δ¹⁸O patterns in massive ice, Gyda River terrace I, northern Gydan Peninsula

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Main Authors: Vasil'chuk, Yurij K, Budantseva, Nadine A, Vasil'chuk, Alla Constantinovna, Podborny, Yevgenij Ye, Chizhova, Julia N
Format: Dataset Open Access
Language:en
Published: PANGAEA 2021
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author Vasil'chuk, Yurij K
Budantseva, Nadine A
Vasil'chuk, Alla Constantinovna
Podborny, Yevgenij Ye
Chizhova, Julia N
author_facet Vasil'chuk, Yurij K
Budantseva, Nadine A
Vasil'chuk, Alla Constantinovna
Podborny, Yevgenij Ye
Chizhova, Julia N
collection Datos científicos de ciencias marinas y ambientales
contents Lenses of massive ground ice and cryopegs were found at different levels in Holocene deposits in the northeastern Yamal Peninsula. Massive ice, 7 to 9 m thick, occurs at the depth 12 m under the Seyakha (Mutnaya) River. Multistage massive ground ice (four lenses, 0.4 m thick and 8 m long) exists in Gyda terrace I. Lateral and vertical δ18O isotope patterns in the Sabetta and Gyda multistage massive ice complexes indicate their heterogeneity and intrasedimental origin by segregation or a combined intrusive-segregation mechanism.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_938419
institution PANGAEA
language en
publishDate 2021
publisher PANGAEA
record_format pangaea
spellingShingle δ¹⁸O patterns in massive ice, Gyda River terrace I, northern Gydan Peninsula
Vasil'chuk, Yurij K
Budantseva, Nadine A
Vasil'chuk, Alla Constantinovna
Podborny, Yevgenij Ye
Chizhova, Julia N
cryopegs; DEPTH, sediment/rock; Gyda_Bay; Holocene; Holocene sea-level changes; Location; massive ice; MULT; Multiple investigations; northern West Siberia; Permafrost; Permafrost temperature; Sample comment; Sample type; Stable isotopes; stable isotopes of water; Yamal-Nenets, Russia; Yamal Peninsula; δ18O
Lenses of massive ground ice and cryopegs were found at different levels in Holocene deposits in the northeastern Yamal Peninsula. Massive ice, 7 to 9 m thick, occurs at the depth 12 m under the Seyakha (Mutnaya) River. Multistage massive ground ice (four lenses, 0.4 m thick and 8 m long) exists in Gyda terrace I. Lateral and vertical δ18O isotope patterns in the Sabetta and Gyda multistage massive ice complexes indicate their heterogeneity and intrasedimental origin by segregation or a combined intrusive-segregation mechanism.
title δ¹⁸O patterns in massive ice, Gyda River terrace I, northern Gydan Peninsula
topic cryopegs; DEPTH, sediment/rock; Gyda_Bay; Holocene; Holocene sea-level changes; Location; massive ice; MULT; Multiple investigations; northern West Siberia; Permafrost; Permafrost temperature; Sample comment; Sample type; Stable isotopes; stable isotopes of water; Yamal-Nenets, Russia; Yamal Peninsula; δ18O
url https://doi.org/10.1594/PANGAEA.938419