The first luminescence dating of Tibetan glacier basal sediment

Dating ice cores drilled in the high mountain glaciers is difficult because seasonal variations cannot be traced at depth due to rapid thinning of the ice layers. Here we provide the first luminescence dating of the basal sediment of the Chongce ice cap in the north-western Tibetan Plateau. Assuming...

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Published in:The Cryosphere
Main Authors: Zhang, Zhu, Hou, Shugui, Yi, Shuangwen
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-12-163-2018
https://tc.copernicus.org/articles/12/163/2018/
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spelling ftcopernicus:oai:publications.copernicus.org:tc58487 2023-05-15T16:38:06+02:00 The first luminescence dating of Tibetan glacier basal sediment Zhang, Zhu Hou, Shugui Yi, Shuangwen 2018-09-27 application/pdf https://doi.org/10.5194/tc-12-163-2018 https://tc.copernicus.org/articles/12/163/2018/ eng eng doi:10.5194/tc-12-163-2018 https://tc.copernicus.org/articles/12/163/2018/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-12-163-2018 2020-07-20T16:23:27Z Dating ice cores drilled in the high mountain glaciers is difficult because seasonal variations cannot be traced at depth due to rapid thinning of the ice layers. Here we provide the first luminescence dating of the basal sediment of the Chongce ice cap in the north-western Tibetan Plateau. Assuming the sediment is of similar (or older) age as the surrounding ice, the luminescence dating of 42 ± 4 ka provides an upper constraint for the age of the bottom ice at the drilling site. This result is more than 1 order of magnitude younger than the previously suggested age of the basal ice of the nearby Guliya ice cap (∼ 40 km in distance). Text Ice cap Copernicus Publications: E-Journals The Cryosphere 12 1 163 168
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description Dating ice cores drilled in the high mountain glaciers is difficult because seasonal variations cannot be traced at depth due to rapid thinning of the ice layers. Here we provide the first luminescence dating of the basal sediment of the Chongce ice cap in the north-western Tibetan Plateau. Assuming the sediment is of similar (or older) age as the surrounding ice, the luminescence dating of 42 ± 4 ka provides an upper constraint for the age of the bottom ice at the drilling site. This result is more than 1 order of magnitude younger than the previously suggested age of the basal ice of the nearby Guliya ice cap (∼ 40 km in distance).
format Text
author Zhang, Zhu
Hou, Shugui
Yi, Shuangwen
spellingShingle Zhang, Zhu
Hou, Shugui
Yi, Shuangwen
The first luminescence dating of Tibetan glacier basal sediment
author_facet Zhang, Zhu
Hou, Shugui
Yi, Shuangwen
author_sort Zhang, Zhu
title The first luminescence dating of Tibetan glacier basal sediment
title_short The first luminescence dating of Tibetan glacier basal sediment
title_full The first luminescence dating of Tibetan glacier basal sediment
title_fullStr The first luminescence dating of Tibetan glacier basal sediment
title_full_unstemmed The first luminescence dating of Tibetan glacier basal sediment
title_sort first luminescence dating of tibetan glacier basal sediment
publishDate 2018
url https://doi.org/10.5194/tc-12-163-2018
https://tc.copernicus.org/articles/12/163/2018/
genre Ice cap
genre_facet Ice cap
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-12-163-2018
https://tc.copernicus.org/articles/12/163/2018/
op_doi https://doi.org/10.5194/tc-12-163-2018
container_title The Cryosphere
container_volume 12
container_issue 1
container_start_page 163
op_container_end_page 168
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