Rayleigh Wave Group Velocity Dispersion in North Atlantic Region
Data from five earthquakes in the Azores Islands recorded in nine stations on the European and American coasts have been used to determine Rayleigh wave group velocity dispersion curves. Analysis of these observations leads to certain conclusions about the nature of the crustal and upper mantle stru...
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Oxford University Press
1974
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fthighwire:oai:open-archive.highwire.org:gji:37/2/297 2023-05-15T17:27:57+02:00 Rayleigh Wave Group Velocity Dispersion in North Atlantic Region Bravo, Cristina Udías, Agustin 1974-05-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/37/2/297 https://doi.org/10.1111/j.1365-246X.1974.tb01240.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/37/2/297 http://dx.doi.org/10.1111/j.1365-246X.1974.tb01240.x Copyright (C) 1974, Oxford University Press Articles TEXT 1974 fthighwire https://doi.org/10.1111/j.1365-246X.1974.tb01240.x 2013-05-28T06:06:24Z Data from five earthquakes in the Azores Islands recorded in nine stations on the European and American coasts have been used to determine Rayleigh wave group velocity dispersion curves. Analysis of these observations leads to certain conclusions about the nature of the crustal and upper mantle structure in the North Atlantic Ocean. The main results are the presence of lower velocities in the upper mantle for the Atlantic than for the Pacific and the absence of appreciable influence of the Mid-Atlantic Ridge on the dispersion of surface waves. Text North Atlantic HighWire Press (Stanford University) Mid-Atlantic Ridge Pacific Geophysical Journal International 37 2 297 304 |
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Open Polar |
collection |
HighWire Press (Stanford University) |
op_collection_id |
fthighwire |
language |
English |
topic |
Articles |
spellingShingle |
Articles Bravo, Cristina Udías, Agustin Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
topic_facet |
Articles |
description |
Data from five earthquakes in the Azores Islands recorded in nine stations on the European and American coasts have been used to determine Rayleigh wave group velocity dispersion curves. Analysis of these observations leads to certain conclusions about the nature of the crustal and upper mantle structure in the North Atlantic Ocean. The main results are the presence of lower velocities in the upper mantle for the Atlantic than for the Pacific and the absence of appreciable influence of the Mid-Atlantic Ridge on the dispersion of surface waves. |
format |
Text |
author |
Bravo, Cristina Udías, Agustin |
author_facet |
Bravo, Cristina Udías, Agustin |
author_sort |
Bravo, Cristina |
title |
Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
title_short |
Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
title_full |
Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
title_fullStr |
Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
title_full_unstemmed |
Rayleigh Wave Group Velocity Dispersion in North Atlantic Region |
title_sort |
rayleigh wave group velocity dispersion in north atlantic region |
publisher |
Oxford University Press |
publishDate |
1974 |
url |
http://gji.oxfordjournals.org/cgi/content/short/37/2/297 https://doi.org/10.1111/j.1365-246X.1974.tb01240.x |
geographic |
Mid-Atlantic Ridge Pacific |
geographic_facet |
Mid-Atlantic Ridge Pacific |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/37/2/297 http://dx.doi.org/10.1111/j.1365-246X.1974.tb01240.x |
op_rights |
Copyright (C) 1974, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1974.tb01240.x |
container_title |
Geophysical Journal International |
container_volume |
37 |
container_issue |
2 |
container_start_page |
297 |
op_container_end_page |
304 |
_version_ |
1766120349575938048 |