A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks
The n.r.m. of samples of dolerite from the Great Whin Sill, and of basalts from Iceland and Argentina, have been examined during cooling and warming between the ambient and liquid nitrogen temperatures. At about −150°C magnetite undergoes a phase transition of the second kind. The thermo-remanent ma...
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Oxford University Press
1967
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fthighwire:oai:open-archive.highwire.org:gji:12/3/301 2023-05-15T16:48:07+02:00 A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks Creer, K. M. Like, C. B. 1967-03-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/12/3/301 https://doi.org/10.1111/j.1365-246X.1967.tb03122.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/12/3/301 http://dx.doi.org/10.1111/j.1365-246X.1967.tb03122.x Copyright (C) 1967, Oxford University Press Articles TEXT 1967 fthighwire https://doi.org/10.1111/j.1365-246X.1967.tb03122.x 2015-02-28T19:07:14Z The n.r.m. of samples of dolerite from the Great Whin Sill, and of basalts from Iceland and Argentina, have been examined during cooling and warming between the ambient and liquid nitrogen temperatures. At about −150°C magnetite undergoes a phase transition of the second kind. The thermo-remanent magnetization acquired when samples of these rocks, which contain magnetite, are cooled and reheated through this temperature has been studied. The name ‘transition thermoremanent magnetization’ (t.t.r.m.) is preferred for this kind of magnetization, rather than ‘inverse’ t.r.m. used by Japanese workers. Text Iceland HighWire Press (Stanford University) Argentina Geophysical Journal International 12 3 301 312 |
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HighWire Press (Stanford University) |
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English |
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Articles |
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Articles Creer, K. M. Like, C. B. A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
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Articles |
description |
The n.r.m. of samples of dolerite from the Great Whin Sill, and of basalts from Iceland and Argentina, have been examined during cooling and warming between the ambient and liquid nitrogen temperatures. At about −150°C magnetite undergoes a phase transition of the second kind. The thermo-remanent magnetization acquired when samples of these rocks, which contain magnetite, are cooled and reheated through this temperature has been studied. The name ‘transition thermoremanent magnetization’ (t.t.r.m.) is preferred for this kind of magnetization, rather than ‘inverse’ t.r.m. used by Japanese workers. |
format |
Text |
author |
Creer, K. M. Like, C. B. |
author_facet |
Creer, K. M. Like, C. B. |
author_sort |
Creer, K. M. |
title |
A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
title_short |
A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
title_full |
A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
title_fullStr |
A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
title_full_unstemmed |
A Low Temperature Investigation of the Natural Remanent Magnetization of Several Igneous Rocks |
title_sort |
low temperature investigation of the natural remanent magnetization of several igneous rocks |
publisher |
Oxford University Press |
publishDate |
1967 |
url |
http://gji.oxfordjournals.org/cgi/content/short/12/3/301 https://doi.org/10.1111/j.1365-246X.1967.tb03122.x |
geographic |
Argentina |
geographic_facet |
Argentina |
genre |
Iceland |
genre_facet |
Iceland |
op_relation |
http://gji.oxfordjournals.org/cgi/content/short/12/3/301 http://dx.doi.org/10.1111/j.1365-246X.1967.tb03122.x |
op_rights |
Copyright (C) 1967, Oxford University Press |
op_doi |
https://doi.org/10.1111/j.1365-246X.1967.tb03122.x |
container_title |
Geophysical Journal International |
container_volume |
12 |
container_issue |
3 |
container_start_page |
301 |
op_container_end_page |
312 |
_version_ |
1766038230090645504 |