δ²H, δ¹⁸O and Deuterium excess values in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia
Fuente:
PANGAEA
Enregistré dans:
| Auteurs principaux: | , , , , , |
|---|---|
| Format: | Dataset Open Access |
| Langue: | en |
| Publié: |
PANGAEA
2021
|
| Sujets: | |
| Accès en ligne: | |
| Tags: |
Ajouter un tag
Pas de tags, Soyez le premier à ajouter un tag!
|
| _version_ | 1867169146163167232 |
|---|---|
| author | Vasil'chuk, Yurij K Budantseva, Nadine A Vasil'chuk, Alla Constantinovna Chizhova, Julia N Podborny, Yevgeny Vasil'chuk, Jessica Yurevna |
| author_facet | Vasil'chuk, Yurij K Budantseva, Nadine A Vasil'chuk, Alla Constantinovna Chizhova, Julia N Podborny, Yevgeny Vasil'chuk, Jessica Yurevna |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. The multistage massive-ice bodies have thickness up to 5.7 m and occur in Holocene sediments of modern floodplain and the first terrace of the coastal lagoon. Stable isotope analyses revealed that the multistage massive ice bodies formed syngenetically during the freezing of water- saturated sediment, under intensive cryogenic fractionation. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_933096 |
| institution | PANGAEA |
| language | en |
| publishDate | 2021 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | δ²H, δ¹⁸O and Deuterium excess values in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia Vasil'chuk, Yurij K Budantseva, Nadine A Vasil'chuk, Alla Constantinovna Chizhova, Julia N Podborny, Yevgeny Vasil'chuk, Jessica Yurevna Borehole number; Depth, relative; Deuterium excess; Holocene; Ice type; Ion concentrations; Location; massive ice; Mass spectrometer Finnigan Delta-V; MULT; Multiple investigations; pollen and spores; Sabettayakha_river; Sabettayakha River; Sample ID; stable isotope data; Yamal Peninsula; Yamal Peninsula, northwestern Siberia; δ18O; δ Deuterium Holocene massive ground ice near the Sabettayakha River mouth, on the coast of the Gulf of Ob, Yamal Peninsula, northwest Siberia is studied. The multistage massive-ice bodies have thickness up to 5.7 m and occur in Holocene sediments of modern floodplain and the first terrace of the coastal lagoon. Stable isotope analyses revealed that the multistage massive ice bodies formed syngenetically during the freezing of water- saturated sediment, under intensive cryogenic fractionation. |
| title | δ²H, δ¹⁸O and Deuterium excess values in Holocene multistage massive ice near the Sabettayakha River mouth, Yamal Peninsula, northwest Siberia |
| topic | Borehole number; Depth, relative; Deuterium excess; Holocene; Ice type; Ion concentrations; Location; massive ice; Mass spectrometer Finnigan Delta-V; MULT; Multiple investigations; pollen and spores; Sabettayakha_river; Sabettayakha River; Sample ID; stable isotope data; Yamal Peninsula; Yamal Peninsula, northwestern Siberia; δ18O; δ Deuterium |
| url | https://doi.org/10.1594/PANGAEA.933096 |