Microanalyses of antarctica micrometeorites
About 260 tonnes of ultraclean blue ice were recently melted and filtered on the Antarctic ice sheet (in January 1991, at Cap-Prudhomme, near the french station of Dumont d'Urville) as to collect all grains with sizes > 25 μm. In the best size fraction (50-100μm) about 10% of the grains are...
Published in: | Proceedings, annual meeting, Electron Microscopy Society of America |
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Cambridge University Press (CUP)
1992
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Online Access: | http://dx.doi.org/10.1017/s0424820100133217 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0424820100133217 |
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crcambridgeupr:10.1017/s0424820100133217 2024-03-03T08:38:46+00:00 Microanalyses of antarctica micrometeorites Maurette, M. Perreau, M. 1992 http://dx.doi.org/10.1017/s0424820100133217 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0424820100133217 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Proceedings, annual meeting, Electron Microscopy Society of America volume 50, issue 2, page 1716-1717 ISSN 0424-8201 2690-1315 General Medicine journal-article 1992 crcambridgeupr https://doi.org/10.1017/s0424820100133217 2024-02-08T08:41:50Z About 260 tonnes of ultraclean blue ice were recently melted and filtered on the Antarctic ice sheet (in January 1991, at Cap-Prudhomme, near the french station of Dumont d'Urville) as to collect all grains with sizes > 25 μm. In the best size fraction (50-100μm) about 10% of the grains are unmelted antarctic micrometeorites (AMMs) with a chondritic composition. About 50% of these grains are complex aggregates of submicron-sized grains. Their characterization, which is very difficult, requires a panoply of analytical techniques allowing their analyses at all scales of magnification between 10 6 μm 3 and 10 -4 μm 3 . We review below analyses performed by various groups, and discuss briefly some of their preliminary implications to various fields of Science. The "large" size of the AMMs allows their multidisciplinary investigations. With a binocular we start selecting an aliquot of ≈50 dark grains showing irregular shapes, and which usually contains about 70% AMMs. Each grain is broken into about 4 fragments and their multidisciplinary analysis proceeds as follow: (1) Polished sections . The largest of these fragments are mounted in an epoxy disc and polished. Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Sheet Cambridge University Press Antarctic The Antarctic Dumont d'Urville ENVELOPE(140.017,140.017,-66.667,-66.667) Dumont-d'Urville ENVELOPE(140.013,140.013,-66.667,-66.667) Proceedings, annual meeting, Electron Microscopy Society of America 50 2 1716 1717 |
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Cambridge University Press |
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crcambridgeupr |
language |
English |
topic |
General Medicine |
spellingShingle |
General Medicine Maurette, M. Perreau, M. Microanalyses of antarctica micrometeorites |
topic_facet |
General Medicine |
description |
About 260 tonnes of ultraclean blue ice were recently melted and filtered on the Antarctic ice sheet (in January 1991, at Cap-Prudhomme, near the french station of Dumont d'Urville) as to collect all grains with sizes > 25 μm. In the best size fraction (50-100μm) about 10% of the grains are unmelted antarctic micrometeorites (AMMs) with a chondritic composition. About 50% of these grains are complex aggregates of submicron-sized grains. Their characterization, which is very difficult, requires a panoply of analytical techniques allowing their analyses at all scales of magnification between 10 6 μm 3 and 10 -4 μm 3 . We review below analyses performed by various groups, and discuss briefly some of their preliminary implications to various fields of Science. The "large" size of the AMMs allows their multidisciplinary investigations. With a binocular we start selecting an aliquot of ≈50 dark grains showing irregular shapes, and which usually contains about 70% AMMs. Each grain is broken into about 4 fragments and their multidisciplinary analysis proceeds as follow: (1) Polished sections . The largest of these fragments are mounted in an epoxy disc and polished. |
format |
Article in Journal/Newspaper |
author |
Maurette, M. Perreau, M. |
author_facet |
Maurette, M. Perreau, M. |
author_sort |
Maurette, M. |
title |
Microanalyses of antarctica micrometeorites |
title_short |
Microanalyses of antarctica micrometeorites |
title_full |
Microanalyses of antarctica micrometeorites |
title_fullStr |
Microanalyses of antarctica micrometeorites |
title_full_unstemmed |
Microanalyses of antarctica micrometeorites |
title_sort |
microanalyses of antarctica micrometeorites |
publisher |
Cambridge University Press (CUP) |
publishDate |
1992 |
url |
http://dx.doi.org/10.1017/s0424820100133217 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0424820100133217 |
long_lat |
ENVELOPE(140.017,140.017,-66.667,-66.667) ENVELOPE(140.013,140.013,-66.667,-66.667) |
geographic |
Antarctic The Antarctic Dumont d'Urville Dumont-d'Urville |
geographic_facet |
Antarctic The Antarctic Dumont d'Urville Dumont-d'Urville |
genre |
Antarc* Antarctic Antarctica Ice Sheet |
genre_facet |
Antarc* Antarctic Antarctica Ice Sheet |
op_source |
Proceedings, annual meeting, Electron Microscopy Society of America volume 50, issue 2, page 1716-1717 ISSN 0424-8201 2690-1315 |
op_rights |
https://www.cambridge.org/core/terms |
op_doi |
https://doi.org/10.1017/s0424820100133217 |
container_title |
Proceedings, annual meeting, Electron Microscopy Society of America |
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50 |
container_issue |
2 |
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1716 |
op_container_end_page |
1717 |
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1792507210606051328 |