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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1977
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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 |
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HighWire Press (Stanford University) |
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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 |
_version_ |
1766006044730851328 |