A Regional Geochronological Study of Late Pleistocene Permafrost

The use of radiocarbon dating in geocryological investigations makes it possible to establish a chronology for permafrost-geological development during the Late Pleistocene. Both global and regional time scales for the formation of Late Pleistocene permafrost have been worked out over the past 15–20...

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Published in:Radiocarbon
Main Author: Kostyukevich, V. V.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1993
Subjects:
Online Access:http://dx.doi.org/10.1017/s0033822200060501
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060501
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spelling crcambridgeupr:10.1017/s0033822200060501 2024-03-03T08:47:45+00:00 A Regional Geochronological Study of Late Pleistocene Permafrost Kostyukevich, V. V. 1993 http://dx.doi.org/10.1017/s0033822200060501 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060501 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Radiocarbon volume 35, issue 3, page 477-486 ISSN 0033-8222 1945-5755 General Earth and Planetary Sciences Archeology journal-article 1993 crcambridgeupr https://doi.org/10.1017/s0033822200060501 2024-02-08T08:36:34Z The use of radiocarbon dating in geocryological investigations makes it possible to establish a chronology for permafrost-geological development during the Late Pleistocene. Both global and regional time scales for the formation of Late Pleistocene permafrost have been worked out over the past 15–20 years at the Permafrost Institute of the Siberian Branch of the Russian Academy of Sciences. I present here results from study areas of northwestern Siberia and of North, Central and West Yakutia. Article in Journal/Newspaper permafrost Yakutia Siberia Cambridge University Press Radiocarbon 35 3 477 486
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic General Earth and Planetary Sciences
Archeology
spellingShingle General Earth and Planetary Sciences
Archeology
Kostyukevich, V. V.
A Regional Geochronological Study of Late Pleistocene Permafrost
topic_facet General Earth and Planetary Sciences
Archeology
description The use of radiocarbon dating in geocryological investigations makes it possible to establish a chronology for permafrost-geological development during the Late Pleistocene. Both global and regional time scales for the formation of Late Pleistocene permafrost have been worked out over the past 15–20 years at the Permafrost Institute of the Siberian Branch of the Russian Academy of Sciences. I present here results from study areas of northwestern Siberia and of North, Central and West Yakutia.
format Article in Journal/Newspaper
author Kostyukevich, V. V.
author_facet Kostyukevich, V. V.
author_sort Kostyukevich, V. V.
title A Regional Geochronological Study of Late Pleistocene Permafrost
title_short A Regional Geochronological Study of Late Pleistocene Permafrost
title_full A Regional Geochronological Study of Late Pleistocene Permafrost
title_fullStr A Regional Geochronological Study of Late Pleistocene Permafrost
title_full_unstemmed A Regional Geochronological Study of Late Pleistocene Permafrost
title_sort regional geochronological study of late pleistocene permafrost
publisher Cambridge University Press (CUP)
publishDate 1993
url http://dx.doi.org/10.1017/s0033822200060501
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0033822200060501
genre permafrost
Yakutia
Siberia
genre_facet permafrost
Yakutia
Siberia
op_source Radiocarbon
volume 35, issue 3, page 477-486
ISSN 0033-8222 1945-5755
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0033822200060501
container_title Radiocarbon
container_volume 35
container_issue 3
container_start_page 477
op_container_end_page 486
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