Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice

The terrestrial ages of three Allan Hills meteorites are between 3 × 10 4 and 3 × 10 5 years and one is (1.54 –0.28 +0.14 ) × 10 6 years old. The Antarctic ice sheet is therefore older than (1.54 –0.28 +0.14 ) × 10 6 years and the meteorite accumulation process at Allan Hills probably began between...

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Published in:Science
Main Authors: Fireman, E. L., Rancitelli, L. A., Kirsten, T.
Format: Article in Journal/Newspaper
Language:English
Published: American Association for the Advancement of Science (AAAS) 1979
Subjects:
Online Access:http://dx.doi.org/10.1126/science.203.4379.453
https://www.science.org/doi/pdf/10.1126/science.203.4379.453
id craaas:10.1126/science.203.4379.453
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spelling craaas:10.1126/science.203.4379.453 2024-06-09T07:38:37+00:00 Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice Fireman, E. L. Rancitelli, L. A. Kirsten, T. 1979 http://dx.doi.org/10.1126/science.203.4379.453 https://www.science.org/doi/pdf/10.1126/science.203.4379.453 en eng American Association for the Advancement of Science (AAAS) Science volume 203, issue 4379, page 453-455 ISSN 0036-8075 1095-9203 journal-article 1979 craaas https://doi.org/10.1126/science.203.4379.453 2024-05-16T12:55:02Z The terrestrial ages of three Allan Hills meteorites are between 3 × 10 4 and 3 × 10 5 years and one is (1.54 –0.28 +0.14 ) × 10 6 years old. The Antarctic ice sheet is therefore older than (1.54 –0.28 +0.14 ) × 10 6 years and the meteorite accumulation process at Allan Hills probably began between 3 × 10 4 and 3 × 10 5 years ago. Article in Journal/Newspaper Antarc* Antarctic Ice Sheet AAAS Resource Center (American Association for the Advancement of Science) Allan Hills ENVELOPE(159.667,159.667,-76.717,-76.717) Antarctic The Antarctic Science 203 4379 453 455
institution Open Polar
collection AAAS Resource Center (American Association for the Advancement of Science)
op_collection_id craaas
language English
description The terrestrial ages of three Allan Hills meteorites are between 3 × 10 4 and 3 × 10 5 years and one is (1.54 –0.28 +0.14 ) × 10 6 years old. The Antarctic ice sheet is therefore older than (1.54 –0.28 +0.14 ) × 10 6 years and the meteorite accumulation process at Allan Hills probably began between 3 × 10 4 and 3 × 10 5 years ago.
format Article in Journal/Newspaper
author Fireman, E. L.
Rancitelli, L. A.
Kirsten, T.
spellingShingle Fireman, E. L.
Rancitelli, L. A.
Kirsten, T.
Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
author_facet Fireman, E. L.
Rancitelli, L. A.
Kirsten, T.
author_sort Fireman, E. L.
title Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
title_short Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
title_full Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
title_fullStr Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
title_full_unstemmed Terrestrial Ages of Four Allan Hills Meteorites: Consequences for Antarctic Ice
title_sort terrestrial ages of four allan hills meteorites: consequences for antarctic ice
publisher American Association for the Advancement of Science (AAAS)
publishDate 1979
url http://dx.doi.org/10.1126/science.203.4379.453
https://www.science.org/doi/pdf/10.1126/science.203.4379.453
long_lat ENVELOPE(159.667,159.667,-76.717,-76.717)
geographic Allan Hills
Antarctic
The Antarctic
geographic_facet Allan Hills
Antarctic
The Antarctic
genre Antarc*
Antarctic
Ice Sheet
genre_facet Antarc*
Antarctic
Ice Sheet
op_source Science
volume 203, issue 4379, page 453-455
ISSN 0036-8075 1095-9203
op_doi https://doi.org/10.1126/science.203.4379.453
container_title Science
container_volume 203
container_issue 4379
container_start_page 453
op_container_end_page 455
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