Collection of Yamato Meteorites, Antarctica, in December 1973

1969年12月,9箇の石質隕石がやまと山脈の南東端付近で発見された(Yamato (a)からYamato (I)と命名).引き続き12箇の石質隕石が1973年12月,第14次南極観測隊の旅行隊によってほぼ同地域で発見された.12箇中,大型のもの4箇(重量500~900 g)はYamato (j), (k), (l), (m)と命名され,Yamato (l)はachondrite,他はchondriteである;残りの8箇(4~40 g)はYamato (n)からYamato (u)と命名された.採集現場での産状写真を示すとともに,地形や氷状についても述べた.将来,さらに発見される可能性があり,...

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Main Authors: 白石 和行, 成瀬 廉二, 楠 宏, Kazuyuki SHIRAISHI, Renji NARUSE, Kou KUSUNOKI
Format: Report
Language:English
Published: 研究論文 1976
Subjects:
Online Access:https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7849
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spelling ftnipr:oai:nipr.repo.nii.ac.jp:00007849 2023-07-16T03:53:24+02:00 Collection of Yamato Meteorites, Antarctica, in December 1973 1973ネン 12ガツ ニ オケル ヤマト インセキ ノ サイシュウ 白石 和行 成瀬 廉二 楠 宏 Kazuyuki SHIRAISHI Renji NARUSE Kou KUSUNOKI 1976-03 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7849 http://id.nii.ac.jp/1291/00007849/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=7849&item_no=1&attribute_id=18&file_no=1 en eng 研究論文 Scientific Paper 北海道大学理学部地質学鉱物学教室 北海道大学低温科学研究所 国立極地研究所 Department of Geology and Mineralogy, Faculty of Science, Hokkaido University The Institute of Low Temperature Science, Hokkaido University National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7849 http://id.nii.ac.jp/1291/00007849/ AN00181831 00857289 南極資料, 55, 49-60(1976-03) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=7849&item_no=1&attribute_id=18&file_no=1 552.6 Departmental Bulletin Paper P(論文) 1976 ftnipr 2023-06-24T19:39:14Z 1969年12月,9箇の石質隕石がやまと山脈の南東端付近で発見された(Yamato (a)からYamato (I)と命名).引き続き12箇の石質隕石が1973年12月,第14次南極観測隊の旅行隊によってほぼ同地域で発見された.12箇中,大型のもの4箇(重量500~900 g)はYamato (j), (k), (l), (m)と命名され,Yamato (l)はachondrite,他はchondriteである;残りの8箇(4~40 g)はYamato (n)からYamato (u)と命名された.採集現場での産状写真を示すとともに,地形や氷状についても述べた.将来,さらに発見される可能性があり,やまと山脈南端の限られた裸氷域に隕石が集中している原因や機構の解明のため,将来室内研究と現場での研究の必要なことを述べた. In addition to 9 meteorites, designated as Yamato meteorites, discovered in December 1969 at the SE end of the Yamato Mountains, East Antarctica, 12 stoney meteorites were found in December 1973 in nearly the same area by the traverse glaciology party of the 14th Japanese Antarctic Research Expedition. Eight pieces among 12 were found at the same site as the 1969 collection and the rest were found on the SW side of the Yamato Mountains. Relatively large 4 samples, weighing between 500 and 900 grams, were designated as Yamato (j), (k), (1), and (m), among which Yamato (1) was achondrite and the rest were chondrites; other 8 samples, weighing 4 to 40 grams, were designated as Yamato (n) to (u) in alphabetical order. Geomorphological and glaciological features of the sampling sites are described, suggesting a further extensive search for more meteorites and glaciological research which may account for the concentration of the meteorites. Report Antarc* Antarctic Antarctica East Antarctica National Institute of Polar Research Repository, Japan Antarctic East Antarctica Yamato ENVELOPE(35.583,35.583,-71.417,-71.417)
institution Open Polar
collection National Institute of Polar Research Repository, Japan
op_collection_id ftnipr
language English
topic 552.6
spellingShingle 552.6
白石 和行
成瀬 廉二
楠 宏
Kazuyuki SHIRAISHI
Renji NARUSE
Kou KUSUNOKI
Collection of Yamato Meteorites, Antarctica, in December 1973
topic_facet 552.6
description 1969年12月,9箇の石質隕石がやまと山脈の南東端付近で発見された(Yamato (a)からYamato (I)と命名).引き続き12箇の石質隕石が1973年12月,第14次南極観測隊の旅行隊によってほぼ同地域で発見された.12箇中,大型のもの4箇(重量500~900 g)はYamato (j), (k), (l), (m)と命名され,Yamato (l)はachondrite,他はchondriteである;残りの8箇(4~40 g)はYamato (n)からYamato (u)と命名された.採集現場での産状写真を示すとともに,地形や氷状についても述べた.将来,さらに発見される可能性があり,やまと山脈南端の限られた裸氷域に隕石が集中している原因や機構の解明のため,将来室内研究と現場での研究の必要なことを述べた. In addition to 9 meteorites, designated as Yamato meteorites, discovered in December 1969 at the SE end of the Yamato Mountains, East Antarctica, 12 stoney meteorites were found in December 1973 in nearly the same area by the traverse glaciology party of the 14th Japanese Antarctic Research Expedition. Eight pieces among 12 were found at the same site as the 1969 collection and the rest were found on the SW side of the Yamato Mountains. Relatively large 4 samples, weighing between 500 and 900 grams, were designated as Yamato (j), (k), (1), and (m), among which Yamato (1) was achondrite and the rest were chondrites; other 8 samples, weighing 4 to 40 grams, were designated as Yamato (n) to (u) in alphabetical order. Geomorphological and glaciological features of the sampling sites are described, suggesting a further extensive search for more meteorites and glaciological research which may account for the concentration of the meteorites.
format Report
author 白石 和行
成瀬 廉二
楠 宏
Kazuyuki SHIRAISHI
Renji NARUSE
Kou KUSUNOKI
author_facet 白石 和行
成瀬 廉二
楠 宏
Kazuyuki SHIRAISHI
Renji NARUSE
Kou KUSUNOKI
author_sort 白石 和行
title Collection of Yamato Meteorites, Antarctica, in December 1973
title_short Collection of Yamato Meteorites, Antarctica, in December 1973
title_full Collection of Yamato Meteorites, Antarctica, in December 1973
title_fullStr Collection of Yamato Meteorites, Antarctica, in December 1973
title_full_unstemmed Collection of Yamato Meteorites, Antarctica, in December 1973
title_sort collection of yamato meteorites, antarctica, in december 1973
publisher 研究論文
publishDate 1976
url https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7849
http://id.nii.ac.jp/1291/00007849/
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=7849&item_no=1&attribute_id=18&file_no=1
long_lat ENVELOPE(35.583,35.583,-71.417,-71.417)
geographic Antarctic
East Antarctica
Yamato
geographic_facet Antarctic
East Antarctica
Yamato
genre Antarc*
Antarctic
Antarctica
East Antarctica
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
op_relation https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=7849
http://id.nii.ac.jp/1291/00007849/
AN00181831
00857289
南極資料, 55, 49-60(1976-03)
https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=7849&item_no=1&attribute_id=18&file_no=1
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