A short note on phase and amplitude tracking for seismic event separation

We propose a method for decomposing a seismic record into atomic events defined by a smooth phase and a smooth amplitude. The method uses an iterative refinement-expansion tracking scheme to minimize the highly nonconvex objective function. We demonstrate the proposed method on a noisy synthetic rec...

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Main Authors: Li, Yunyue, Demanet, Laurent
Other Authors: Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Format: Article
Published: Society of Exploration Geophysicists 2018
Online Access:http://hdl.handle.net/1721.1/115507
https://orcid.org/0000-0003-4225-2735
https://orcid.org/0000-0001-7052-5097
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author Li, Yunyue
Demanet, Laurent
author2 Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
author_facet Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences
Li, Yunyue
Demanet, Laurent
author_sort Li, Yunyue
collection MIT
description We propose a method for decomposing a seismic record into atomic events defined by a smooth phase and a smooth amplitude. The method uses an iterative refinement-expansion tracking scheme to minimize the highly nonconvex objective function. We demonstrate the proposed method on a noisy synthetic record from the shallow Marmousi model. Finally, we show an application of our method to low frequency extrapolation on the same record. This note is a short version of Li and Demanet (2015).
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spelling mit-1721.1/1155072022-09-28T16:27:17Z A short note on phase and amplitude tracking for seismic event separation Li, Yunyue Demanet, Laurent Massachusetts Institute of Technology. Department of Earth, Atmospheric, and Planetary Sciences Massachusetts Institute of Technology. Department of Mathematics Li, Yunyue Demanet, Laurent We propose a method for decomposing a seismic record into atomic events defined by a smooth phase and a smooth amplitude. The method uses an iterative refinement-expansion tracking scheme to minimize the highly nonconvex objective function. We demonstrate the proposed method on a noisy synthetic record from the shallow Marmousi model. Finally, we show an application of our method to low frequency extrapolation on the same record. This note is a short version of Li and Demanet (2015). TOTAL (Firm) United States. Air Force. Office of Scientific Research United States. Off National Science Foundation (U.S.) 2018-05-18T19:08:15Z 2018-05-18T19:08:15Z 2015 2018-05-17T17:42:19Z Article http://purl.org/eprint/type/ConferencePaper 1949-4645 http://hdl.handle.net/1721.1/115507 Li, Yunyue Elita, and Laurent Demanet. “A Short Note on Phase and Amplitude Tracking for Seismic Event Separation.” SEG Technical Program Expanded Abstracts 2015 (August 19, 2015). https://orcid.org/0000-0003-4225-2735 https://orcid.org/0000-0001-7052-5097 http://dx.doi.org/10.1190/SEGAM2015-5848430.1 SEG Technical Program Expanded Abstracts 2015 Creative Commons Attribution-Noncommercial-Share Alike http://creativecommons.org/licenses/by-nc-sa/4.0/ application/pdf Society of Exploration Geophysicists MIT Web Domain
spellingShingle Li, Yunyue
Demanet, Laurent
A short note on phase and amplitude tracking for seismic event separation
title A short note on phase and amplitude tracking for seismic event separation
title_full A short note on phase and amplitude tracking for seismic event separation
title_fullStr A short note on phase and amplitude tracking for seismic event separation
title_full_unstemmed A short note on phase and amplitude tracking for seismic event separation
title_short A short note on phase and amplitude tracking for seismic event separation
title_sort short note on phase and amplitude tracking for seismic event separation
url http://hdl.handle.net/1721.1/115507
https://orcid.org/0000-0003-4225-2735
https://orcid.org/0000-0001-7052-5097
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