PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA
P(論文) Paleomagnetic samples were collected at eight sites from granulites of the Archean Napier Complex and dolerite dikes intruding the complex in the Mt. Riiser-Larsen area in Enderby Land, East Antarctica. Progressive demagnetization results indicate the presence of two magnetic components : the...
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Language: | English |
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National Institute of Polar Research
1997
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Online Access: | https://nipr.repo.nii.ac.jp/record/2845/files/KJ00002368118.pdf https://doi.org/10.15094/00002845 https://nipr.repo.nii.ac.jp/records/2845 |
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author | イシカワ, ナオト フナキ, ミノル ISHIKAWA, Naoto FUNAKI, Minoru |
author_facet | イシカワ, ナオト フナキ, ミノル ISHIKAWA, Naoto FUNAKI, Minoru |
author_sort | イシカワ, ナオト |
collection | National Institute of Polar Research Repository, Japan |
description | P(論文) Paleomagnetic samples were collected at eight sites from granulites of the Archean Napier Complex and dolerite dikes intruding the complex in the Mt. Riiser-Larsen area in Enderby Land, East Antarctica. Progressive demagnetization results indicate the presence of two magnetic components : the low-stability (L) and high-stability (H) components. A principal carrier of the H component is fine-grained magnetite, while the L component may be carried by coarser titanomagnetite. L components with steep negative inclination were remarkably observed in both granulite and dolerite samples. The characteristic L component is considered as a viscous remanence (VRM) in the recent geomagnetic field. A complete overprint of the VRM is observed in samples from one granulite site. The H components of two dolerite sites have positive inclinations, and their virtual geomagnetic pole positions are situated near the segment of the apparent polar wander path between 1.0 and 1.2 Ga for Australia in the East Gondwanaland frame. This may imply that the formation of East Gondwanaland can be dated back to about 1.2 Ga, if the intrusions of the dolerite dikes was related to the Amundsen dike activity in the Napier complex. The H component direction determined at one granulite site is inconsistent with other component directions, implying the possibility that the remanence might have been acquired before the intrusion of the dolerite dikes. departmental bulletin paper |
genre | Antarc* Antarctica East Antarctica Enderby Land Geomagnetic Pole |
genre_facet | Antarc* Antarctica East Antarctica Enderby Land Geomagnetic Pole |
geographic | East Antarctica Riiser-Larsen Napier |
geographic_facet | East Antarctica Riiser-Larsen Napier |
id | ftnipr:oai:nipr.repo.nii.ac.jp:00002845 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(50.667,50.667,-66.783,-66.783) ENVELOPE(-58.440,-58.440,-62.167,-62.167) |
op_collection_id | ftnipr |
op_doi | https://doi.org/10.15094/00002845 |
op_relation | Proceedings of the NIPR Symposium on Antarctic Geosciences 10 79 91 AA1072335X https://nipr.repo.nii.ac.jp/record/2845/files/KJ00002368118.pdf https://doi.org/10.15094/00002845 https://nipr.repo.nii.ac.jp/records/2845 |
publishDate | 1997 |
publisher | National Institute of Polar Research |
record_format | openpolar |
spelling | ftnipr:oai:nipr.repo.nii.ac.jp:00002845 2025-04-13T14:08:54+00:00 PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA イシカワ, ナオト フナキ, ミノル ISHIKAWA, Naoto FUNAKI, Minoru 1997-09 application/pdf https://nipr.repo.nii.ac.jp/record/2845/files/KJ00002368118.pdf https://doi.org/10.15094/00002845 https://nipr.repo.nii.ac.jp/records/2845 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 10 79 91 AA1072335X https://nipr.repo.nii.ac.jp/record/2845/files/KJ00002368118.pdf https://doi.org/10.15094/00002845 https://nipr.repo.nii.ac.jp/records/2845 paleomagnetism the Napier Complex the Amundsen dikes East Gondwanaland 1997 ftnipr https://doi.org/10.15094/00002845 2025-03-19T10:19:57Z P(論文) Paleomagnetic samples were collected at eight sites from granulites of the Archean Napier Complex and dolerite dikes intruding the complex in the Mt. Riiser-Larsen area in Enderby Land, East Antarctica. Progressive demagnetization results indicate the presence of two magnetic components : the low-stability (L) and high-stability (H) components. A principal carrier of the H component is fine-grained magnetite, while the L component may be carried by coarser titanomagnetite. L components with steep negative inclination were remarkably observed in both granulite and dolerite samples. The characteristic L component is considered as a viscous remanence (VRM) in the recent geomagnetic field. A complete overprint of the VRM is observed in samples from one granulite site. The H components of two dolerite sites have positive inclinations, and their virtual geomagnetic pole positions are situated near the segment of the apparent polar wander path between 1.0 and 1.2 Ga for Australia in the East Gondwanaland frame. This may imply that the formation of East Gondwanaland can be dated back to about 1.2 Ga, if the intrusions of the dolerite dikes was related to the Amundsen dike activity in the Napier complex. The H component direction determined at one granulite site is inconsistent with other component directions, implying the possibility that the remanence might have been acquired before the intrusion of the dolerite dikes. departmental bulletin paper Other/Unknown Material Antarc* Antarctica East Antarctica Enderby Land Geomagnetic Pole National Institute of Polar Research Repository, Japan East Antarctica Riiser-Larsen ENVELOPE(50.667,50.667,-66.783,-66.783) Napier ENVELOPE(-58.440,-58.440,-62.167,-62.167) |
spellingShingle | paleomagnetism the Napier Complex the Amundsen dikes East Gondwanaland イシカワ, ナオト フナキ, ミノル ISHIKAWA, Naoto FUNAKI, Minoru PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title | PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title_full | PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title_fullStr | PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title_full_unstemmed | PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title_short | PRELIMINARY REPORT ON PALEOMAGNETIC STUDY OF ROCKS FROM THE MT. RIISER-LARSEN AREA IN ENDERBY LAND, EAST ANTARCTICA |
title_sort | preliminary report on paleomagnetic study of rocks from the mt. riiser-larsen area in enderby land, east antarctica |
topic | paleomagnetism the Napier Complex the Amundsen dikes East Gondwanaland |
topic_facet | paleomagnetism the Napier Complex the Amundsen dikes East Gondwanaland |
url | https://nipr.repo.nii.ac.jp/record/2845/files/KJ00002368118.pdf https://doi.org/10.15094/00002845 https://nipr.repo.nii.ac.jp/records/2845 |