Selectivity of the Yellowknife Seismic Array
An idealized signal, consisting of a noise-free, single-frequency infiniteduration input, is theoretically applied to the Yellowknife seismic array. A comparison of the output responses resulting from three possible signal processing techniques, viz. cross-correlation, sumall-squared, and multiple c...
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Oxford University Press
1966
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fthighwire:oai:open-archive.highwire.org:gji:10/4/401 2023-05-15T18:45:38+02:00 Selectivity of the Yellowknife Seismic Array Somers, H. Manchee, E. B. 1966-01-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/10/4/401 https://doi.org/10.1111/j.1365-246X.1966.tb03067.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/10/4/401 http://dx.doi.org/10.1111/j.1365-246X.1966.tb03067.x Copyright (C) 1966, Oxford University Press Articles TEXT 1966 fthighwire https://doi.org/10.1111/j.1365-246X.1966.tb03067.x 2015-02-28T19:24:59Z An idealized signal, consisting of a noise-free, single-frequency infiniteduration input, is theoretically applied to the Yellowknife seismic array. A comparison of the output responses resulting from three possible signal processing techniques, viz. cross-correlation, sumall-squared, and multiple correlation, indicates that cross-correlation is the preferred technique for determining the azimuth and velocity of arrival of the incident seismic energy. Text Yellowknife HighWire Press (Stanford University) Yellowknife Geophysical Journal International 10 4 401 412 |
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HighWire Press (Stanford University) |
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fthighwire |
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English |
topic |
Articles |
spellingShingle |
Articles Somers, H. Manchee, E. B. Selectivity of the Yellowknife Seismic Array |
topic_facet |
Articles |
description |
An idealized signal, consisting of a noise-free, single-frequency infiniteduration input, is theoretically applied to the Yellowknife seismic array. A comparison of the output responses resulting from three possible signal processing techniques, viz. cross-correlation, sumall-squared, and multiple correlation, indicates that cross-correlation is the preferred technique for determining the azimuth and velocity of arrival of the incident seismic energy. |
format |
Text |
author |
Somers, H. Manchee, E. B. |
author_facet |
Somers, H. Manchee, E. B. |
author_sort |
Somers, H. |
title |
Selectivity of the Yellowknife Seismic Array |
title_short |
Selectivity of the Yellowknife Seismic Array |
title_full |
Selectivity of the Yellowknife Seismic Array |
title_fullStr |
Selectivity of the Yellowknife Seismic Array |
title_full_unstemmed |
Selectivity of the Yellowknife Seismic Array |
title_sort |
selectivity of the yellowknife seismic array |
publisher |
Oxford University Press |
publishDate |
1966 |
url |
http://gji.oxfordjournals.org/cgi/content/short/10/4/401 https://doi.org/10.1111/j.1365-246X.1966.tb03067.x |
geographic |
Yellowknife |
geographic_facet |
Yellowknife |
genre |
Yellowknife |
genre_facet |
Yellowknife |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/10/4/401 http://dx.doi.org/10.1111/j.1365-246X.1966.tb03067.x |
op_rights |
Copyright (C) 1966, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1966.tb03067.x |
container_title |
Geophysical Journal International |
container_volume |
10 |
container_issue |
4 |
container_start_page |
401 |
op_container_end_page |
412 |
_version_ |
1766236739957948416 |