A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex
Secondary magnetization produced during a thermal experiment in Thelliers' method was studied on 12 samples from the Mt. Riiser-Larsen area for that paleomagnetic data already been reported (N. ISHIKAWA and M. FUNAKI: Proc. NIPR Symp. Antarct. Geosci., 10, 79, 1997), and considered suitable for...
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Natural Science Laboratory, Toyo University
1998
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ftnipr:oai:nipr.repo.nii.ac.jp:00003023 2023-05-15T13:49:00+02:00 A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex Naoko Ueno Tomoko Ogishima Naoto Ishikawa Minoru Funaki 1998-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3023 http://id.nii.ac.jp/1291/00003023/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3023&item_no=1&attribute_id=18&file_no=1 en eng Natural Science Laboratory, Toyo University Mejiro Gakuen High School School of Earth Sciences, IHS, Kyoto University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3023 http://id.nii.ac.jp/1291/00003023/ AA1130866X Polar geoscience, 11, 125-131(1998-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3023&item_no=1&attribute_id=18&file_no=1 paleointensity Thelliers method secondary magnetization the Napier Complex Departmental Bulletin Paper P(論文) 1998 ftnipr 2022-11-26T19:42:23Z Secondary magnetization produced during a thermal experiment in Thelliers' method was studied on 12 samples from the Mt. Riiser-Larsen area for that paleomagnetic data already been reported (N. ISHIKAWA and M. FUNAKI: Proc. NIPR Symp. Antarct. Geosci., 10, 79, 1997), and considered suitable for paleomagnetic study from the rock magnetic characteristics of samples. A remeasurement test of NRM on the same temperature step (NRM-check) as well as PTRM (PTRM-check) in air and in vacuum revealed secondary magnetization concerned with NRM and TRM which appeared at the same temperature, around 350℃, that would be explained by the oxidation of sulfide observed under a microscope. Secondary magnetization around 550℃ which appeared in air might also be caused by magneto-mineralogical change. These results are supported by the large variation of initial susceptibility around 300℃ and 550℃. Both the secondary magnetization of NRM and that of PTRM produced in vacuum were comparable to in air. Report Antarc* Polar geoscience National Institute of Polar Research Repository, Japan Riiser-Larsen ENVELOPE(50.667,50.667,-66.783,-66.783) Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
topic |
paleointensity Thelliers method secondary magnetization the Napier Complex |
spellingShingle |
paleointensity Thelliers method secondary magnetization the Napier Complex Naoko Ueno Tomoko Ogishima Naoto Ishikawa Minoru Funaki A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
topic_facet |
paleointensity Thelliers method secondary magnetization the Napier Complex |
description |
Secondary magnetization produced during a thermal experiment in Thelliers' method was studied on 12 samples from the Mt. Riiser-Larsen area for that paleomagnetic data already been reported (N. ISHIKAWA and M. FUNAKI: Proc. NIPR Symp. Antarct. Geosci., 10, 79, 1997), and considered suitable for paleomagnetic study from the rock magnetic characteristics of samples. A remeasurement test of NRM on the same temperature step (NRM-check) as well as PTRM (PTRM-check) in air and in vacuum revealed secondary magnetization concerned with NRM and TRM which appeared at the same temperature, around 350℃, that would be explained by the oxidation of sulfide observed under a microscope. Secondary magnetization around 550℃ which appeared in air might also be caused by magneto-mineralogical change. These results are supported by the large variation of initial susceptibility around 300℃ and 550℃. Both the secondary magnetization of NRM and that of PTRM produced in vacuum were comparable to in air. |
format |
Report |
author |
Naoko Ueno Tomoko Ogishima Naoto Ishikawa Minoru Funaki |
author_facet |
Naoko Ueno Tomoko Ogishima Naoto Ishikawa Minoru Funaki |
author_sort |
Naoko Ueno |
title |
A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
title_short |
A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
title_full |
A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
title_fullStr |
A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
title_full_unstemmed |
A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex |
title_sort |
preliminary study of secondary magnetization during successive heating of rocks from the napier complex |
publisher |
Natural Science Laboratory, Toyo University |
publishDate |
1998 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3023 http://id.nii.ac.jp/1291/00003023/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3023&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(50.667,50.667,-66.783,-66.783) ENVELOPE(-58.440,-58.440,-62.167,-62.167) |
geographic |
Riiser-Larsen Napier |
geographic_facet |
Riiser-Larsen Napier |
genre |
Antarc* Polar geoscience |
genre_facet |
Antarc* Polar geoscience |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=3023 http://id.nii.ac.jp/1291/00003023/ AA1130866X Polar geoscience, 11, 125-131(1998-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=3023&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250336105791488 |