering of bodywaves to develop a method of wave-equation reflection tomography with broad-band waveform data— which in exploration seismics is identified as a method of wave-equation migration velocity analysis. In the transition from transmission to reflection tomography the usual cross correlation between modelled and observed waveforms of a particular phase arrival is replaced by the action of operators (annihilators) to the observed broad-bandwave fields. Using the generalized screen expansion for one-way wave propagation, we develop the Fréchet (or sensitivity) kernel, and show how it can be evaluated with an adjoint state method. We cast the reflection tomography into an optimization procedure; the kernel appears in the gradient of this procedure.We include a numerical example of evaluating the kernel in a modified Marmousi model, which illustrates the complex dependency of the kernel on frequency band and, hence, scale. In heterogeneous media the kernels reflect proper wave dynamics and do not reveal a self-similar dependence on frequency: low-frequency wave components sample preferentially the smoother parts of the model, whereas the high-frequency data are—as expected—more sensitive to the stronger heterogeneity.We develop the concept for acoustic waves but there are no inherent limitations for the extension to the fully elastic case. TOTAL (Firm) National Science Foundation (U.S.) (grant EAR-0409816) 2012-01-06T19:50:38Z 2012-01-06T19:50:38Z 2007 Technical Report http://hdl.handle.net/1721.1/68030 Earth Resources Laboratory Industry Consortia Annual Report;2007-16 application/pdf Massachusetts Institute of Technology. Earth Resources Laboratory
spellingShingle Tomography
van der Hilst, Robert D.
de Hoop, Maarten V.
Shen, Peng
Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title_full Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title_fullStr Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title_full_unstemmed Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title_short Wave-Equation Reflection Tomography: Annihilators and Sensitivity Kernals
title_sort wave equation reflection tomography annihilators and sensitivity kernals
topic Tomography
url http://hdl.handle.net/1721.1/68030
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