PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA
Thellier's method was applied to the metamorphic and volcanic rocks of the Napier Complex in Enderby Land, Ongul Islands, Mawson Station, Sor Rondane Mountains and McMurdo Sound. The samples treated have partly ambiguous ages and sometimes show undesirable thermomagnetic properties which cause...
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Natural Science Laboratory, Toyo University
1991
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ftnipr:oai:nipr.repo.nii.ac.jp:00002689 2023-05-15T13:48:59+02:00 PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA ウエノ ナオコ フナキ ミノル Naoko UENO Minoru FUNAKI 1991-09 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2689 http://id.nii.ac.jp/1291/00002689/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2689&item_no=1&attribute_id=18&file_no=1 en eng Natural Science Laboratory, Toyo University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2689 http://id.nii.ac.jp/1291/00002689/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 5, 75-83(1991-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2689&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1991 ftnipr 2022-11-19T19:41:26Z Thellier's method was applied to the metamorphic and volcanic rocks of the Napier Complex in Enderby Land, Ongul Islands, Mawson Station, Sor Rondane Mountains and McMurdo Sound. The samples treated have partly ambiguous ages and sometimes show undesirable thermomagnetic properties which cause only a small linear portion in NRM-TRM diagrams and inconsistent paleointensity values for different specimens of the same sample. However, results from Enderby Land, Sor Rondane and McMurdo Sound indicate that geomagnetic field strength was 20% higher in the period of 2.5 Ga to 500Ma, 20% lower 500Ma ago and 30% higher 1 Ma ago than today, respectively. Report Antarc* Antarctica Enderby Land McMurdo Sound National Institute of Polar Research Repository, Japan McMurdo Sound Ongul ENVELOPE(39.533,39.533,-69.017,-69.017) Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) Mawson Station ENVELOPE(62.874,62.874,-67.603,-67.603) Sor-Rondane ENVELOPE(25.000,25.000,-72.000,-72.000) Sor Rondane Mountains ENVELOPE(25.000,25.000,-72.000,-72.000) |
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Open Polar |
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National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Thellier's method was applied to the metamorphic and volcanic rocks of the Napier Complex in Enderby Land, Ongul Islands, Mawson Station, Sor Rondane Mountains and McMurdo Sound. The samples treated have partly ambiguous ages and sometimes show undesirable thermomagnetic properties which cause only a small linear portion in NRM-TRM diagrams and inconsistent paleointensity values for different specimens of the same sample. However, results from Enderby Land, Sor Rondane and McMurdo Sound indicate that geomagnetic field strength was 20% higher in the period of 2.5 Ga to 500Ma, 20% lower 500Ma ago and 30% higher 1 Ma ago than today, respectively. |
format |
Report |
author |
ウエノ ナオコ フナキ ミノル Naoko UENO Minoru FUNAKI |
spellingShingle |
ウエノ ナオコ フナキ ミノル Naoko UENO Minoru FUNAKI PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
author_facet |
ウエノ ナオコ フナキ ミノル Naoko UENO Minoru FUNAKI |
author_sort |
ウエノ ナオコ |
title |
PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
title_short |
PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
title_full |
PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
title_fullStr |
PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
title_full_unstemmed |
PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA |
title_sort |
preliminary note on paleointensities of the geomagnetic field obtained from rocks in antarctica |
publisher |
Natural Science Laboratory, Toyo University |
publishDate |
1991 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2689 http://id.nii.ac.jp/1291/00002689/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2689&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(39.533,39.533,-69.017,-69.017) ENVELOPE(-58.440,-58.440,-62.167,-62.167) ENVELOPE(62.874,62.874,-67.603,-67.603) ENVELOPE(25.000,25.000,-72.000,-72.000) ENVELOPE(25.000,25.000,-72.000,-72.000) |
geographic |
McMurdo Sound Ongul Napier Mawson Station Sor-Rondane Sor Rondane Mountains |
geographic_facet |
McMurdo Sound Ongul Napier Mawson Station Sor-Rondane Sor Rondane Mountains |
genre |
Antarc* Antarctica Enderby Land McMurdo Sound |
genre_facet |
Antarc* Antarctica Enderby Land McMurdo Sound |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=2689 http://id.nii.ac.jp/1291/00002689/ AA1072335X Proceedings of the NIPR Symposium on Antarctic Geosciences, 5, 75-83(1991-09) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=2689&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250296600690688 |