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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Bibliographic Details
Published in:The Cryosphere
Main Authors: Z. Zhang, S. Hou, S. Yi
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2018
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-12-163-2018
https://www.the-cryosphere.net/12/163/2018/tc-12-163-2018.pdf
https://doaj.org/article/be3f21ed699a4cd593d6845969daa78b
id fttriple:oai:gotriple.eu:oai:doaj.org/article:be3f21ed699a4cd593d6845969daa78b
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spelling fttriple:oai:gotriple.eu:oai:doaj.org/article:be3f21ed699a4cd593d6845969daa78b 2023-05-15T16:38:06+02:00 The first luminescence dating of Tibetan glacier basal sediment Z. Zhang S. Hou S. Yi 2018-01-01 https://doi.org/10.5194/tc-12-163-2018 https://www.the-cryosphere.net/12/163/2018/tc-12-163-2018.pdf https://doaj.org/article/be3f21ed699a4cd593d6845969daa78b en eng Copernicus Publications doi:10.5194/tc-12-163-2018 1994-0416 1994-0424 https://www.the-cryosphere.net/12/163/2018/tc-12-163-2018.pdf https://doaj.org/article/be3f21ed699a4cd593d6845969daa78b undefined The Cryosphere, Vol 12, Pp 163-168 (2018) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2018 fttriple https://doi.org/10.5194/tc-12-163-2018 2023-01-22T19:37:20Z 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). Article in Journal/Newspaper Ice cap The Cryosphere Unknown The Cryosphere 12 1 163 168
institution Open Polar
collection Unknown
op_collection_id fttriple
language English
topic geo
envir
spellingShingle geo
envir
Z. Zhang
S. Hou
S. Yi
The first luminescence dating of Tibetan glacier basal sediment
topic_facet geo
envir
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 Article in Journal/Newspaper
author Z. Zhang
S. Hou
S. Yi
author_facet Z. Zhang
S. Hou
S. Yi
author_sort Z. Zhang
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
publisher Copernicus Publications
publishDate 2018
url https://doi.org/10.5194/tc-12-163-2018
https://www.the-cryosphere.net/12/163/2018/tc-12-163-2018.pdf
https://doaj.org/article/be3f21ed699a4cd593d6845969daa78b
genre Ice cap
The Cryosphere
genre_facet Ice cap
The Cryosphere
op_source The Cryosphere, Vol 12, Pp 163-168 (2018)
op_relation doi:10.5194/tc-12-163-2018
1994-0416
1994-0424
https://www.the-cryosphere.net/12/163/2018/tc-12-163-2018.pdf
https://doaj.org/article/be3f21ed699a4cd593d6845969daa78b
op_rights undefined
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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