Uranium-series dating of tephra-banded Allan Hills ice
Tephra-banded ice samples from the main Allan Hills icefield, Antarctica, are dated by a uranium-series method, which is based on the ^<226>Ra/^<230>Th and ^<226>Ra/^<234>U ratios dissolved in ice from tephra. The consistence between the age determined from the ^<226>Ra...
Main Author: | |
---|---|
Format: | Report |
Language: | English |
Published: |
Smithsonian Astrophysical Observatory
1989
|
Subjects: | |
Online Access: | https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4495 http://id.nii.ac.jp/1291/00004495/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4495&item_no=1&attribute_id=18&file_no=1 |
id |
ftnipr:oai:nipr.repo.nii.ac.jp:00004495 |
---|---|
record_format |
openpolar |
spelling |
ftnipr:oai:nipr.repo.nii.ac.jp:00004495 2023-05-15T13:49:01+02:00 Uranium-series dating of tephra-banded Allan Hills ice Edward L. Fireman 1989-10 https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4495 http://id.nii.ac.jp/1291/00004495/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4495&item_no=1&attribute_id=18&file_no=1 en eng Smithsonian Astrophysical Observatory National Institute of Polar Research https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4495 http://id.nii.ac.jp/1291/00004495/ AA10784627 Proceedings of the NIPR Symposium on Antarctic Meteorites, 2, 335-343(1989-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4495&item_no=1&attribute_id=18&file_no=1 Departmental Bulletin Paper P(論文) 1989 ftnipr 2023-01-28T20:04:07Z Tephra-banded ice samples from the main Allan Hills icefield, Antarctica, are dated by a uranium-series method, which is based on the ^<226>Ra/^<230>Th and ^<226>Ra/^<234>U ratios dissolved in ice from tephra. The consistence between the age determined from the ^<226>Ra/^<230>Th ratio with the age determined from the ^<226>Ra/^<234>U ratio serves as a check on the method. For ice from a location at the western border of the 50-km^2 area that is richly laden with meteorites, the ^<226>Ra/^<230>Th and ^<226>Ra/^<234>U ages are (95±10)×10^3 and (100±10)×10^3 years, respectively. For ice from a location within this meteorite-rich area near its eastern border (approximately 5km closer to the Allan Hills land barrier), these ages are (185±25)×10^3 and (210±30)×10^3 years, respectively. The ice flow is from west to east, the dates indicate that most of the ice in the meteorite-rich area is between 1×10^5 and 2×10^5 years old with the age of the ice increasing in the flow direction as theoretically predicted for ice approaching a land barrier. The comparison of this ice chronology with the terrestrial ages of the meteorites leads to a number of conclusions about the meteorite fall rate and history of the ice movement. Report Antarc* Antarctica National Institute of Polar Research Repository, Japan Allan Hills ENVELOPE(159.667,159.667,-76.717,-76.717) |
institution |
Open Polar |
collection |
National Institute of Polar Research Repository, Japan |
op_collection_id |
ftnipr |
language |
English |
description |
Tephra-banded ice samples from the main Allan Hills icefield, Antarctica, are dated by a uranium-series method, which is based on the ^<226>Ra/^<230>Th and ^<226>Ra/^<234>U ratios dissolved in ice from tephra. The consistence between the age determined from the ^<226>Ra/^<230>Th ratio with the age determined from the ^<226>Ra/^<234>U ratio serves as a check on the method. For ice from a location at the western border of the 50-km^2 area that is richly laden with meteorites, the ^<226>Ra/^<230>Th and ^<226>Ra/^<234>U ages are (95±10)×10^3 and (100±10)×10^3 years, respectively. For ice from a location within this meteorite-rich area near its eastern border (approximately 5km closer to the Allan Hills land barrier), these ages are (185±25)×10^3 and (210±30)×10^3 years, respectively. The ice flow is from west to east, the dates indicate that most of the ice in the meteorite-rich area is between 1×10^5 and 2×10^5 years old with the age of the ice increasing in the flow direction as theoretically predicted for ice approaching a land barrier. The comparison of this ice chronology with the terrestrial ages of the meteorites leads to a number of conclusions about the meteorite fall rate and history of the ice movement. |
format |
Report |
author |
Edward L. Fireman |
spellingShingle |
Edward L. Fireman Uranium-series dating of tephra-banded Allan Hills ice |
author_facet |
Edward L. Fireman |
author_sort |
Edward L. Fireman |
title |
Uranium-series dating of tephra-banded Allan Hills ice |
title_short |
Uranium-series dating of tephra-banded Allan Hills ice |
title_full |
Uranium-series dating of tephra-banded Allan Hills ice |
title_fullStr |
Uranium-series dating of tephra-banded Allan Hills ice |
title_full_unstemmed |
Uranium-series dating of tephra-banded Allan Hills ice |
title_sort |
uranium-series dating of tephra-banded allan hills ice |
publisher |
Smithsonian Astrophysical Observatory |
publishDate |
1989 |
url |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4495 http://id.nii.ac.jp/1291/00004495/ https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4495&item_no=1&attribute_id=18&file_no=1 |
long_lat |
ENVELOPE(159.667,159.667,-76.717,-76.717) |
geographic |
Allan Hills |
geographic_facet |
Allan Hills |
genre |
Antarc* Antarctica |
genre_facet |
Antarc* Antarctica |
op_relation |
https://nipr.repo.nii.ac.jp/?action=repository_uri&item_id=4495 http://id.nii.ac.jp/1291/00004495/ AA10784627 Proceedings of the NIPR Symposium on Antarctic Meteorites, 2, 335-343(1989-10) https://nipr.repo.nii.ac.jp/?action=repository_action_common_download&item_id=4495&item_no=1&attribute_id=18&file_no=1 |
_version_ |
1766250471807254528 |