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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Language: | English |
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Cambridge University Press (CUP)
1993
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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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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 |
_version_ |
1792504003993534464 |