Teleseismic P-wave Delay Time in Iceland

An evaluation is made of relative teleseismic P -wave delays between stations in Iceland and EKA (Scotland), KIR (Sweden) and KTG (Greenland). A detailed analysis of possible sources of error including the use of array data to detect the onset of events, shows there is a delay of at least 1 s associ...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Long, R. E., Mitchell, M. G.
Format: Text
Language:English
Published: Oxford University Press 1970
Subjects:
Articles
Greenland
Iceland
Online Access:http://gji.oxfordjournals.org/cgi/content/short/20/1/41
https://doi.org/10.1111/j.1365-246X.1970.tb06747.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:20/1/41 2023-05-15T16:27:50+02:00 Teleseismic P-wave Delay Time in Iceland Long, R. E. Mitchell, M. G. 1970-06-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/20/1/41 https://doi.org/10.1111/j.1365-246X.1970.tb06747.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/20/1/41 http://dx.doi.org/10.1111/j.1365-246X.1970.tb06747.x Copyright (C) 1970, Oxford University Press Articles TEXT 1970 fthighwire https://doi.org/10.1111/j.1365-246X.1970.tb06747.x 2012-11-23T22:15:04Z An evaluation is made of relative teleseismic P -wave delays between stations in Iceland and EKA (Scotland), KIR (Sweden) and KTG (Greenland). A detailed analysis of possible sources of error including the use of array data to detect the onset of events, shows there is a delay of at least 1 s associated with the upper mantle beneath Iceland. The delay does not appear to vary with distance or azimuth, and shows little variations over Iceland itself. Text Greenland Iceland HighWire Press (Stanford University) Greenland Geophysical Journal International 20 1 41 48
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Long, R. E.
Mitchell, M. G.
Teleseismic P-wave Delay Time in Iceland
topic_facet Articles
description An evaluation is made of relative teleseismic P -wave delays between stations in Iceland and EKA (Scotland), KIR (Sweden) and KTG (Greenland). A detailed analysis of possible sources of error including the use of array data to detect the onset of events, shows there is a delay of at least 1 s associated with the upper mantle beneath Iceland. The delay does not appear to vary with distance or azimuth, and shows little variations over Iceland itself.
format Text
author Long, R. E.
Mitchell, M. G.
author_facet Long, R. E.
Mitchell, M. G.
author_sort Long, R. E.
title Teleseismic P-wave Delay Time in Iceland
title_short Teleseismic P-wave Delay Time in Iceland
title_full Teleseismic P-wave Delay Time in Iceland
title_fullStr Teleseismic P-wave Delay Time in Iceland
title_full_unstemmed Teleseismic P-wave Delay Time in Iceland
title_sort teleseismic p-wave delay time in iceland
publisher Oxford University Press
publishDate 1970
url http://gji.oxfordjournals.org/cgi/content/short/20/1/41
https://doi.org/10.1111/j.1365-246X.1970.tb06747.x
geographic Greenland
geographic_facet Greenland
genre Greenland
Iceland
genre_facet Greenland
Iceland
op_relation http://gji.oxfordjournals.org/cgi/content/short/20/1/41
http://dx.doi.org/10.1111/j.1365-246X.1970.tb06747.x
op_rights Copyright (C) 1970, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1970.tb06747.x
container_title Geophysical Journal International
container_volume 20
container_issue 1
container_start_page 41
op_container_end_page 48
_version_ 1766017384485748736

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