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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Main Authors: イシカワ, ナオト, フナキ, ミノル, ISHIKAWA, Naoto, FUNAKI, Minoru
Language:English
Published: National Institute of Polar Research 1997
Subjects:
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
_version_ 1829298762544054272
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