MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA

P(論文) Total intensities of the geomagnetic field were measured in the eastern part of West Ongul Island and the southern part of East Ongul Island during the 30th Japanese Antarctic Research Expedition (JARE-30) in 1989. Measurements were carried out along two east-west observation lines in West Ong...

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Main Authors: ノギ, ヨシフミ, セアマ, ノブカズ, イセザキ, ノブヒロ, フナキ, ミノル, NOGI, Yoshifumi, SEAMA, Nobukazu, ISEZAKI, Nobuhiro, FUNAKI, Minoru
Language:English
Published: National Institute of Polar Research 1991
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/record/2682/files/KJ00002368265.pdf
https://doi.org/10.15094/00002682
https://nipr.repo.nii.ac.jp/records/2682
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author ノギ, ヨシフミ
セアマ, ノブカズ
イセザキ, ノブヒロ
フナキ, ミノル
NOGI, Yoshifumi
SEAMA, Nobukazu
ISEZAKI, Nobuhiro
FUNAKI, Minoru
author_facet ノギ, ヨシフミ
セアマ, ノブカズ
イセザキ, ノブヒロ
フナキ, ミノル
NOGI, Yoshifumi
SEAMA, Nobukazu
ISEZAKI, Nobuhiro
FUNAKI, Minoru
author_sort ノギ, ヨシフミ
collection National Institute of Polar Research Repository, Japan
description P(論文) Total intensities of the geomagnetic field were measured in the eastern part of West Ongul Island and the southern part of East Ongul Island during the 30th Japanese Antarctic Research Expedition (JARE-30) in 1989. Measurements were carried out along two east-west observation lines in West Ongul Island and two east-west and three north-south observation lines in East Ongul Island. The variations of magnetic anomalies in West Ongul Island seem to correlate with the surface geology, while those in East Ongul Island do not. A model calculation showed a positive correlation of the obtained variations in West Ongul Island with the geological structure and the paleomagnetic results. However, widths and positions of the magnetic anomaly source model are slightly different from those of the surface geological structure. These differences provide information how the surface geological structure extends underground. departmental bulletin paper
genre Antarc*
Antarctic
Antarctica
East Antarctica
East Ongul Island
Ongul Island
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
East Ongul Island
Ongul Island
geographic Antarctic
East Antarctica
Ongul
Ongul Island
East Ongul Island
geographic_facet Antarctic
East Antarctica
Ongul
Ongul Island
East Ongul Island
id ftnipr:oai:nipr.repo.nii.ac.jp:00002682
institution Open Polar
language English
long_lat ENVELOPE(39.533,39.533,-69.017,-69.017)
ENVELOPE(39.533,39.533,-69.017,-69.017)
ENVELOPE(39.583,39.583,-69.017,-69.017)
op_collection_id ftnipr
op_doi https://doi.org/10.15094/00002682
op_relation Proceedings of the NIPR Symposium on Antarctic Geosciences
5
11
19
AA1072335X
https://nipr.repo.nii.ac.jp/record/2682/files/KJ00002368265.pdf
https://doi.org/10.15094/00002682
https://nipr.repo.nii.ac.jp/records/2682
publishDate 1991
publisher National Institute of Polar Research
record_format openpolar
spelling ftnipr:oai:nipr.repo.nii.ac.jp:00002682 2025-04-13T14:07:51+00:00 MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA ノギ, ヨシフミ セアマ, ノブカズ イセザキ, ノブヒロ フナキ, ミノル NOGI, Yoshifumi SEAMA, Nobukazu ISEZAKI, Nobuhiro FUNAKI, Minoru 1991-09 application/pdf https://nipr.repo.nii.ac.jp/record/2682/files/KJ00002368265.pdf https://doi.org/10.15094/00002682 https://nipr.repo.nii.ac.jp/records/2682 eng eng National Institute of Polar Research Proceedings of the NIPR Symposium on Antarctic Geosciences 5 11 19 AA1072335X https://nipr.repo.nii.ac.jp/record/2682/files/KJ00002368265.pdf https://doi.org/10.15094/00002682 https://nipr.repo.nii.ac.jp/records/2682 1991 ftnipr https://doi.org/10.15094/00002682 2025-03-19T10:19:57Z P(論文) Total intensities of the geomagnetic field were measured in the eastern part of West Ongul Island and the southern part of East Ongul Island during the 30th Japanese Antarctic Research Expedition (JARE-30) in 1989. Measurements were carried out along two east-west observation lines in West Ongul Island and two east-west and three north-south observation lines in East Ongul Island. The variations of magnetic anomalies in West Ongul Island seem to correlate with the surface geology, while those in East Ongul Island do not. A model calculation showed a positive correlation of the obtained variations in West Ongul Island with the geological structure and the paleomagnetic results. However, widths and positions of the magnetic anomaly source model are slightly different from those of the surface geological structure. These differences provide information how the surface geological structure extends underground. departmental bulletin paper Other/Unknown Material Antarc* Antarctic Antarctica East Antarctica East Ongul Island Ongul Island National Institute of Polar Research Repository, Japan Antarctic East Antarctica Ongul ENVELOPE(39.533,39.533,-69.017,-69.017) Ongul Island ENVELOPE(39.533,39.533,-69.017,-69.017) East Ongul Island ENVELOPE(39.583,39.583,-69.017,-69.017)
spellingShingle ノギ, ヨシフミ
セアマ, ノブカズ
イセザキ, ノブヒロ
フナキ, ミノル
NOGI, Yoshifumi
SEAMA, Nobukazu
ISEZAKI, Nobuhiro
FUNAKI, Minoru
MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title_full MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title_fullStr MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title_full_unstemmed MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title_short MAGNETIC SURVEY IN ONGUL ISLANDS, EAST ANTARCTICA
title_sort magnetic survey in ongul islands, east antarctica
url https://nipr.repo.nii.ac.jp/record/2682/files/KJ00002368265.pdf
https://doi.org/10.15094/00002682
https://nipr.repo.nii.ac.jp/records/2682