STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)

The study of the extraterrestrial material collected in Antarctica is reported. The extrateirestnal material comprises cosmic dust, tektite, and meteorite. Antarctica is the most suitable place for collecting such material, since the Antarctic Continent is covered with thick ice and is hardly contam...

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Bibliographic Details
Main Authors: Makoto SHIMA, Hideo YABUKI
Format: Article in Journal/Newspaper
Language:English
Published: National Institute of Polar Research 1968
Subjects:
geo
Online Access:https://doi.org/10.15094/00007532
https://doaj.org/article/a26f706d4a244ab3933789cefd48f02e
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:a26f706d4a244ab3933789cefd48f02e 2023-05-15T13:55:01+02:00 STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I) Makoto SHIMA Hideo YABUKI 1968-12-01 https://doi.org/10.15094/00007532 https://doaj.org/article/a26f706d4a244ab3933789cefd48f02e en other eng National Institute of Polar Research doi:10.15094/00007532 0085-7289 2432-079X https://doaj.org/article/a26f706d4a244ab3933789cefd48f02e undefined Antarctic Record, Iss 33, Pp 53-64 (1968) geo Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 1968 fttriple https://doi.org/10.15094/00007532 2023-01-22T17:53:18Z The study of the extraterrestrial material collected in Antarctica is reported. The extrateirestnal material comprises cosmic dust, tektite, and meteorite. Antarctica is the most suitable place for collecting such material, since the Antarctic Continent is covered with thick ice and is hardly contaminated by terrestrial material, so that the extrater-restrial material is easily picked up. This report describes the chemical composition and the size distribution of cosmic dust. By the chemical composition, cosmic dust is classified into three groups, 1) Ni-Fe group, 2) Fe group and 3) silicate group. The glassy material composed mainly of silica is thought to be a kind of tektite. Annual fall rate of cosmic dust near Syowa Station would be estimated at 3 × 10^4 ton/year. Article in Journal/Newspaper Antarc* Antarctic Antarctica Unknown Antarctic Syowa Station The Antarctic
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
spellingShingle geo
Makoto SHIMA
Hideo YABUKI
STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
topic_facet geo
description The study of the extraterrestrial material collected in Antarctica is reported. The extrateirestnal material comprises cosmic dust, tektite, and meteorite. Antarctica is the most suitable place for collecting such material, since the Antarctic Continent is covered with thick ice and is hardly contaminated by terrestrial material, so that the extrater-restrial material is easily picked up. This report describes the chemical composition and the size distribution of cosmic dust. By the chemical composition, cosmic dust is classified into three groups, 1) Ni-Fe group, 2) Fe group and 3) silicate group. The glassy material composed mainly of silica is thought to be a kind of tektite. Annual fall rate of cosmic dust near Syowa Station would be estimated at 3 × 10^4 ton/year.
format Article in Journal/Newspaper
author Makoto SHIMA
Hideo YABUKI
author_facet Makoto SHIMA
Hideo YABUKI
author_sort Makoto SHIMA
title STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
title_short STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
title_full STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
title_fullStr STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
title_full_unstemmed STUDY ON THE EXTRATERRESTRIAL MATERIAL AT ANTARCTICA (I)
title_sort study on the extraterrestrial material at antarctica (i)
publisher National Institute of Polar Research
publishDate 1968
url https://doi.org/10.15094/00007532
https://doaj.org/article/a26f706d4a244ab3933789cefd48f02e
geographic Antarctic
Syowa Station
The Antarctic
geographic_facet Antarctic
Syowa Station
The Antarctic
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_source Antarctic Record, Iss 33, Pp 53-64 (1968)
op_relation doi:10.15094/00007532
0085-7289
2432-079X
https://doaj.org/article/a26f706d4a244ab3933789cefd48f02e
op_rights undefined
op_doi https://doi.org/10.15094/00007532
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