Further evidence for a strong intermediate state of the palaeomagnetic field

Both the magnitude and direction of the palaeomagnetic field have been determined during the Lousetown Creek polarity transition. The results, which agree with previous work, show that the geomagnetic field can change in magnitude without changing direction when the virtual geomagnetic pole is close...

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Published in:Geophysical Journal International
Main Author: Shaw, J.
Format: Text
Language:English
Published: Oxford University Press 1977
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/48/2/263
https://doi.org/10.1111/j.1365-246X.1977.tb01299.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:48/2/263 2023-05-15T16:19:38+02:00 Further evidence for a strong intermediate state of the palaeomagnetic field Shaw, J. 1977-02-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/48/2/263 https://doi.org/10.1111/j.1365-246X.1977.tb01299.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/48/2/263 http://dx.doi.org/10.1111/j.1365-246X.1977.tb01299.x Copyright (C) 1977, Oxford University Press Articles TEXT 1977 fthighwire https://doi.org/10.1111/j.1365-246X.1977.tb01299.x 2013-05-27T17:41:59Z Both the magnitude and direction of the palaeomagnetic field have been determined during the Lousetown Creek polarity transition. The results, which agree with previous work, show that the geomagnetic field can change in magnitude without changing direction when the virtual geomagnetic pole is close to the equator. Text Geomagnetic Pole HighWire Press (Stanford University) Geophysical Journal International 48 2 263 269
institution Open Polar
collection HighWire Press (Stanford University)
op_collection_id fthighwire
language English
topic Articles
spellingShingle Articles
Shaw, J.
Further evidence for a strong intermediate state of the palaeomagnetic field
topic_facet Articles
description Both the magnitude and direction of the palaeomagnetic field have been determined during the Lousetown Creek polarity transition. The results, which agree with previous work, show that the geomagnetic field can change in magnitude without changing direction when the virtual geomagnetic pole is close to the equator.
format Text
author Shaw, J.
author_facet Shaw, J.
author_sort Shaw, J.
title Further evidence for a strong intermediate state of the palaeomagnetic field
title_short Further evidence for a strong intermediate state of the palaeomagnetic field
title_full Further evidence for a strong intermediate state of the palaeomagnetic field
title_fullStr Further evidence for a strong intermediate state of the palaeomagnetic field
title_full_unstemmed Further evidence for a strong intermediate state of the palaeomagnetic field
title_sort further evidence for a strong intermediate state of the palaeomagnetic field
publisher Oxford University Press
publishDate 1977
url http://gji.oxfordjournals.org/cgi/content/short/48/2/263
https://doi.org/10.1111/j.1365-246X.1977.tb01299.x
genre Geomagnetic Pole
genre_facet Geomagnetic Pole
op_relation http://gji.oxfordjournals.org/cgi/content/short/48/2/263
http://dx.doi.org/10.1111/j.1365-246X.1977.tb01299.x
op_rights Copyright (C) 1977, Oxford University Press
op_doi https://doi.org/10.1111/j.1365-246X.1977.tb01299.x
container_title Geophysical Journal International
container_volume 48
container_issue 2
container_start_page 263
op_container_end_page 269
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