Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland

Apparent velocity measurements of P arrivals from Mid-Atlantic Ridge earthquakes across pairs of stations in Iceland and Greenland have been made using bulletin data. They define both the vertical and horizontal extent of the low velocity anomalous mantle zone between 50° and 70° N.

Bibliographic Details
Published in:Geophysical Journal International
Main Author: Francis, T. J. G.
Format: Text
Language:English
Published: Oxford University Press 1969
Subjects:
Articles
Greenland
Mid-Atlantic Ridge
Iceland
Online Access:http://gji.oxfordjournals.org/cgi/content/short/17/5/507
https://doi.org/10.1111/j.1365-246X.1969.tb00254.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:17/5/507 2023-05-15T16:27:07+02:00 Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland Francis, T. J. G. 1969-07-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/17/5/507 https://doi.org/10.1111/j.1365-246X.1969.tb00254.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/17/5/507 http://dx.doi.org/10.1111/j.1365-246X.1969.tb00254.x Copyright (C) 1969, Oxford University Press Articles TEXT 1969 fthighwire https://doi.org/10.1111/j.1365-246X.1969.tb00254.x 2015-02-28T18:38:00Z Apparent velocity measurements of P arrivals from Mid-Atlantic Ridge earthquakes across pairs of stations in Iceland and Greenland have been made using bulletin data. They define both the vertical and horizontal extent of the low velocity anomalous mantle zone between 50° and 70° N. Text Greenland Iceland HighWire Press (Stanford University) Greenland Mid-Atlantic Ridge Geophysical Journal International 17 5 507 520
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Francis, T. J. G.
Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
topic_facet Articles
description Apparent velocity measurements of P arrivals from Mid-Atlantic Ridge earthquakes across pairs of stations in Iceland and Greenland have been made using bulletin data. They define both the vertical and horizontal extent of the low velocity anomalous mantle zone between 50° and 70° N.
format Text
author Francis, T. J. G.
author_facet Francis, T. J. G.
author_sort Francis, T. J. G.
title Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
title_short Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
title_full Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
title_fullStr Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
title_full_unstemmed Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland
title_sort upper mantle structure along the axis of the mid-atlantic ridge near iceland
publisher Oxford University Press
publishDate 1969
url http://gji.oxfordjournals.org/cgi/content/short/17/5/507
https://doi.org/10.1111/j.1365-246X.1969.tb00254.x
geographic Greenland
Mid-Atlantic Ridge
geographic_facet Greenland
Mid-Atlantic Ridge
genre Greenland
Iceland
genre_facet Greenland
Iceland
op_relation http://gji.oxfordjournals.org/cgi/content/short/17/5/507
http://dx.doi.org/10.1111/j.1365-246X.1969.tb00254.x
op_rights Copyright (C) 1969, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1969.tb00254.x
container_title Geophysical Journal International
container_volume 17
container_issue 5
container_start_page 507
op_container_end_page 520
_version_ 1766016179506249728

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