Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ...
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a...
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Online Access: | https://dx.doi.org/10.1594/pangaea.939682 https://doi.pangaea.de/10.1594/PANGAEA.939682 |
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ftdatacite:10.1594/pangaea.939682 2024-09-09T19:44:20+00:00 Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna 2022 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.939682 https://doi.pangaea.de/10.1594/PANGAEA.939682 en eng PANGAEA https://dx.doi.org/10.1016/s0012-821x(00)00122-9 https://dx.doi.org/10.1016/s0168-583x(00)00212-3 https://dx.doi.org/10.3103/s0145875218010131 https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.21782/ec2541-9994-2020-2(3-13) https://dx.doi.org/10.1017/s0033822200041199 https://dx.doi.org/10.1134/s1028334x19110096 https://dx.doi.org/10.1134/s1028334x20020154 Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 Late Pleistocene organic organic accumulation Permafrost radiocarbon dating syngenetic ice-wedges Event label Latitude of event Longitude of event Sample ID Sample comment Location AGE Age, error ELEVATION Age, dated material Reference/source Multiple investigations Age, radiocarbon dataset Dataset 2022 ftdatacite https://doi.org/10.1594/pangaea.93968210.1016/s0012-821x(00)00122-910.1016/s0168-583x(00)00212-310.3103/s014587521801013110.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1017/s003382220004119910.1134/s1028334x1911009610.1134/s1028334x2 2024-08-01T10:50:55Z Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. ... : The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky). ... Dataset Ice permafrost wedge* DataCite |
institution |
Open Polar |
collection |
DataCite |
op_collection_id |
ftdatacite |
language |
English |
topic |
Late Pleistocene organic organic accumulation Permafrost radiocarbon dating syngenetic ice-wedges Event label Latitude of event Longitude of event Sample ID Sample comment Location AGE Age, error ELEVATION Age, dated material Reference/source Multiple investigations Age, radiocarbon |
spellingShingle |
Late Pleistocene organic organic accumulation Permafrost radiocarbon dating syngenetic ice-wedges Event label Latitude of event Longitude of event Sample ID Sample comment Location AGE Age, error ELEVATION Age, dated material Reference/source Multiple investigations Age, radiocarbon Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
topic_facet |
Late Pleistocene organic organic accumulation Permafrost radiocarbon dating syngenetic ice-wedges Event label Latitude of event Longitude of event Sample ID Sample comment Location AGE Age, error ELEVATION Age, dated material Reference/source Multiple investigations Age, radiocarbon |
description |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedges polygonal massives of Russian permafrost zone is represented. Dating of Late Pleistocene syngenetic ice wedges is possible with using of radiocarbon dates of the host sediments indirectly. Formation of syngenetic ice wedges is a cyclically-interrupted process. Fluvial origin of syngenetic sediments formed of ice wedge thickness determines presence of allochthonous and autochthonous organic material there. This is the main cause of age inversions or disturbances in the radiocarbon date series from syngenetic permafrost cross-sections. ... : The ¹⁴C measurements were made in the Geological Institute of the Russian Academy of Sciences (L. Sulerzhitsky). ... |
format |
Dataset |
author |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_facet |
Vasil'chuk, Yurij K Vasil'chuk, Alla Constantinovna |
author_sort |
Vasil'chuk, Yurij K |
title |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
title_short |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
title_full |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
title_fullStr |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
title_full_unstemmed |
Radiocarbon dating of the Late Pleistocene thick syngenetic ice-wedge polygonal massives of Russian permafrost zone ... |
title_sort |
radiocarbon dating of the late pleistocene thick syngenetic ice-wedge polygonal massives of russian permafrost zone ... |
publisher |
PANGAEA |
publishDate |
2022 |
url |
https://dx.doi.org/10.1594/pangaea.939682 https://doi.pangaea.de/10.1594/PANGAEA.939682 |
genre |
Ice permafrost wedge* |
genre_facet |
Ice permafrost wedge* |
op_relation |
https://dx.doi.org/10.1016/s0012-821x(00)00122-9 https://dx.doi.org/10.1016/s0168-583x(00)00212-3 https://dx.doi.org/10.3103/s0145875218010131 https://dx.doi.org/10.21782/kz1560-7496-2018-5(3-19) https://dx.doi.org/10.21782/ec2541-9994-2020-2(3-13) https://dx.doi.org/10.1017/s0033822200041199 https://dx.doi.org/10.1134/s1028334x19110096 https://dx.doi.org/10.1134/s1028334x20020154 |
op_rights |
Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode cc-by-4.0 |
op_doi |
https://doi.org/10.1594/pangaea.93968210.1016/s0012-821x(00)00122-910.1016/s0168-583x(00)00212-310.3103/s014587521801013110.21782/kz1560-7496-2018-5(3-19)10.21782/ec2541-9994-2020-2(3-13)10.1017/s003382220004119910.1134/s1028334x1911009610.1134/s1028334x2 |
_version_ |
1809914050172157952 |