Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)

Unusually large cryoturbation structures (4–4.5 m amplitude), developed in channel gravels and overbank fine‐grained deposits of a river terrace on the NE Tibet Plateau, China, were formed by loadcasting as late Pleistocene‐age permafrost degraded. It is suggested that the oversaturation and liquefa...

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Published in:Permafrost and Periglacial Processes
Main Authors: J. Vandenberghe, X. Wang, D. Vandenberghe
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Ice
Online Access:https://doi.org/10.1002/ppp.1847
id ftrepec:oai:RePEc:wly:perpro:v:27:y:2016:i:1:p:138-143
record_format openpolar
spelling ftrepec:oai:RePEc:wly:perpro:v:27:y:2016:i:1:p:138-143 2023-05-15T16:36:55+02:00 Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China) J. Vandenberghe X. Wang D. Vandenberghe https://doi.org/10.1002/ppp.1847 unknown https://doi.org/10.1002/ppp.1847 article ftrepec https://doi.org/10.1002/ppp.1847 2020-12-04T13:31:25Z Unusually large cryoturbation structures (4–4.5 m amplitude), developed in channel gravels and overbank fine‐grained deposits of a river terrace on the NE Tibet Plateau, China, were formed by loadcasting as late Pleistocene‐age permafrost degraded. It is suggested that the oversaturation and liquefaction of the thawed sediments could have been achieved only if the amount of ice in the upper 4–4.5 m of terrace sediments had been very high. The structures, dated at around 26–20 ka by OSL, point to the presence of a massive icy layer existing within a permafrost body during the Last Permafrost Maximum. Copyright © 2015 John Wiley & Sons, Ltd. Article in Journal/Newspaper Ice permafrost RePEc (Research Papers in Economics) Permafrost and Periglacial Processes 27 1 138 143
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Unusually large cryoturbation structures (4–4.5 m amplitude), developed in channel gravels and overbank fine‐grained deposits of a river terrace on the NE Tibet Plateau, China, were formed by loadcasting as late Pleistocene‐age permafrost degraded. It is suggested that the oversaturation and liquefaction of the thawed sediments could have been achieved only if the amount of ice in the upper 4–4.5 m of terrace sediments had been very high. The structures, dated at around 26–20 ka by OSL, point to the presence of a massive icy layer existing within a permafrost body during the Last Permafrost Maximum. Copyright © 2015 John Wiley & Sons, Ltd.
format Article in Journal/Newspaper
author J. Vandenberghe
X. Wang
D. Vandenberghe
spellingShingle J. Vandenberghe
X. Wang
D. Vandenberghe
Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
author_facet J. Vandenberghe
X. Wang
D. Vandenberghe
author_sort J. Vandenberghe
title Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
title_short Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
title_full Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
title_fullStr Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
title_full_unstemmed Very Large Cryoturbation Structures of Last Permafrost Maximum Age at the Foot of the Qilian Mountains (NE Tibet Plateau, China)
title_sort very large cryoturbation structures of last permafrost maximum age at the foot of the qilian mountains (ne tibet plateau, china)
url https://doi.org/10.1002/ppp.1847
genre Ice
permafrost
genre_facet Ice
permafrost
op_relation https://doi.org/10.1002/ppp.1847
op_doi https://doi.org/10.1002/ppp.1847
container_title Permafrost and Periglacial Processes
container_volume 27
container_issue 1
container_start_page 138
op_container_end_page 143
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