A Study of the Palaeomagnetism of the Pilansberg Dykes
A detailed study has been made of the remanent magnetization of five Pilansberg dykes, by means of measurements on oriented specimens of the rocks. Outcrops of the dykes prove to have suffered magnetic disturbance of their original thermo-remanent magnetization. Specimens from depths of a few thousa...
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Oxford University Press
1956
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fthighwire:oai:open-archive.highwire.org:gjiarc:7/4/196 2023-05-15T17:39:16+02:00 A Study of the Palaeomagnetism of the Pilansberg Dykes Gough, D. I. 1956-08-01 00:00:00.0 text/html http://gsmnras.oxfordjournals.org/cgi/content/short/7/4/196 https://doi.org/10.1111/j.1365-246X.1956.tb05564.x en eng Oxford University Press http://gsmnras.oxfordjournals.org/cgi/content/short/7/4/196 http://dx.doi.org/10.1111/j.1365-246X.1956.tb05564.x Copyright (C) 1956, Oxford University Press Articles TEXT 1956 fthighwire https://doi.org/10.1111/j.1365-246X.1956.tb05564.x 2016-11-16T17:00:22Z A detailed study has been made of the remanent magnetization of five Pilansberg dykes, by means of measurements on oriented specimens of the rocks. Outcrops of the dykes prove to have suffered magnetic disturbance of their original thermo-remanent magnetization. Specimens from depths of a few thousand feet, taken in Witwatersrand gold mines, show highly consistent magnetisation of the basic parts of the dykes over considerable distances between sampling sites. The mean directions given by the five dykes agree well, and the mean direction from the five dykes gives a North-seeking magnetic pole with inclination +69°.3 and azimuth N 24° 0 E. Assuming thermo-remanent magnetisation by a geocentric dipole field, this places a North magnetic pole in latitude 7½° N, longitude 42½° E at the time of intrusion of the dykes. The age of the dykes is uncertain, but is probably about 300 to 400 million years. Some of the specimens have been subjected to alternating magnetic fields in order to test the stability of their magnetisations. The basic specimens are found to be highly stable, being only slightly affected by fields of 100 to 300 oersteds. The possible implications of the results are discussed, in terms of hypotheses of polar wandering and continental drift. Text North Magnetic Pole HighWire Press (Stanford University) Geophysical Journal International 7 196 213 |
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English |
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Articles Gough, D. I. A Study of the Palaeomagnetism of the Pilansberg Dykes |
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description |
A detailed study has been made of the remanent magnetization of five Pilansberg dykes, by means of measurements on oriented specimens of the rocks. Outcrops of the dykes prove to have suffered magnetic disturbance of their original thermo-remanent magnetization. Specimens from depths of a few thousand feet, taken in Witwatersrand gold mines, show highly consistent magnetisation of the basic parts of the dykes over considerable distances between sampling sites. The mean directions given by the five dykes agree well, and the mean direction from the five dykes gives a North-seeking magnetic pole with inclination +69°.3 and azimuth N 24° 0 E. Assuming thermo-remanent magnetisation by a geocentric dipole field, this places a North magnetic pole in latitude 7½° N, longitude 42½° E at the time of intrusion of the dykes. The age of the dykes is uncertain, but is probably about 300 to 400 million years. Some of the specimens have been subjected to alternating magnetic fields in order to test the stability of their magnetisations. The basic specimens are found to be highly stable, being only slightly affected by fields of 100 to 300 oersteds. The possible implications of the results are discussed, in terms of hypotheses of polar wandering and continental drift. |
format |
Text |
author |
Gough, D. I. |
author_facet |
Gough, D. I. |
author_sort |
Gough, D. I. |
title |
A Study of the Palaeomagnetism of the Pilansberg Dykes |
title_short |
A Study of the Palaeomagnetism of the Pilansberg Dykes |
title_full |
A Study of the Palaeomagnetism of the Pilansberg Dykes |
title_fullStr |
A Study of the Palaeomagnetism of the Pilansberg Dykes |
title_full_unstemmed |
A Study of the Palaeomagnetism of the Pilansberg Dykes |
title_sort |
study of the palaeomagnetism of the pilansberg dykes |
publisher |
Oxford University Press |
publishDate |
1956 |
url |
http://gsmnras.oxfordjournals.org/cgi/content/short/7/4/196 https://doi.org/10.1111/j.1365-246X.1956.tb05564.x |
genre |
North Magnetic Pole |
genre_facet |
North Magnetic Pole |
op_relation |
http://gsmnras.oxfordjournals.org/cgi/content/short/7/4/196 http://dx.doi.org/10.1111/j.1365-246X.1956.tb05564.x |
op_rights |
Copyright (C) 1956, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1956.tb05564.x |
container_title |
Geophysical Journal International |
container_volume |
7 |
container_start_page |
196 |
op_container_end_page |
213 |
_version_ |
1766140034439708672 |