The nature of particle motion in regional seismograms and its utilization for phase identification

The particle motion of regional arrivals is frequently treated in automatic phase-recognition schemes as that appropriate to simple P or S waves incident on an elastic, laterally homogeneous half-space. This model implies that the motion in ‘ P -type’ phases can be described in terms of a single, ge...

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Published in:Geophysical Journal International
Main Authors: Der, Zoltan A., Baumgardt, Douglas R., Shumway, Robert H.
Format: Text
Language:English
Published: Oxford University Press 1993
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/115/3/1012
https://doi.org/10.1111/j.1365-246X.1993.tb01506.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:115/3/1012 2023-05-15T17:05:03+02:00 The nature of particle motion in regional seismograms and its utilization for phase identification Der, Zoltan A. Baumgardt, Douglas R. Shumway, Robert H. 1993-12-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/115/3/1012 https://doi.org/10.1111/j.1365-246X.1993.tb01506.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/115/3/1012 http://dx.doi.org/10.1111/j.1365-246X.1993.tb01506.x Copyright (C) 1993, Oxford University Press Articles TEXT 1993 fthighwire https://doi.org/10.1111/j.1365-246X.1993.tb01506.x 2016-11-16T17:05:47Z The particle motion of regional arrivals is frequently treated in automatic phase-recognition schemes as that appropriate to simple P or S waves incident on an elastic, laterally homogeneous half-space. This model implies that the motion in ‘ P -type’ phases can be described in terms of a single, generalized signal process and ‘ S -type’ phases in terms of two independent processes ( SV and SH ) and thus, all regional arrivals could be fully characterized by three components of motion. In this paper, we present anlyses of the particle-motion patterns of various regional arrivals recorded at the ARCESS array from closely spaced events in the Kola Peninsula. We have found that only Pn -particle motion, described in terms of two independent signal processes, can be reliably characterized by three-component recordings. On the other hand, the various regional arrivals following Pn , such as Pg and Sn and Lg , can only be poorly characterized on the basis of three-component recordings alone. The reason is that these arrivals must be described in terms of more than two independent generalized signal processes, at least three for Pg and Sn , and possibly up to five for Lg . Recognition of these phases will thus require the use of more sensors than signal processes in the observing sensor configuration, such as three-component sensors combined with a small tripartite array. We have investigated the feasibility of adaptive, automatic recognition of regional arrivials by a wavefield extrapolation scheme utilizing such a mini-array. The process, which appear to be promising, adaptively learns the particle-motion patterns of individual arrivals, including complex site-response functions, from examples of closely located regional events. Text kola peninsula HighWire Press (Stanford University) Kola Peninsula Geophysical Journal International 115 3 1012 1024
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Der, Zoltan A.
Baumgardt, Douglas R.
Shumway, Robert H.
The nature of particle motion in regional seismograms and its utilization for phase identification
topic_facet Articles
description The particle motion of regional arrivals is frequently treated in automatic phase-recognition schemes as that appropriate to simple P or S waves incident on an elastic, laterally homogeneous half-space. This model implies that the motion in ‘ P -type’ phases can be described in terms of a single, generalized signal process and ‘ S -type’ phases in terms of two independent processes ( SV and SH ) and thus, all regional arrivals could be fully characterized by three components of motion. In this paper, we present anlyses of the particle-motion patterns of various regional arrivals recorded at the ARCESS array from closely spaced events in the Kola Peninsula. We have found that only Pn -particle motion, described in terms of two independent signal processes, can be reliably characterized by three-component recordings. On the other hand, the various regional arrivals following Pn , such as Pg and Sn and Lg , can only be poorly characterized on the basis of three-component recordings alone. The reason is that these arrivals must be described in terms of more than two independent generalized signal processes, at least three for Pg and Sn , and possibly up to five for Lg . Recognition of these phases will thus require the use of more sensors than signal processes in the observing sensor configuration, such as three-component sensors combined with a small tripartite array. We have investigated the feasibility of adaptive, automatic recognition of regional arrivials by a wavefield extrapolation scheme utilizing such a mini-array. The process, which appear to be promising, adaptively learns the particle-motion patterns of individual arrivals, including complex site-response functions, from examples of closely located regional events.
format Text
author Der, Zoltan A.
Baumgardt, Douglas R.
Shumway, Robert H.
author_facet Der, Zoltan A.
Baumgardt, Douglas R.
Shumway, Robert H.
author_sort Der, Zoltan A.
title The nature of particle motion in regional seismograms and its utilization for phase identification
title_short The nature of particle motion in regional seismograms and its utilization for phase identification
title_full The nature of particle motion in regional seismograms and its utilization for phase identification
title_fullStr The nature of particle motion in regional seismograms and its utilization for phase identification
title_full_unstemmed The nature of particle motion in regional seismograms and its utilization for phase identification
title_sort nature of particle motion in regional seismograms and its utilization for phase identification
publisher Oxford University Press
publishDate 1993
url http://gji.oxfordjournals.org/cgi/content/short/115/3/1012
https://doi.org/10.1111/j.1365-246X.1993.tb01506.x
geographic Kola Peninsula
geographic_facet Kola Peninsula
genre kola peninsula
genre_facet kola peninsula
op_relation http://gji.oxfordjournals.org/cgi/content/short/115/3/1012
http://dx.doi.org/10.1111/j.1365-246X.1993.tb01506.x
op_rights Copyright (C) 1993, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1993.tb01506.x
container_title Geophysical Journal International
container_volume 115
container_issue 3
container_start_page 1012
op_container_end_page 1024
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