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Source separation on seismic data : application in a geophysical setting
Date Issued
2012-05
Date Available
2012-06-26T13:47:49Z
Abstract
This article gives a brief description of the Degenerate Unmixing Estimation Technique (DUET) and applies it in a geophysical setting. Source separation has not been fully
addressed by geophysicists and is a crucial first step to locating simultaneous sources, which in turn helps with understanding the
dynamics of the sources and their source mechanisms. DUET is applied to synthetic seismic signals. The source separation
method works successfully to separate two contemporary explosive sources, and two simultaneous oblique tensile cracks in a 3D
structural model of Mt Etna. The method is also applied to field recordings on Mt Etna from 2008. The method separates Long Period events from tremor, Long Period events from Volcano Tectonic events and different sources of tremor from each other.
addressed by geophysicists and is a crucial first step to locating simultaneous sources, which in turn helps with understanding the
dynamics of the sources and their source mechanisms. DUET is applied to synthetic seismic signals. The source separation
method works successfully to separate two contemporary explosive sources, and two simultaneous oblique tensile cracks in a 3D
structural model of Mt Etna. The method is also applied to field recordings on Mt Etna from 2008. The method separates Long Period events from tremor, Long Period events from Volcano Tectonic events and different sources of tremor from each other.
Sponsorship
Science Foundation Ireland
Type of Material
Journal Article
Publisher
Institute of Electrical and Electronic Engineers
Journal
IEEE Signal Processing Magazine
Volume
29
Issue
3
Start Page
16
End Page
28
Copyright (Published Version)
2012 IEEE
Subject – LCSH
Source separation (Signal processing)
Geophysics
Seismological stations
Volcanology
Language
English
Status of Item
Peer reviewed
This item is made available under a Creative Commons License
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Name
duetgeoloc.pdf
Size
4.9 MB
Format
Adobe PDF
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